沙漠中偶发地表径流的地貌印记

Q4 Social Sciences
A. Saleem, Islam El‑Desouky
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引用次数: 0

摘要

沙漠中的山洪虽然罕见,但具有显著的地貌影响。本文报道了2015年11月4日发生在埃及西部沙漠的山洪暴发。卫星图像处理、实地调查、近距离摄影测量和沉积物分析可以量化不同规模的洪水地貌影响。在Wadi An Natrun洼地,湖泊面积翻了一番,出现了数百个新的临时池塘。到第二年夏天,所有的池塘都干涸了,湖边变成了盐田。在局部范围内,四个详细的案例研究表明,同一山洪事件在冲沟形态、沉积物破坏或稳定性、从粘土到块体的沉积物大小输送以及扇体扩展方面对地貌的影响有多大。这种可变性取决于当地土壤的可蚀性,包括基岩异质性、土壤凝聚力和渗透性、植被覆盖和继承地形。形成短暂池塘和playa的有机泥浆可能为埃及西部沙漠过去的洪水事件提供了相关的沉积代理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geomorphological imprints of episodic surface runoff in deserts
Flash floods in desert, however they are rare, have significant geomorphic effects. The present paper reports the 4th November 2015 flash flood that occurred in the Western Desert of Egypt. Satellite images processing, field survey, close range photogrammetry and sediment analyses allow the quantification of flood geomorphologic impacts at different size scales. At Wadi An-Natrun depression, lake size doubled, hundreds of new ephemeral ponds appear. All ponds were dry by the next summer and lake margins were transformed into salt pans. At a local scale, four detailed case studies show how much geomorphic impacts of the same flash flood event vary in terms of gully morphology, sediment failure or stability, sediment size transport from clays to blocks and fan extension. This variability depends on local soil erodibility, including bedrock heterogeneity, soil cohesion and permeability, vegetation cover and inherited topography. Organic muds formed into ephemeral ponds and playa may provide a relevant sedimentary proxy for past flood events in the Western Desert of Egypt.
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来源期刊
Mediterranee
Mediterranee Social Sciences-Urban Studies
CiteScore
0.20
自引率
0.00%
发文量
18
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