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岩石海岸过程:特别提及软岩悬崖的后退

Rocky coast processes: with special reference to the recession of soft rock cliffs.

作者信息

Sunamura Tsuguo

机构信息

Professor Emeritus, Osaka University.

出版信息

Proc Jpn Acad Ser B Phys Biol Sci. 2015;91(9):481-500. doi: 10.2183/pjab.91.481.

Abstract

Substantial progress in research on the recession of coastal cliffs composed of soft materials has been made in recent years and data with higher accuracy have been accumulated. This paper provides the state of the art review in the recession studies and highlights two new findings obtained from the reanalysis of existing data. The review topics are: episodic and localized nature of cliff recession; the development of cliffline; the relationship between cliff height and recession rate; mechanisms of cliff toe erosion by waves; a fundamental equation for wave-induced toe erosion; factors controlling toe erosion; and slope instabilities and mass movements. The findings are presented on (1) the temporal change in cliffline recession mode and (2) the effect of beach sediment at the cliff base on the cliff erosion.

摘要

近年来,在由软质材料构成的海岸悬崖后退研究方面取得了重大进展,并积累了更高精度的数据。本文对悬崖后退研究的现状进行了综述,并突出了对现有数据重新分析后获得的两项新发现。综述主题包括:悬崖后退的间歇性和局部性特征;悬崖线的演变;悬崖高度与后退速率之间的关系;波浪对悬崖底部的侵蚀机制;波浪引起的底部侵蚀基本方程;控制底部侵蚀的因素;以及边坡失稳和块体运动。研究结果涉及(1)悬崖线后退模式的时间变化,以及(2)悬崖底部海滩沉积物对悬崖侵蚀的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b78e/4754505/a81482e5c845/pjab-91-481-g001.jpg

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