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Fluid Mud Layer and Its Effects on the Hydrodynamics of Benthic Boundary Layers
Xiao Hua WangSchool of Geography and Oceanography
University of New South Wales@Australian Defence Force Academy
Canberra, Australia
1. Introduction
2. Model description2.1. Hydrodynamic model2.2. Sediment transport model
3. Experiment setup
4. Model results 4.1. Benchmark experiment4.2. Resuspension hysteresis—the nepheloid layer4.2.1. Sensitivity to Mellor-Yamada turbulent closure assumptions4.2.2. Effects of flocculation4.2.3. Effects of freshwater runoffs4.3. Hyperpicnal plume4.4. Bottom drag coefficient 4.5. Model sensitivity to vertical resolution
5. Summary and conclusions
Hydrodynamic model—Princeton Ocean Model with following new features: (1) C
s
ww )1(
(2) 2
0 ]/)ln()1/(
1[
zzH
ARC b
fd
where A=5.5 (Adams & Weatherly, 1981) and Rf is flux Richardson number Model forcing
22
22
2sin
2sin
SS
MM T
ta
T
ta
at x=60 km
where am2=0.4 m, as2=0.1 m, Tm2=12.42 hours and Ts2=12 hours
S e d i m e n t t r a n s p o r t m o d e l
C
t
x
uC
y( vC )
z
[ w w s C ] z
( K h
C
z) F C
Ez
CK h
a t z = - H
A c c o r d i n g t o A r i a t h u r a i & K r o n e ( 1 9 7 6 )
(12)
if )1(
if )1(0
cbc
bsb
cbc
b
wC
EE
E0=10-4 kg m-2 s-1, ws=-10-4 m s-1, c=0.02 N m-2
Setup of numerical experiments
Experiment )(C ws x10-4
(m s-1)
spring
(m)
R
(m3 s-1)
(zb+H)/z0
1a-1b C=0, C0 -1 0.5 0 100
2a-2b C0 -0.5, -2 0.5 0 100
3a-3b C=0, C0 -1 0.5 800 100
4a-4b C0 -1 0.4, 0.6 0 100
5a-5c C0 -0.5
0.5, 0.4,
0.6
0 100
6a-6b C=0, C0 -1 0.5 0 1000
7a-7b C=0, C0 -1 0.5 0 4000
Summary & conclusions This work describes exploratory numerical modelling
results of sediment transport processes in both neutrally and sediment-induced stratified tidal estuary. The focus was placed on description and prediction of the dynamics of a fluid mud layer developed in the estuary due to the coupling effect of the seawater and resuspended sediment concentration.
It can be concluded that the establishment of the fluid
mud layer in the BBL causes: 1) a significant reduction in the total sediment transport
along the estuary; 2) occurrence of resuspension hysteresis event that
forms a highly concentrated fluid-mud bottom wall layer;
3) variability in the bottom drag coefficient Cd.