首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Rapid assessment of field erosion and sediment transport pathways in cultivated catchments after heavy rainfall events
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Rapid assessment of field erosion and sediment transport pathways in cultivated catchments after heavy rainfall events

机译:快速评估暴雨后耕作流域的田间侵蚀和泥沙输送路径

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摘要

This paper explores a scale-adapted erosion mapping method which aims at a rapid assessment of field erosion and sediment transport pathways in catchments up to several square kilometres and compares the results with the output of a well-known erosion model (LISEM). The mapping method is based on an event-defined classification scheme of erosion intensity (zero, weak, moderate and strong) that is applied to arable fields, in combination with incision measurements of erosion features for each erosion intensity class on a small sample of fields. Sediment deposition is classified on the basis of quantity indicators and abundance. In addition, relevant conditions and erosion factors are determined for each field.The method was applied to an agricultural catchment (4-2 km(2)) in the Sundgau (Alsace), after a short but violent thunderstorm in May 2001, to illustrate its potential use and its limitations. The rainfall event led to strong erosion on the arable fields and a muddy flow that caused significant damage in the built-up area. On the basis of the analyses of the incision measurements in combination with the mapping of erosion intensity classes, total erosion for the catchment was estimated as 15 000 t (an average of about 36 t/ha). Sediment deposition was found to occur in three major locations: (1) in thalwegs at the interface between maize and downslope winter wheat fields, (2) in downslope headlands where the flow direction suddenly changed due to oriented tillage structures in the perpendicular direction, and (3) the lowest corners of fields which collect all the runoff from the field. Preliminary data analyses suggest that erosion intensity is related to field size and/or tillage direction and to slope morphology. Model output (LISEM) appeared to depend more strongly on slope gradient than the results obtained with the mapping method.The method yields a database, which can be used as a foundation for conservation strategies in small regions with similar land use and geomorphology. The mapping and modelling methods are compared, and their complementary aspects are highlighted. Copyright (C) 2005 John Wiley Sons, Ltd.
机译:本文探索了一种适应规模的侵蚀测绘方法,旨在快速评估长达数平方公里的流域的田间侵蚀和泥沙输送路径,并将结果与​​著名的侵蚀模型(LISEM)进行比较。该映射方法基于适用于耕地的侵蚀强度(零,弱,中和强)的事件定义分类方案,并结合了对一小块田地上每种侵蚀强度类别的侵蚀特征的切口测量。根据数量指标和丰度对沉积物进行分类。此外,还确定了每个油田的相关条件和侵蚀因子。该方法在2001年5月发生短暂但猛烈的雷暴天气后,被用于Sundgau(阿尔萨斯)的一个农业流域(4-2 km(2)),以说明它的潜在用途及其局限性。降雨事件导致耕地受到严重侵蚀,泥泞的水流对建成区造成了严重破坏。在对切口测量结果进行分析并结合侵蚀强度等级图的基础上,该流域的总侵蚀量估计为15000吨(平均约36吨/公顷)。发现沉积物沉积发生在三个主要位置:(1)在玉米和下坡冬麦田之间的交界处的thalwegs;(2)在下坡岬角,由于垂直耕作结构定向,流向突然改变;以及(3)田地的最低角,从田地收集所有径流。初步数据分析表明,侵蚀强度与耕地面积和/或耕作方向以及坡度形态有关。模型输出(LISEM)似乎比通过映射方法获得的结果更依赖于坡度,该方法产生了一个数据库,该数据库可以用作土地用途和地貌相似的小区域保护策略的基础。比较了映射和建模方法,并突出了它们的互补方面。版权所有(C)2005 John Wiley Sons,Ltd.

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