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Weetwood Surface Water Training 10 January 2014 Geoff Waite

Weetwood Surface Water Training 10 January 2014 Geoff Waite

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Page 1: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Weetwood Surface Water Training

10 January 2014

Geoff Waite

Page 2: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Agenda

TOPIC TIME STAFF

Historical Background to Sewer Hydraulics 09.00 - 09.30 KB, AE, HE

Modified Rational Method 09.30 - 10.30 KB, AE, HE

Micro Drainage – Basic Tank/Pond 10.30 - 11.00 KB, HE

Micro Drainage – Flow Controls 11.00 - 11.30 KB, HE

Micro Drainage – Complex Controls 11.30 - 12.00 KB, CC, AE, HE

Lunch

Micro Drainage – Other SUDs Components 12.45 - 13.45 KB, CC, AE, HE

Micro Drainage – Cascade 13.45 - 14.15 KB, CC, AE, HE

Interception Losses and Long Term Storage 14.15 - 15.00 KB, CC, AE, HE

Break

Drainage Strategy and Deliverability 15.15 – 17.00 KB, CC, AE, HE, RE

Close

Page 3: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulic Calculations

Method Year

Lloyd Davies – Rational Method 1906

TRRL (Watkins) Method 1962

Wallingford Procedure 1981

InfoWorks 1996

Page 4: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Definitions

• Types of Sewerage System

• Separate Sewerage Systems

• Combined Sewerage Systems

• Partially Separate Sewerage Systems

• Ancillaries – overflows, pumping stations, attenuation tanks, dual manhole

• Standard Technical Committee Report 25 (STC25)

Page 5: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Lloyd Davies – Rational Method

• Put simply: flow = impermeable area multiplied by rainfall intensity

• Method originally developed to size pipes rather than to calculate flow rates

• Main difficulty is how to calculate the correct rainfall intensity to use in the analysis

• Provides only a peak flow (not a hydrograph)

Page 6: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Rational Method - Assumptions

• Rainfall - uniform intensity over whole catchment being analysed

• Pipes run full (i.e. storage, surcharge and flooding is ignored)

• The whole area upstream contributes to runoff at the location being analysed

Page 7: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Rational Method

Q = 2.78 * imp area * rainfall intensity

• 2.78 is a factor to calculate flows in litres/sec if the impermeable area is in hectares and the rainfall intensity is in mm/hr

• Flow is at a maximum when the whole area upstream just starts to contribute runoff at the point of consideration

• The time at which this occurs (which is different for every pipe in the network) is known as the Time of Concentration

Page 8: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulics - Background

Page 9: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulics – Background (1)

• Rational Method known to over estimate flows

• Key weaknesses – uniform rainfall intensity, using the whole catchment upstream of the point of analysis and ignoring storage available in the pipe system

• Other weaknesses include catchment shapes, unable to deal with surcharge and effect of any ancillaries

Be wary of carrier pipes with no impermeable areas

Page 10: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulics – Background (2)

• TRRL – introduced for design of pipes on motorways

• Computer Method running on mainframe computers

• Incorporated variable rainfall intensities, area/time diagrams and allowed for pipe storage

• Produces Hydrographs

• Shortcomings – could not analyse surcharge/flooding and no ancillary modelling available

Page 11: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulics – Background (3)

1981 – Wallingford Procedure (Four Main Volumes)

• Software – WASSP running on mainframes

• Utilised rainfall data from the 1975 Flood Studies Report and rainfall/runoff research for urban areas

• Separate inputs (RED, SSD) and models for rainfall, urban rainfall/runoff process, pipe analysis and ancillaries

• Pipe analysis included surcharge and flooding (although to a limited extent)

Page 12: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulics – Background (4)

• Modified Rational Method is Volume 4 – utilised the findings of the Wallingford Procedure

• Rainfall data and urban rainfall/runoff models were incorporated into the procedure

Page 13: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulics – Background (5)

• Circa 1990 - Wallingford software circa converted to run on a pc and called WALLRUS

• Weaknesses - pipe analysis was limited to dendritic systems and could not deal with reverse flows

• Intermediate software introduced circa 1994 to handle reverse flows and backwater effects – SPIDA

• Infoworks introduced circa 1996 – fully pc based

Page 14: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Sewer Hydraulics – Background (6)

• Infoworks is GIS Based information using STC25 Referencing

• Separate databases for nodes, links and area information

• New pipe analysis software based upon St Venant open channel flow equations (deal with reverse flows)

• Internationally applicable with different runoff models for different countries/catchments

• Dry Weather Flow (foul sewage) generator and Water Quality analysis

Page 15: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Modified Rational Method

Q = 2.78 * Cv * CR * i * A

• Cv is the volumetric runoff coefficient (proportion of rainfall which enters the pipe network)

