Surfzone-Beach-Dune interactions: Flow and Sediment Transport across the Intertidal Beach and Backshore
Surfzone-Beach-Dune interactions: Flow and Sediment Transport across the Intertidal Beach and Backshore
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冲浪区-海滩-沙丘相互作用：潮间带海滩和后岸的水流和沉积物输送
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发表时间：
2016
期刊：
影响因子：
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通讯作者：
T. Smyth
中科院分区：
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作者：
P. Hesp;T. Smyth
帕特里克·赫斯普史密斯，T.A.G.，2016. Surfzone-海滩-沙丘相互作用：回顾;以及穿过潮间带海滩和后滨的水流和沉积物输运。In：Vila-Concejo，A.;布鲁斯，E.;肯尼迪，D.M.，和McCarroll，R.J.（eds.），第14届国际沿海研讨会论文集（澳大利亚悉尼）。《海岸研究杂志》，特刊，第75期，第8 -12页。椰子溪（佛罗里达），ISSN 0749-0208。最初的波浪-海滩-沙丘模型（Hesp，1982年）指出，从中长期来看，模态耗散海滩显示出最大的陆上波浪驱动沉积物输运、最大的海滩风成输运、最大的前沙丘高度和体积以及最大的全新世沙丘区。模态反射海滩显示相反，而模态中间海滩显示这些从相对较高到相对较低的泥沙输运，前沙丘体积和全新世屏障体积的趋势，从耗散到反射的趋势。本文提出的三种典型海滩的水流计算流体动力学（CFD）模型和输沙计算结果表明，有关风成沙输沙的原始概念和实测资料是正确的。耗散海滩表现出最大的长期潜力的沉积物输送到后滨，而反射海滩显示最少，从相对较高到较低的中间海滩状态范围内的趋势。
ABSTRACT Hesp, Patrick A. and Smyth, T.A.G., 2016. Surfzone-Beach-Dune interactions: Review; and flow and sediment transport across the intertidal beach and backshore. In: Vila-Concejo, A.; Bruce, E.; Kennedy, D.M., and McCarroll, R.J. (eds.), Proceedings of the 14th International Coastal Symposium (Sydney, Australia). Journal of Coastal Research, Special Issue, No. 75, pp.8–12. Coconut Creek (Florida), ISSN 0749-0208. The original wave-beach-dune model (Hesp, 1982) stated that in the medium to long term, modal dissipative beaches display maximum onshore wave driven sediment transport, maximum aeolian transport off beaches, the largest foredune heights and volumes, and the largest Holocene dunefields. Modal reflective beaches display the opposite, while modal intermediate beaches display a trend in these from relatively high to relatively low sediment transport, foredune volumes, and Holocene barrier volumes with a trend from dissipative to reflective. New Computational Fluid Dynamic (CFD) modelling of flow and calculation of sediment transport over three modal beach types presented here shows that the original conceptual ideas and field data regarding aeolian sediment transport are correct. Dissipative beaches show the greatest long term potential for sediment delivery to the backshore whilst reflective beaches display the least, with a trend from relatively high to low in the intermediate beach state range.