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Parameter Dictionary for QUEST4D – 22 October 2008 Parameter: BDENS - Bulk density Method: 1040 Matrix: US - Unfractionated Unit: g/cm3 Description: Determination of vertical bulk density profiles by non-intrusive gamma- ray-attenuation measurements. The gamma-ray-densitometer moves automatically along the sediment core in 1 cm steps. The magnitude of attenuation depends on the bulk density of the exposed material and the diameter of the column. (Gerland and Villiger, 1995). Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2 Sample Handling Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None Separation: None Procedure description:

Dictionary for QUEST4D 22 October 2008 - mumm.ac.be€¦Parameter Dictionary for QUEST4D – 22 October 2008 Parameter: BDENS - Bulk density Method: 1040 Matrix: US - Unfractionated

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Parameter Dictionary for QUEST4D – 22 October 2008 

Parameter: BDENS - Bulk density

Method: 1040

Matrix: US - Unfractionated

Unit: g/cm3 Description: Determination of vertical bulk density profiles by non-intrusive gamma-

ray-attenuation measurements. The gamma-ray-densitometer moves automatically along the sediment core in 1 cm steps. The magnitude of attenuation depends on the bulk density of the exposed material and the diameter of the column. (Gerland and Villiger, 1995).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: TAU_CR_E - Critical shear stress for erosion

Method: 1041

Matrix: US - Unfractionated

Unit: Pa Description: The SETEG-System determines a depth oriented measurement of the

critical erosion shear stress (usually in depth intervals of 2-3 cm). The sediment core is mounted on the bottom of the pressure duct, exposing the sediment surface to the flow. The continuously adjustable discharge is increased, until entrainment of sediment particles from the surface can be observed. The corresponding wall shear stress can be determined by a hydraulic calibration function which describes the relationship between wall shear stress and discharge through pressure loss.

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.44 - Erosion rate at an excess shear stress of 0.44 Pa

Method: 1042

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.01 - Erosion rate at an excess shear stress of 0.01 Pa

Method: 1043

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.02 - Erosion rate at an excess shear stress of 0.02 Pa

Method: 1044

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.03 - Erosion rate at an excess shear stress of 0.03 Pa

Method: 1045

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.04 - Erosion rate at an excess shear stress of 0.04 Pa

Method: 1046

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.05 - Erosion rate at an excess shear stress of 0.05 Pa

Method: 1047

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.06 - Erosion rate at an excess shear stress of 0.06 Pa

Method: 1048

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.07 - Erosion rate at an excess shear stress of 0.07 Pa

Method: 1049

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.09 - Erosion rate at an excess shear stress of 0.09 Pa

Method: 1050

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.10 - Erosion rate at an excess shear stress of 0.1 Pa

Method: 1051

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.11 - Erosion rate at an excess shear stress of 0.11 Pa

Method: 1052

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.12 - Erosion rate at an excess shear stress of 0.12 Pa

Method: 1053

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.13 - Erosion rate at an excess shear stress of 0.13 Pa

Method: 1054

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.14 - Erosion rate at an excess shear stress of 0.14 Pa

Method: 1055

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.15 - Erosion rate at an excess shear stress of 0.15 Pa

Method: 1056

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.16 - Erosion rate at an excess shear stress of 0.16 Pa

Method: 1057

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.17 - Erosion rate at an excess shear stress of 0.17 Pa

Method: 1058

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.18 - Erosion rate at an excess shear stress of 0.18 Pa

Method: 1059

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.19 - Erosion rate at an excess shear stress of 0.19 Pa

Method: 1060

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.20 - Erosion rate at an excess shear stress of 0.2 Pa

Method: 1061

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.21 - Erosion rate at an excess shear stress of 0.21 Pa

Method: 1062

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.22 - Erosion rate at an excess shear stress of 0.22 Pa

Method: 1063

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.23 - Erosion rate at an excess shear stress of 0.23 Pa

Method: 1064

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.24 - Erosion rate at an excess shear stress of 0.24 Pa

Method: 1065

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.25 - Erosion rate at an excess shear stress of 0.25 Pa

