Technical Papers
Jun 30, 2020

Numerical Simulation of Turbidity Current in Approach Channels with a Closed End

Publication: Journal of Waterway, Port, Coastal, and Ocean Engineering
Volume 146, Issue 5

Abstract

This study aims to gain insights into turbidity currents in approach channels with a closed end. A vertical two-dimensional numerical model was introduced, which considers the viscosity of sediment and assumes rheological behavior of the very near-bed layer. The dynamic propagation of the turbidity current, both before and after it reaches the closed end, was studied. It is found that before the turbidity current reaches the closed end, the velocity of the current head is unaffected by the length of the channel, while the velocity and height of the turbidity head are decreased along the channel. When the head reaches the wall, a surge and reverse flow occur. After a quasi-stable state has formed, results show that the speed of current along the channel decreases gradually to zero speed at the closed end. The current speed increases asymptotically with the initial sediment concentration toward a limiting value at high concentrations. The depth of the turbidity current is about 0.3–0.6 times the total depth. The sediment concentration is reasonably constant along the channel. The study deepens the understanding of turbidity currents in these special channels and provides theoretical guidance for engineering practice.

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Acknowledgments

The authors thank various people for their helpful suggestions given during this study. The authors also gratefully appreciate the financial support of the National Key R&D Program of China (Grant No. 2018YFC0407404), the China Scholarship Council (Grant Nos. 201808320127 and 201808320128), Science and Technology Program of the Ministry of Housing and Urban–Rural Development (Grant No. 2019-K-141), Entrepreneurial team of sponge City (Grant No. 2017R02002), Nanjing University of Information Science & Technology Research Foundation (Grant No. 2017r097), Open Research Foundation for Jiangsu Key Laboratory of Agricultural Meteorology, Nanjing University of Information Science & Technology(Grant No. JKLAM1701), and Meteorological Open Research Fund in Huai River Basin (Grant No. HRM201702).

Notation

The following symbols are used in this paper:
C
sediment concentration of the turbidity current (kg · m−3);
C0
sediment concentration at the position of density current formed (kg · m−3);
Cin
sediment concentration at the inlet (kg · m−3);
C¯
layer-averaged concentration of the turbidity current (kg · m−3);
d
sediment particle size (m);
Frini
densimetric Froude number at the initial stage;
g
reduced gravity acceleration = g(ρρw)/ρw;
g
gravity acceleration (m · s²);
H
total depth of model (m);
h
thickness of density current (m);
k
turbulence energy;
ks
parameter applied to describe the hindered settling of activated sludge;
L
length of the channel (m);
l
dimensionless length can be defined as l = (x − 1)/(L − 1);
p
static pressure (Pa);
q
inlet unit discharge (m2 · s−1);
qd
inlet unit discharge of the lower layer (m2 · s−1);
qs
sediment transport volume of single width (m2 · s−1);
qsd
sediment transport volume of the lower layer (m2 · s−1);
qsu
sediment transport volume of the upper layer (m2 · s−1);
qu
inlet unit discharge of the upper layer (m2 · s−1);
t
time (s);
U
average flow velocity along water depth (m · s−1);
U0
velocity at the position of density current formed (m · s−1);
Uini
velocity of turbidity current at the inlet (m · s−1);
u
velocity in the x-direction (m · s−1);
v
velocity in the y-direction (m · s−1);
vs
settling velocity (m · s−1);
W
dimensionless deposition rate = (qsdqsu)/qsd;
x
coordinate in the horizontal direction (m);
y
coordinate in the vertical direction (m);
γ
unit weight of turbid water (N · m−3);
γs
unit weight of sediment (N · m−3);
δ
distance from the bottom to the position where u becomes to be 0 (m);
ɛ
dissipation rate of turbulence energy;
λ1, λ2, λ3
parameters in settling equations, which related to the particle size, surface properties, iron characteristics;
μ
viscosity of clean water (kg · m−1 · s−1);
μp
plastic viscosity of turbid water (kg · m−1 · s−1);
ρ
mixture density of fluid (kg · m−3);
ρp
dry density of sediment (kg · m−3);
ρw
clean water density (kg · m−3);
σc
turbulent Schmidt number (–);
τb
yield stress in the Bingham method (kg · m−1 · s−2);
τij
shearing stress of turbid fluid (kg · m−1 · s−2);
υ
viscosity kinematic coefficient (m2 · s−1); and
υt
turbulent kinematic viscosity (m2 · s−1).

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Go to Journal of Waterway, Port, Coastal, and Ocean Engineering
Journal of Waterway, Port, Coastal, and Ocean Engineering
Volume 146Issue 5September 2020

History

Received: Oct 19, 2019
Accepted: Mar 26, 2020
Published online: Jun 30, 2020
Published in print: Sep 1, 2020
Discussion open until: Nov 30, 2020

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Authors

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Lecturer, School of Hydrology and Water Resources, Nanjing Univ. of Information Science & Technology, 219 Ningliu Rd., Nanjing 210044, China; Key Laboratory of Navigation Structure Construction Technology, Ministry of Transport, 225 Guangzhou Rd., Nanjing 210029, China. ORCID: https://orcid.org/0000-0002-6663-7341. Email: [email protected]
Professor, Nanjing Hydraulic Research Institute, 223 Guangzhou Rd., Nanjing 210029, China; Key Laboratory of Navigation Structure Construction Technology, Ministry of Transport, 225 Guangzhou Rd., Nanjing 210029, China (corresponding author). Email: [email protected]
Guoxiang Xuan [email protected]
Professor, Nanjing Hydraulic Research Institute, 223 Guangzhou Rd., Nanjing 210029, China; Key Laboratory of Navigation Structure Construction Technology, Ministry of Transport, 225 Guangzhou Rd., Nanjing 210029, China. Email: [email protected]
Bruce W. Melville, M.ASCE [email protected]
Professor, Dept. of Civil and Environmental Engineering, Univ. of Auckland, Private Bag 92019, Auckland 1142, New Zealand. Email: [email protected]
Graham H. Macky [email protected]
Professional Teaching Fellow, Dept. of Civil and Environmental Engineering, Univ. of Auckland, Private Bag 92019, Auckland 1142, New Zealand. Email: [email protected]

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