暴雨内降雨分布对土壤侵蚀速率的影响

S. I. Ahmed, R. Rudra, Bahram Gharabaghi, K. Mackenzie, W. Dickinson
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引用次数: 16

摘要

本文探讨了暴雨事件中降雨时间分布模式对土壤侵蚀速率的影响,以及采用降雨侵蚀力模型的可能性。在1.0 m2的硅砂和壤土上,用降雨模拟器模拟不同的降雨分布模式,至少重复3次。结果表明,随着降雨强度的急剧增加,土壤侵蚀速率急剧上升,然后逐渐下降到稳定的侵蚀速率。瞬态效应导致振荡降雨分布的土壤侵蚀速率比具有相同持续时间和相同平均降雨强度的稳态降雨强度事件的土壤侵蚀速率高2倍以上。建立了基于过程的降雨侵蚀力测度的3参数和4参数雨功率模型。4参数模型与观测数据吻合较好,在所有降雨分布下对硅砂的土壤侵蚀速率预测较准确,对低强度降雨条件下壤土的土壤侵蚀速率预测较好。为了提高土壤侵蚀预测模型在更大范围降雨分布下的准确性,还需要进行更多的研究。
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Within-Storm Rainfall Distribution Effect on Soil Erosion Rate
This study investigates the effect of rainfall temporal distribution pattern within a storm event on soil erosion rate and the possibility of using rain power type model for rainfall erosivity. Various rainfall distribution patterns, simulated by rainfall simulator, were used on 1.0 m2 plot of silica sand and loam soil with a minimum of three replications. The results show that the soil erosion rates spiked following every sharp increase in rainfall intensity followed by a gradual decline to a steady erosion rate. Transient effects resulted in the soil erosion rates for an oscillatory rainfall distribution to be more than two fold higher than those obtained for a steady-state rainfall intensity event with same duration and same average rainfall intensity. The 3-parameter and 4-parameter rain power models were developed for a process-based measure of rainfall erosivity. The 4 parameter model yielded better match with the observed data and predicted soil erosion rates more accurately for silica sand under all rainfall distributions, and good results for loam soil under low intensity rainfall. More research is necessary to improve the accuracy of soil erosion prediction models for a wider range of rainfall distributions.
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Within-Storm Rainfall Distribution Effect on Soil Erosion Rate
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