Method: 1066

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.26 - Erosion rate at an excess shear stress of 0.26 Pa

Method: 1067

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.27 - Erosion rate at an excess shear stress of 0.27 Pa

Method: 1068

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.28 - Erosion rate at an excess shear stress of 0.28 Pa

Method: 1069

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.29 - Erosion rate at an excess shear stress of 0.29 Pa

Method: 1070

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.30 - Erosion rate at an excess shear stress of 0.3 Pa

Method: 1071

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.31 - Erosion rate at an excess shear stress of 0.31 Pa

Method: 1072

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.32 - Erosion rate at an excess shear stress of 0.32 Pa

Method: 1073

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.33 - Erosion rate at an excess shear stress of 0.33 Pa

Method: 1074

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.34 - Erosion rate at an excess shear stress of 0.34 Pa

Method: 1075

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.35 - Erosion rate at an excess shear stress of 0.35 Pa

Method: 1076

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.36 - Erosion rate at an excess shear stress of 0.36 Pa

Method: 1077

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.37 - Erosion rate at an excess shear stress of 0.37 Pa

Method: 1078

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET.378 - Erosion rate at an excess shear stress of 0.378 Pa

Method: 1079

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.38 - Erosion rate at an excess shear stress of 0.38 Pa

Method: 1080

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.39 - Erosion rate at an excess shear stress of 0.39 Pa

Method: 1081

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.40 - Erosion rate at an excess shear stress of 0.4 Pa

Method: 1082

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.41 - Erosion rate at an excess shear stress of 0.41 Pa

Method: 1083

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.43 - Erosion rate at an excess shear stress of 0.43 Pa

Method: 1084

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.45 - Erosion rate at an excess shear stress of 0.45 Pa

Method: 1085

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.46 - Erosion rate at an excess shear stress of 0.46 Pa

Method: 1086

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.47 - Erosion rate at an excess shear stress of 0.47 Pa

Method: 1087

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.48 - Erosion rate at an excess shear stress of 0.48 Pa

Method: 1088

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.49 - Erosion rate at an excess shear stress of 0.49 Pa

Method: 1089

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.50 - Erosion rate at an excess shear stress of 0.5 Pa

Method: 1090

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.51 - Erosion rate at an excess shear stress of 0.51 Pa

Method: 1091

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.54 - Erosion rate at an excess shear stress of 0.54 Pa

Method: 1092

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.55 - Erosion rate at an excess shear stress of 0.55 Pa

Method: 1093

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.56 - Erosion rate at an excess shear stress of 0.56 Pa

Method: 1094

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.57 - Erosion rate at an excess shear stress of 0.57 Pa

Method: 1095

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.58 - Erosion rate at an excess shear stress of 0.58 Pa

Method: 1096

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.59 - Erosion rate at an excess shear stress of 0.59 Pa

Method: 1097

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.61 - Erosion rate at an excess shear stress of 0.61 Pa

Method: 1098

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.62 - Erosion rate at an excess shear stress of 0.62 Pa

Method: 1099

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.63 - Erosion rate at an excess shear stress of 0.63 Pa

Method: 1100

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.64 - Erosion rate at an excess shear stress of 0.64 Pa

Method: 1101

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.66 - Erosion rate at an excess shear stress of 0.66 Pa

Method: 1102

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.67 - Erosion rate at an excess shear stress of 0.67 Pa

Method: 1103

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.68 - Erosion rate at an excess shear stress of 0.68 Pa

Method: 1104

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.69 - Erosion rate at an excess shear stress of 0.69 Pa

Method: 1105

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.72 - Erosion rate at an excess shear stress of 0.72 Pa

Method: 1106

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.73 - Erosion rate at an excess shear stress of 0.73 Pa

Method: 1107

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.74 - Erosion rate at an excess shear stress of 0.74 Pa

Method: 1108

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.75 - Erosion rate at an excess shear stress of 0.75 Pa

Method: 1109

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.77 - Erosion rate at an excess shear stress of 0.77 Pa

Method: 1110

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.78 - Erosion rate at an excess shear stress of 0.78 Pa

Method: 1111

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.80 - Erosion rate at an excess shear stress of 0.8 Pa

