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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. cross- and long-shore sediment. beach profile vs. cross-shore sediment . beach profile vs. cross-shore sediment. depth of closure. Hallermerier (1978, 1981). - PowerPoint PPT Presentation
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Cross-shore sediment transportChang Hsien Kuo
10259
NRCESTcross- and long-shore sediment
beach profile vs. cross-shore sediment
beach profile vs. cross-shore sediment
depth of closureHallermerier (1978, 1981)
annul mean significant wave height + standard deviation
Birkemeier (1985)cross-shore sediment transportMadsen and Grant (1976): sediment transport for half wave period
Watanabe et al. (1980): net sediment transport
cross-shore sediment transportSunamura (1982): Dominant sediment transport
Bar formationKeulegan (1945)
Bar formationSix types of longshore bars
Bar formationKeulegan (1945)
Bar formationKeulegan ratio=ht/hc~1.69
Bar formationNayaks criterion for longshore bars:Wave steepness (H/L) vs. wave height (H/h)
Bar formationStanding wave and wave reflection
Bar formationPartterns of secondary currents associated with different types of three dimensional longshore bar
Beach cuspBeach cusps were first described by Palmer (1834)
Beach cuspCusp spacing is about one-half the wavelength of edge waves
transverse sand bars
transverse sand barsTen years (1987-1996) of time exposure vidieo images of nearshore region at Duck, NC were used to study transverse sand bars.
transverse sand barsTransverse bar spacing :mean longshore current and beach slope
Komar (1998)
transverse sand barsPredicted values were much less than the measured values
Bed shear stress
Bed shear stress
Bed shear stress
Soulsby, 1997: free stream velocity
23Bed shear stress
Nielsen, 2002: shear velocity
Bed shear stress
Dick and Sleath, 1991: Momentum-integral method
Sedimment/fluid mixtureDixen at al., 2008: Log-fit method (Law of the wall)The velocity profile can be approximated by a logrithmic function
Bed shear stress
Phase lagfluctuationApplication to predict sand transport rate
Nielsen, 2006: Bedload formulation
Momentum integral methodSymbols : testsTop: skewness of shear stressBottom: phase lead of shear stress to free stream velocityBed shear stress
Four kinds of formulas for shear velocityRecent study-1
Net transport rate : velocity-load equationRecent study-1
Watanabe and Sato, 2004:Half-wave cycleRecent study-1
Shields parameter
Recent study-1
Wave-current friction factor (Ribberink, 1998)
Recent study-1Sediment load between half cycles: Phase lag parameter
Phase lag parameterRecent study-1
Recent study-1
For velocity-skewed oscillatory sheet flows with d > 0.2mmData: 32Goodness:R2:0.78 Fac2%:97%Fac5%:100%Recent study-1For acceleration-skewed oscillatory sheet flows with d > 0.2mm
Data: 32Goodness:R2:0.87 Fac2%:84%Fac5%:97%Recent study-1
For oscillatory sheet flows with d < 0.2mmData: 29Goodness:R2:0.80 Fac2%:86%Fac5%:93%Recent study-1
For oscillatory sheet flows over rippled bedData: 50Goodness:R2:0.65 Fac2%:62%Fac5%:89%Recent study-1
For oscillatory sheet flows with colinear currentsData: 50Goodness:R2:0.84 Fac2%:70%Fac5%:86%Recent study-1Steady sheet-flow