• CR is a routing coefficient = 1.3

• i is rainfall intensity

• A is imp area

Page 16: Weetwood Surface Water Training 10 January 2014 Geoff Waite

MRM – Input Parameters

1. Site Areas (Impermeable and Permeable)

2. Rainfall (M5-60, ratio and SAAR)

3. Soil Type/Soil Index

4. Time of Entry

5. Time of Flow

Page 17: Weetwood Surface Water Training 10 January 2014 Geoff Waite

MRM – Derived Parameters

1. Time of Concentration = Time of Entry + Time of Flow

2. Urban Catchment Wetness Index (UCWI)

3. Percentage Impermeable Area (PIMP)

4. Percentage Runoff (Pr)

5. Cv

Page 18: Weetwood Surface Water Training 10 January 2014 Geoff Waite

MRM – Pr Equation

Pr = 0.829*PIMP + 25*SOIL + 0.078*UCWI - 20.7

• Cv = Pr / PIMP

• Limitations of the Pr equation

Page 19: Weetwood Surface Water Training 10 January 2014 Geoff Waite

MRM – Rainfall Calculation

• Rainfall intensity based upon the time of concentration

• Obtain the M5- 60 and rainfall ratio values

• Calculate M5-D (where D is the time of concentration) – using the Z1 coefficient

• Calculate MT-D rainfall depths (where T is return period)

• Determine appropriate rainfall intensities

Page 20: Weetwood Surface Water Training 10 January 2014 Geoff Waite

MRM - Spreadsheet

Example of using the Spreadsheet

Page 21: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Micro Drainage – Basic Tank/Pond

• Source Control Basic Principles

• Quick Storage Estimate

• Tank/Pond

Page 22: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Source Control – Basic Principles (1)

• Firstly, always sketch out the layout of the component including levels

• For any SUDs component there is:– Inflow – principally rainfall– One, two or three outflows

1. Infiltration2. Flow Control (primarily controls the filling of the

component)3. Overflow (when the storage is full)

There must be at least one outflow but all three can be used

Page 23: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Component

Rainfall

Control

Overflow

Infiltration (Sides/Base)

Component provides Storage

Typical SUDs Component

Page 24: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Source Control – Basic Principles (2)

For each SUDs component we need to define:

1. Global Variables – overview of inflow, component, controls, climate change

2. Rainfall - inflow

3. Area Time Diagram – impermeable areas

4. Details of the SUDs component itself

5. Details of Flow Controls/Overflows/Infiltration

Page 25: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Quick Storage Estimate

• Useful tool for quick calculation

• Provides estimated storage requirements with or without infiltration

• Provides results for a range of infiltration components

• Useful way to input data required for analysis

Page 26: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Basic Tank/Pond

Freeboard

Flow Control Outflow at Base

Pipe Inflow above max storage level

Design Fill Level

Page 27: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Basic Tank/Pond

• Adam to Continue

Page 28: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Micro Drainage – Flow Controls

• Orifice

• HydroBrake

• Weir

• Complex Control – more than one control

• ALL flow controls use a head/discharge relationship

• Can be lower than the base of the SUDs component

Page 29: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Flow Control - Orifice

0.0 10.0 20.0 30.0 40.0 50.0 60.0 70.00

0.2

0.4

0.6

0.8

1

1.2

1.4

1.6

Flow in litres/sec

Head

in m

Page 30: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Flow Control - Hydrobrake

• Self activating vortex with air core• Type MD1 Hydrobrake 210mm diameter• Type MD12 Hydrobrake, 272mm diameter

0.0 10.0 20.0 30.0 40.0 50.0 60.0 70.00

0.2

0.4

0.6

0.8

1

1.2

1.4

1.6

1.8

OrificeHydrobrake MD12Hydrobrake MD1

Flow in litres/sec

Head in m

Page 31: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Flow Control - Weir

Page 32: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Flow Control – Complex Control

• Two controls at different levels to satisfy 2 year, 30 year and 100y+cc flow rates

• Normally hydrobrake/orifice combination

Page 33: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Flow Control – Complex Control

• Lower control – hydrobrake for 2 year flow

• Higher control – normally orifice with soffit set at 2 year water level

• Hydrobrake and orifice pass forward 100y+cc flow when component is full

• Complex control builder – trial and error

• Analyse with SUDs component and check results for 2 year, 30 year and 100 year+cc flow rates

• Adjust as necessary (may need to adjust control and component)

Page 34: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Micro Drainage – SUDs Components

1. Soakaway - Lined and House

2. Permeable Paving

3. Cellular Storage

4. Swale

5. Pipe Storage

Page 35: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components – Lined Soakaway

• Comprises circular concrete manhole rings with holes• Constructed within a square excavation filled with porous stone• Infiltration at base and sides

Page 36: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components – House Soakaway

• Comprise a square excavation filled with porous stone• Typically one per house

Page 37: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components – Permeable Paving