Method: 1112

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.81 - Erosion rate at an excess shear stress of 0.81 Pa

Method: 1113

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.82 - Erosion rate at an excess shear stress of 0.82 Pa

Method: 1114

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.83 - Erosion rate at an excess shear stress of 0.83 Pa

Method: 1115

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.84 - Erosion rate at an excess shear stress of 0.84 Pa

Method: 1116

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.85 - Erosion rate at an excess shear stress of 0.85 Pa

Method: 1117

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.88 - Erosion rate at an excess shear stress of 0.88 Pa

Method: 1118

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.89 - Erosion rate at an excess shear stress of 0.89 Pa

Method: 1119

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.90 - Erosion rate at an excess shear stress of 0.9 Pa

Method: 1120

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.92 - Erosion rate at an excess shear stress of 0.92 Pa

Method: 1121

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.94 - Erosion rate at an excess shear stress of 0.94 Pa

Method: 1122

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.97 - Erosion rate at an excess shear stress of 0.97 Pa

Method: 1123

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.99 - Erosion rate at an excess shear stress of 0.99 Pa

Method: 1124

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.00 - Erosion rate at an excess shear stress of 1 Pa

Method: 1125

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.01 - Erosion rate at an excess shear stress of 1.01 Pa

Method: 1126

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.03 - Erosion rate at an excess shear stress of 1.03 Pa

Method: 1127

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.04 - Erosion rate at an excess shear stress of 1.04 Pa

Method: 1128

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.06 - Erosion rate at an excess shear stress of 1.06 Pa

Method: 1129

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.08 - Erosion rate at an excess shear stress of 1.08 Pa

Method: 1130

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.09 - Erosion rate at an excess shear stress of 1.09 Pa

Method: 1131

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.11 - Erosion rate at an excess shear stress of 1.11 Pa

Method: 1132

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.12 - Erosion rate at an excess shear stress of 1.12 Pa

Method: 1133

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.15 - Erosion rate at an excess shear stress of 1.15 Pa

Method: 1134

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.16 - Erosion rate at an excess shear stress of 1.16 Pa

Method: 1135

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.17 - Erosion rate at an excess shear stress of 1.17 Pa

Method: 1136

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.18 - Erosion rate at an excess shear stress of 1.18 Pa

Method: 1137

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.19 - Erosion rate at an excess shear stress of 1.19 Pa

Method: 1138

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.20 - Erosion rate at an excess shear stress of 1.2 Pa

Method: 1139

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.23 - Erosion rate at an excess shear stress of 1.23 Pa

Method: 1140

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.25 - Erosion rate at an excess shear stress of 1.25 Pa

Method: 1141

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.35 - Erosion rate at an excess shear stress of 1.35 Pa

Method: 1142

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.37 - Erosion rate at an excess shear stress of 1.37 Pa

Method: 1143

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.40 - Erosion rate at an excess shear stress of 1.4 Pa

Method: 1144

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.41 - Erosion rate at an excess shear stress of 1.41 Pa

Method: 1145

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.45 - Erosion rate at an excess shear stress of 1.45 Pa

Method: 1146

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.46 - Erosion rate at an excess shear stress of 1.46 Pa

Method: 1147

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.54 - Erosion rate at an excess shear stress of 1.54 Pa

Method: 1148

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.69 - Erosion rate at an excess shear stress of 1.69 Pa

Method: 1149

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.72 - Erosion rate at an excess shear stress of 1.72 Pa

Method: 1150

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.73 - Erosion rate at an excess shear stress of 1.73 Pa

Method: 1151

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.81 - Erosion rate at an excess shear stress of 1.81 Pa

Method: 1152

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.82 - Erosion rate at an excess shear stress of 1.82 Pa

Method: 1153

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.84 - Erosion rate at an excess shear stress of 1.84 Pa

Method: 1154

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.85 - Erosion rate at an excess shear stress of 1.85 Pa

Method: 1155

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.88 - Erosion rate at an excess shear stress of 1.88 Pa

Method: 1156

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.89 - Erosion rate at an excess shear stress of 1.89 Pa

