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Mathematical model of sediment and solute transport along slope land in different rainfall pattern conditions

机译:不同降雨模式条件下坡地沉积物的数学模型及斜坡土地

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Rainfall erosion is a major cause of inducing soil degradation, and rainfall patterns have a significant influence on the process of sediment yield and nutrient loss. The mathematical models developed in this study were used to simulate the sediment and nutrient loss in surface runoff. Four rainfall patterns, each with a different rainfall intensity variation, were applied during the simulated rainfall experiments. These patterns were designated as: uniform-type, increasing-type, increasing- decreasing -type and decreasing-type. The results revealed that changes in the rainfall intensity can have an appreciable impact on the process of runoff generation, but only a slight effect on the total amount of runoff generated. Variations in the rainfall intensity in a rainfall event not only had a significant effect on the process of sediment yield and nutrient loss, but also the total amount of sediment and nutrient produced, and early high rainfall intensity may lead to the most severe erosion and nutrient loss. In this study, the calculated data concur with the measured values. The model can be used to predict the process of surface runoff, sediment transport and nutrient loss associated with different rainfall patterns.
机译:降雨侵蚀是诱导土壤退化的主要原因,降雨模式对沉积物产量和营养损失的过程具有显着影响。本研究开发的数学模型用于模拟表面径流中的沉积物和营养损失。在模拟的降雨实验期间,应用了四种降雨量,每种有雨强度变化的降雨量。这些图案被指定为:均匀型,增加型,增加 - 减少 - 型和减少型。结果表明,降雨强度的变化可以对径流生成的过程具有明显的影响,但只对产生的径流总量略有影响。降雨事件中的降雨强度的变化不仅对沉积物产量和营养损失的过程产生了显着影响,而且产生的沉积物和营养素的总量,以及早期的降雨强度可能导致最严重的侵蚀和营养素失利。在本研究中,计算的数据同意测量值。该模型可用于预测与不同降雨模式相关的表面径流,沉积物传输和养分损失的过程。

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