植被覆盖对土壤侵蚀和径流沉积的影响

Ernesto H. Pedroza-Parga, M. Velásquez-Valle, A. Pedroza-Sandoval, I. Sánchez-Cohen, L. G. Yáñez-Chávez
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引用次数: 2

摘要

在干旱地区,土壤流失是由暴雨事件和径流的侵蚀能造成的。目的:量化不同类型的植被覆盖对土壤侵蚀和坡面流造成的土壤沉积的影响。方法:试验于2017年7月至9月进行,采用随机区组试验设计,3个重复。评价的处理分别是玉米收获残茬和缓冲草(Cenchrus ciliaris L.)播种(MHR + G)、玉米收获残茬和缓冲草播种(MHR)和对照(C)。结果:MHR + G处理比对照(58.6 t·ha-1)减少了44% (26.3 t·ha-1)的侵蚀。MHR + G和G的土壤沉积量分别为47.6和51.7 t·ha-1,而C的土壤沉积量为26.1 t·ha-1。本研究的局限性:所得结果适用于本研究的土壤和水条件。原创性:关于径流条件下土壤颗粒去除和沉积过程行为的技术和科学报道较少。结论:在坡面流条件下,移积土壤的层厚与土壤覆盖类型有关。MHR + G处理显著减少了土壤侵蚀,使其成为一种可行的替代方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The impact of vegetation cover on soil erosion and soil deposition due to runoff
Introduction: In arid regions, soil losses are caused by torrential rainfall events and by the erosive energy of runoff. Objectives: To quantify the impact of the use of different types of vegetation cover on soil erosion and soil deposition caused by overland flow. Methodology: The experiment was carried out from July to September 2017 under a randomized block experimental design with three replications. The treatments evaluated were maize harvest residues and buffel grass (Cenchrus ciliaris L.) sowing (MHR + G), maize harvest residues (MHR), buffel grass sowing (G), and the control (C). Results: The MHR + G treatment reduced erosion by 44 % (26.3 t·ha-1) compared to the control (58.6 t·ha-1). Soil deposition was 47.6 and 51.7 t·ha-1 with MHR + G and G, respectively, while in C was 26.1 t·ha-1. Limitations of the study: The results found are valid for the soil and water conditions of this study Originality: There are few technical and scientific reports on the behavior of soil particle removal and deposition processes under runoff conditions. Conclusions: The layer thickness of soil removed and deposited, under overland flow conditions, depends on the type of soil cover. The MHR + G treatment significantly reduced soil erosion, making it a viable alternative.
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