Method: 1157

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.90 - Erosion rate at an excess shear stress of 1.9 Pa

Method: 1158

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET1.98 - Erosion rate at an excess shear stress of 1.98 Pa

Method: 1159

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.00 - Erosion rate at an excess shear stress of 2 Pa

Method: 1160

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.04 - Erosion rate at an excess shear stress of 2.04 Pa

Method: 1161

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.15 - Erosion rate at an excess shear stress of 2.15 Pa

Method: 1162

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.18 - Erosion rate at an excess shear stress of 2.18 Pa

Method: 1163

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.27 - Erosion rate at an excess shear stress of 2.27 Pa

Method: 1164

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.30 - Erosion rate at an excess shear stress of 2.3 Pa

Method: 1165

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.33 - Erosion rate at an excess shear stress of 2.33 Pa

Method: 1166

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.34 - Erosion rate at an excess shear stress of 2.34 Pa

Method: 1167

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.39 - Erosion rate at an excess shear stress of 2.39 Pa

Method: 1168

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.49 - Erosion rate at an excess shear stress of 2.49 Pa

Method: 1169

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.55 - Erosion rate at an excess shear stress of 2.55 Pa

Method: 1170

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.70 - Erosion rate at an excess shear stress of 2.7 Pa

Method: 1171

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.84 - Erosion rate at an excess shear stress of 2.84 Pa

Method: 1172

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.85 - Erosion rate at an excess shear stress of 2.85 Pa

Method: 1173

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.87 - Erosion rate at an excess shear stress of 2.87 Pa

Method: 1174

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.95 - Erosion rate at an excess shear stress of 2.95 Pa

Method: 1175

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.00 - Erosion rate at an excess shear stress of 3 Pa

Method: 1176

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.10 - Erosion rate at an excess shear stress of 3.1 Pa

Method: 1177

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.14 - Erosion rate at an excess shear stress of 3.14 Pa

Method: 1178

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.15 - Erosion rate at an excess shear stress of 3.15 Pa

Method: 1179

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.25 - Erosion rate at an excess shear stress of 3.25 Pa

Method: 1180

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.33 - Erosion rate at an excess shear stress of 3.33 Pa

Method: 1181

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.50 - Erosion rate at an excess shear stress of 3.5 Pa

Method: 1182

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.74 - Erosion rate at an excess shear stress of 3.74 Pa

Method: 1183

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.75 - Erosion rate at an excess shear stress of 3.75 Pa

Method: 1184

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.84 - Erosion rate at an excess shear stress of 3.84 Pa

Method: 1185

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET3.93 - Erosion rate at an excess shear stress of 3.93 Pa

Method: 1186

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET4.05 - Erosion rate at an excess shear stress of 4.05 Pa

Method: 1187

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET4.30 - Erosion rate at an excess shear stress of 4.3 Pa

Method: 1188

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET4.40 - Erosion rate at an excess shear stress of 4.4 Pa

Method: 1189

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET4.41 - Erosion rate at an excess shear stress of 4.41 Pa

Method: 1190

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET4.45 - Erosion rate at an excess shear stress of 4.45 Pa

Method: 1191

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET5.00 - Erosion rate at an excess shear stress of 5 Pa

Method: 1192

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET5.33 - Erosion rate at an excess shear stress of 5.33 Pa

Method: 1193

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET5.90 - Erosion rate at an excess shear stress of 5.9 Pa

Method: 1194

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET0.86 - Erosion rate at an excess shear stress of 0.86 Pa

Method: 1195

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: ERET2.82 - Erosion rate at an excess shear stress of 2.82 Pa

Method: 1196

Matrix: US - Unfractionated

Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which

projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).

Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2

Sample Handling

Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None

Separation: None Procedure description:

Parameter: BDENS - Bulk density

Method: 1197

Matrix: US - Unfractionated

Unit: g/cm3 Description: Analysed using the GEOTEK Multi Sensor Core Logger (MSCL) of the

University of Amsterdam. The density (Cs137 with energies principally at 0.662 MeV) was measured on whole-round sections.

