Onshore sediment transport on a sandy beach under varied wave conditions: Flow velocity skewness, wave asymmetry or bed ventilation?

被引:29
作者
Austin, Martin [1 ]
Masselink, Gerhard [2 ]
O'Hare, Tim [1 ]
Russell, Paul [1 ]
机构
[1] Univ Plymouth, Sch Earth Ocean & Environm Sci, Plymouth PL4 8AA, Devon, England
[2] Univ Plymouth, Sch Geog, Plymouth PL4 8AA, Devon, England
基金
英国自然环境研究理事会;
关键词
suspended sediment; cross-shore transport; flow velocity acceleration; bed ventilation; flow velocity skewness; flow velocity asymmetry; macrotidal beach; SWASH INFILTRATION-EXFILTRATION; OPTICAL BACKSCATTER SENSORS; SHEET FLOW; INNER-SURF; ZONE; DYNAMICS; GENERATION; MORPHOLOGY; EVOLUTION; FLUXES;
D O I
10.1016/j.margeo.2009.01.001
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Measurements of the cross-shore suspended sediment flux obtained from a planar and barred beachface have been used to investigate the propensity for wave-driven onshore sediment transport during medium energy conditions. Three processes capable of transporting sediments onshore-flow velocity skewness, wave asymmetry and bed-ventilation were investigated to determine their relative importance. Onshore-directed flow accelerations under the steep front face of asymmetric waves were significantly correlated with sediment suspension, whilst the effects of flow skewness and bed-ventilation were discounted. An acceleration-modified form of the Meyer-Peter-type formula is used as initial attempt at modelling the onshore transport using a temporal filter to modify the bed shear stresses. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:86 / 101
页数:16
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