Download presentation
Presentation is loading. Please wait.
1
Cross-shore sediment transport
Chang Hsien Kuo 國立交通大學土木工程學系 中華民國102年5月9日
2
cross- and long-shore sediment
3
beach profile vs. cross-shore sediment
4
beach profile vs. cross-shore sediment
5
depth of closure Hallermerier (1978, 1981) Birkemeier (1985)
annul mean significant wave height + standard deviation Birkemeier (1985)
6
cross-shore sediment transport
Madsen and Grant (1976): sediment transport for half wave period Watanabe et al. (1980): net sediment transport
7
cross-shore sediment transport
Sunamura (1982): Dominant sediment transport
8
Bar formation Keulegan (1945)
9
Bar formation Six types of longshore bars
10
Bar formation Keulegan (1945)
11
Bar formation Keulegan ratio=ht/hc ~1.69
12
Bar formation Nayak’s criterion for longshore bars:
Wave steepness (H/L) vs. wave height (H/h)
13
Bar formation Standing wave and wave reflection
14
Bar formation Partterns of secondary currents associated with different types of three dimensional longshore bar
15
Beach cusp Beach cusps were first described by Palmer (1834)
16
Beach cusp Cusp spacing is about one-half the wavelength of edge waves
17
transverse sand bars
18
transverse sand bars Ten years ( ) of time exposure vidieo images of nearshore region at Duck, NC were used to study transverse sand bars.
19
transverse sand bars Transverse bar spacing :
mean longshore current and beach slope Komar (1998)
20
transverse sand bars Predicted values were much less than the measured values
21
Bed shear stress
22
Bed shear stress
23
Bed shear stress Soulsby, 1997: free stream velocity
24
Bed shear stress Nielsen, 2002: shear velocity
25
Bed shear stress Dick and Sleath, 1991: Momentum-integral method
Sedimment/fluid mixture Dixen at al., 2008: Log-fit method (Law of the wall) The velocity profile can be approximated by a logrithmic function
26
Bed shear stress Phase lag fluctuation
27
Application to predict sand transport rate
Nielsen, 2006: Bedload formulation Momentum integral method Symbols : tests Top: skewness of shear stress Bottom: phase lead of shear stress to free stream velocity
28
Bed shear stress Four kinds of formulas for shear velocity
29
Recent study-1 Net transport rate : velocity-load equation
30
Recent study-1 Watanabe and Sato, 2004: Half-wave cycle
31
Recent study-1 Shields parameter
32
Recent study-1 Wave-current friction factor (Ribberink, 1998)
33
Recent study-1 Sediment load between half cycles: Phase lag parameter
34
Recent study-1
35
Recent study-1 For velocity-skewed oscillatory sheet flows with d > 0.2mm Data: 32 Goodness: R2:0.78 Fac2%:97% Fac5%:100%
36
Recent study-1 Data: 32 Goodness: R2:0.87 Fac2%:84% Fac5%:97%
For acceleration-skewed oscillatory sheet flows with d > 0.2mm Data: 32 Goodness: R2:0.87 Fac2%:84% Fac5%:97%
37
Recent study-1 Data: 29 Goodness: R2:0.80 Fac2%:86% Fac5%:93%
For oscillatory sheet flows with d < 0.2mm Data: 29 Goodness: R2:0.80 Fac2%:86% Fac5%:93%
38
Recent study-1 Data: 50 Goodness: R2:0.65 Fac2%:62% Fac5%:89%
For oscillatory sheet flows over rippled bed Data: 50 Goodness: R2:0.65 Fac2%:62% Fac5%:89%
39
Recent study-1 Data: 50 Goodness: R2:0.84 Fac2%:70% Fac5%:86%
For oscillatory sheet flows with colinear currents Data: 50 Goodness: R2:0.84 Fac2%:70% Fac5%:86%
40
Recent study-1 Steady sheet-flow
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.