Analytical Lab: TNO, Bouw en Ondergrond (TNO) Significant Nrs:

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSVFSAND - Grain size volume fraction range > 63 and < 2000 micron (sand)

Method: 1198

Matrix: FS - Fractionated

Unit: % Description: Sediment particle-size analyses were performed on the subsamples

using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs: 2

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSVFSAND - Grain size volume fraction range > 63 and < 2000 micron (sand)

Method: 1198

Matrix: FS - Fractionated

Unit: % Description: Sediment particle-size analyses were performed on the subsamples

using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs: 2

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSVFCLAY - Grain size volume fraction < 63 micron (silt/clay)

Method: 1199

Matrix: FS - Fractionated

Unit: % Description: Sediment particle-size analyses were performed on the subsamples

using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs: 2

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSVFCLAY - Grain size volume fraction < 63 micron (silt/clay)

Method: 1199

Matrix: FS - Fractionated

Unit: % Description: Sediment particle-size analyses were performed on the subsamples

using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs: 2

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSMEA - Mean grain size

Method: 1200

Matrix: US - Unfractionated

Unit: µm Description: Sediment particle-size analyses were performed on the subsamples

using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs: 2

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSMEA - Mean grain size

Method: 1200

Matrix: US - Unfractionated

Unit: µm Description: Sediment particle-size analyses were performed on the subsamples

using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs: 2

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSSKEW - Grain size skewness

Method: 1201

Matrix: US - Unfractionated

Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on

the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs:

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSSKEW - Grain size skewness

Method: 1201

Matrix: US - Unfractionated

Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on

the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs:

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSSORT - Grain size sorting

Method: 1202

Matrix: FS - Fractionated

Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on

the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs:

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: GSSORT - Grain size sorting

Method: 1202

Matrix: FS - Fractionated

Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on

the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.

Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs:

Sample Handling

Seqno: 153 Preservation: Kept at room temperature Pretreatment: None

Separation: None Procedure description: Samples were stored vertically.

Parameter: NTRZ - Nitrate + Nitrite (-N)

Method: 1203

Matrix: DI - Dissolved

Unit: µmol/l Description: Colorimetry.

Analytical Lab: VUB, Laboratorium voor Analytische en Milieuchemie (ANCH) Significant Nrs: 2

Sample Handling

Seqno: 39 Preservation: Kept in deep-freeze (-18 C) Pretreatment: None

Separation: PC filter (0.6 µm) Procedure description:

Parameter: NTRZ - Nitrate + Nitrite (-N)

Method: 1203

Matrix: DI - Dissolved

Unit: µmol/l Description: Colorimetry.

Analytical Lab: Vrije Universiteit Brussel, Laboratory of Analytical and Environmental Chemistry (ANCH)

Significant Nrs: 2 Sample Handling

Seqno: 39 Preservation: Kept in deep-freeze (-18 C) Pretreatment: None

Separation: PC filter (0.6 µm) Procedure description:

Parameter: DENSV - Density per unit of volume

Method: 1204

Matrix: NA - Not applicable

Unit: 10e3 coc/l Description: Inverted microscopy. Cell densities of colonial cells are counted.

Analytical Lab: Université Libre de Bruxelles, Ecology of Aquatic systems (ESA) Significant Nrs: 1

Sample Handling

Seqno: 110 Preservation: Cooled (4 C), dark Pretreatment: Lugol-Glutaraldehyde (1 % final concentration)

Separation: Unfiltered Procedure description: Concentration by Utermöhl method. The samples were analysed 1-3 months after sampling.

Parameter: DENSV - Density per unit of volume

Method: 1204

Matrix: NA - Not applicable

Unit: 10e3 coc/l Description: Inverted microscopy. Cell densities of colonial cells are counted.

Analytical Lab: ULB, Ecologie des Systèmes Aquatiques (ESA) Significant Nrs: 1

Sample Handling

Seqno: 110 Preservation: Cooled (4 C), dark Pretreatment: Lugol-Glutaraldehyde (1 % final concentration)

Separation: Unfiltered Procedure description: Concentration by Utermöhl method. The samples were analysed 1-3 months after sampling.