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A simplified hillslope erosion model with vegetation elements for practical applications

机译:实际应用的简化植被植被坡面侵蚀模型

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Soil and water conservation practices are increasingly being considered for curbing non-point source pollution from agricultural land. Several studies have demonstrated that stream power is a simple and good predictor of soil detachment and transport and can be used to predict the effect of soil and water conservation practices on soil loss. Our objective was, therefore, to develop a simple water erosion simulation model that is physically based on stream power, handles vegetation in terms of contact cover, and considers the settling velocity characteristics of the eroding sediment. The model assumes that rill flow can occur on hillslope segments with net erosion, but on segments with net deposition sheet flow is assumed. Input parameters include the depositability of the soil, rill shape, rill density, net precipitation, and an empirical power function describing the decrease of sediment concentration with vegetative cover increase. The model was evaluated by comparison of predicted and observed relationships between sediment concentration, slope, and vegetative residue cover in two experimental studies using simulated rainfall: one that involved erosion plots with various uniform slopes and levels of vegetative cover, and another that involved the observation of soil movement on mechanically shaped concave, uniform, and convex slopes with negligible vegetation. Without calibration, the model appeared to represent soil erosion relationships observed in these studies and is simple enough to be included in grid-based variable source hydrology models. (C) 2002 Elsevier Science B.V. All rights reserved. [References: 36]
机译:人们越来越多地考虑采用水土保持措施来抑制农业用地的面源污染。多项研究表明,流能是土壤脱离和运输的简单而又很好的预测因子,可用于预测水土保持措施对土壤流失的影响。因此,我们的目标是建立一个简单的水蚀模拟模型,该模型物理上基于水流功率,以接触覆盖率处理植被,并考虑侵蚀性沉积物的沉降速度特征。该模型假设在具有净侵蚀的山坡段上可能发生钻探流,但是假设具有沉积片状流的段上发生钻探。输入参数包括土壤的可沉积性,小溪的形状,小溪的密度,净降水量,以及经验功率函数,该函数描述了随着植被覆盖度的增加,沉积物浓度降低。在两项使用模拟降雨的实验研究中,通过比较沉积物浓度,坡度和植物残渣覆盖率之间的预测关系和观察关系,对模型进行了评估:一个涉及坡度和植被覆盖度均一的侵蚀图,另一个涉及观测值在植被形状可忽略的机械形状的凹凸,均匀和凸起斜坡上的土壤运动未经校准,该模型似乎代表了在这些研究中观察到的土壤侵蚀关系,并且足够简单,可以包含在基于网格的可变源水文模型中。 (C)2002 Elsevier Science B.V.保留所有权利。 [参考:36]

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