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Experimental study on soil erosion process on the slopes of different soils texture

机译:不同土壤纹理斜坡土壤侵蚀过程的实验研究

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Soil erosion on slope was one of the key points in soil erosion research. Soil texture was one important factors influencing soil erosion. By indoor runoff scouring experiments, runoff erosion characteristics on the slopes with two different soils were studied systematically to reveal the influence of soil texture on soil erosion on the slope. Results indicated that the sediment yield increased fluctuate with scouring time with one or two peak values in the process. The time of peak sediment concentration appeared in advance with the increase of runoff discharge; influence of runoff discharge on soil erosion was not linear, and critical runoff discharge existed; the finer the soil particle was, the bigger soil detachment ratio was. Based on shear stress and runoff energy consumption theory, relations between the detachment rate and runoff shear stress, runoff energy consumption were established separately. The results showed that the critical runoff shear stress and the critical runoff energy consumption of some runoff experiments were less than zero. In comparison, the soil erosion based on the runoff energy consumption theory has a better precision than shear stress, and was better in description soil erosion on the slope.
机译:坡度的土壤侵蚀是土壤侵蚀研究的关键之一。土壤纹理是影响土壤侵蚀的一个重要因素。通过室内径流冲洗实验,系统地研究了两种不同土壤的斜坡上的径流侵蚀特性,揭示了土壤纹理对坡面土壤侵蚀的影响。结果表明,沉积物产量增加了在该过程中具有一个或两个峰值的冲洗时间波动。峰值沉积物浓度的时间提前出现,随着径流排出的增加而出现;径流放电对土壤腐蚀的影响不是线性的,存在临界径流放电;土壤颗粒越细,土壤脱离率越大。基于剪切应力和径流能量消耗理论,分别建立了分离率和径流剪切应力的关系,径流能耗。结果表明,一些径流实验的临界径流剪切应力和临界径流能量消耗小于零。相比之下,基于径流能量消耗理论的土壤侵蚀具有比剪切应力更好的精度,并且在坡度的描述土壤侵蚀中更好。

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