CBPP (Concrete Block Permeable Paving)

Clay pavers

Permeable Macadam

Permeable Resin-bound

aggregate

Gravel

Grass paving

Permeable/No-fines concrete

Self-binding golden gravel

Page 38: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components – Permeable Paving

• Typically 600mm deep• 400mm porous stone, 200mm blocks• With or without infiltration• Consider longitudinal gradient

Design Fill Level

Porous Stone

Block Paving

Page 39: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components – Permeable Paving• Typically 600mm deep• 400mm porous stone, 200mm blocks / laying course• With or without infiltration• Consider longitudinal gradient

Grit not sand

Course graded aggregate

Page 40: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components – Cellular Storage

• Cellular Units typically 350mm or 660mm deep• Cover required – 500mm landscaped areas and

600mm to 1m depending on traffic loads• With or without infiltration• Consider longitudinal levels

Design Fill Level

Cover to Units

Units

Sound undisturbed earth or prepared subgrade

Coarse Sand/Gravel

Page 41: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components - Swale

Freeboard

Side Slopes 1 in 4Base Width (variable)

• Overall Depth typically 500mm• Freeboard 150mm• Consider Longitudinal Gradient

Page 42: Weetwood Surface Water Training 10 January 2014 Geoff Waite

SUDs Components – Pipe Storage

• Generally Source Control only applicable for simple pipe systems

• Manholes provide large storage volumes of storage (not accounted for in Source Control)

• Consider Longitudinal Gradient

Page 43: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Micro Drainage - Cascade

• Joining together one or more SUDs Components

• Components can be linked in a chain

• Multiple components can be connected to a single component

• The flow control and the overflow can link to a downstream Component

• Some components can have infiltration

• Non upstream components need not receive runoff from rainfall

• Relative levels between components are not considered (beware! because Source Control only analyses levels for individual components)

• Must be one outfall?

Page 44: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Cascade Example

Page 45: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Cascade Process

1. Design Individual SUDs components

2. Downstream Components – take account of upstream inputs and/or rainfall

3. Link together in cascade facility

4. Analyse

5. Review results and adjust downstream components and re-analyse

Page 46: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Interception Storage

• 50% of rainfall events < 5mm • No measurable runoff from greenfield areas• Runoff from a development takes place for virtually every

rainfall event - frequent discharges with polluted runoff• Interception storage - prevent any runoff from rainfall depths

up to 5mm. • Certain SuDS features such as swales and pervious pavements

provide runoff characteristics that reflect this behaviour

Page 47: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Long Term Storage

Vol = RD.A.10[ (α 0.8) + 1- (β.SPR) – SPR]

Where:

Vol = the extra runoff volume (m3) of development runoff over greenfield runoff

RD = rainfall depth for 100 year, 6 hour event (mm)

PIMP = Impermeable area as a percentage of total area

A = area of site (ha)

SPR = standard percentage runoff index for the soil type

= proportion of impermeable surface draining to network / receiving waterbody

= proportion of permeable surface draining to network / receiving waterbody

100

PIMP

100

PIMP

Page 48: Weetwood Surface Water Training 10 January 2014 Geoff Waite

100 year 6 hour

Rainfall Depth

Page 49: Weetwood Surface Water Training 10 January 2014 Geoff Waite

100 year 6 hour Rainfall Depth

Page 50: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Drainage Strategy Detail

• Pre-planning• Informing the masterplan - Opportunities & Constraints• Deliverability • SuDS & land take

• Planning • NPPF • Demonstrating a feasible solution• EA, LLFA / LPA and IDB requirements• Deliverability & flexibility for the detailed design

Page 51: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Detailed Design/Planning Conditions

• By this stage the development proposals (layout/site levels) are finalised

• The foul and SW pipe systems can be designed

• Use Micro Drainage Simulation to analyse the SW pipe network including controls

• Design Outputs – plans, long section, manhole drawings (with emphasis on the flow control manhole)

• Brief report

Page 52: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Storage – 1 in 30 year and 1 in 100 year plus climate change

• Is the pipe system to be adopted by the water company under a Section 24 agreement?

• If so, the pipe system must:– Run free (no surcharge) in the 1 in 2 year event– No flooding in the 1 in 30 year event

• Still cater for 100 year+cc flows on site

• Take account of flow control and/or restrictions

Page 53: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Pipe Storage/Conveyance

• Do pipes store the 30 year event?

• Flow control and/or restriction required to do this – some flooding may result

• Pipes can still contain the 30 year event even if rates are restricted to greenfield

• Need to consider the interaction between the pipe network and the SUDs components (s) which requires a Simulation model

Page 54: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Levels/Watercourse Interaction

• Claire

Page 55: Weetwood Surface Water Training 10 January 2014 Geoff Waite

Pipe Free Conveyance Systems

• Claire