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TO BREACH OR NOT TO BREACH? SPIT DYNAMICS AND COASTAL MANAGEMENT

机译:违反或不违反?吐痰动力学和沿海管理

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The breaching of spits can have important consequences for subsequent spit evolution as well as flooding and siltation within estuaries. This paper describes an investigation into spit evolution and breach formation at East Head, Hampshire, UK. A multi-disciplinary approach was adopted which considered past coastal changes, sediment transport, geomorphological regime relationships and numerical modelling of sediment transport. Synthesising these results shows that East Head spit has had a long history of erosion (since at least 1842). This has arisen from decreasing longshore sediment supply following the development of a stable crenulate bay system between Selsey and Portsmouth. Spit recession has been closely associated with increases in the cross sectional area of the estuary mouth, which also has been brought about by the decreasing longshore sediment supply. In the future, erosion is likely to continue leading to the potential formation of a breach at the neck of the spit. Modelling indicates that a breach of 1.0m ODN depth could be kept open by tidal and wave action and that, if this breach deepened to 0.5m ODN, it would produce increases in siltation within the Harbour mouth. In the short term, the presence of rock armouring and gabions is likely to retard breach formation. The long term evolution of East Head is dependant on the sea defence strategy for the updrift frontage of West Wittering.
机译:违背唾液可能对河口内随后的吐流量和洪水和淤积产生重要影响。本文介绍了汉普郡,英国东部吐痰进化和突破形成的调查。采用了多学科方法,考虑了沿海变化,沉积物运输,地貌政权关系和沉积物运输的数值模型。综合这些结果表明,东部头部唾液具有悠久的侵蚀历史(自至少1842年)。在塞尔西和朴茨茅斯之间的稳定陈列湾制度发展之后,这从龙岸沉积物供应降低了这一点。吐痰经济衰退与河口口的横截面积的增加密切相关,这也被龙岸沉积物供应减少所带来。在未来,侵蚀可能会继续导致散步颈部突破的潜在形成。建模表明,潮汐和波浪动作可以保持突破1.0米的ODN深度,如果这种违约未加深到0.5米的ODN,则会产生港口嘴内的淤积增加。在短期内,岩石铠装和族的存在可能会延迟突发形成。东部的长期演变取决于西吹雾的膀胱前沿的海防战略。

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