runoff erosion

  • runoff erosion
  • 释义

    流水侵蚀

纠错 数据更新时间:2026-04-19 17:29:21
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The process that runoff and sediment material collect into the channel and migrate through the channel network is important in simulating the hydrological and erosion areas. And river confluence relations in the basin is the base of hydrological and erosion models.

径流和泥沙物质向沟道的汇集和通过沟道网络系统的运移过程,是水文和侵蚀模拟的重要环节,而流域之间汇流关系的建立,则是流域水文和侵蚀模型的基础。

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In this article the authors studied the law of soil erosion under different cultivated models and slopes on 6-21 ° red soil sloping fields with the method of runoff plot The result showed that the amount of soil erosion could be decreased by 70-80% on terrace land;

在6~21°的红壤坡地上,采用径流小区法研究不同耕作模式和坡度下水土流失的规律。结果表明:梯地可以减少土壤侵蚀量70-80%;

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4、

Both runoff erosion and splash erosion in rills is calculated at the same time when its runoff is less then 6 mm.

当坡面细沟水流平均深度小于6mm时,在细沟内同时进行水流侵蚀和降雨溅蚀的计算。

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Under the condition of same slope steepness and runoff, sediment delivery caused by rainfall erosion is bigger than that caused by feeding runoff washing. Sediment delivery has increased by 50% when rainfall intensity increases 1 time.

在坡度一致和坡面径流量基本相同时,降雨侵蚀产沙量大于供水径流的侵蚀产沙量,降雨强度增大1倍时,坡面侵蚀产沙量增大约50%;

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Since Xia and Shang dynasties, the human agricultural cultivation activities affected the surface of pluvial-alluvial fan and promoted the slope runoff erosion and deposit process.

自夏商时代以来,农业耕垦活动影响古洪积扇地表,促进了坡面流水侵蚀堆积过程,发生了面状流水侵蚀;

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Evaluating the measuring methods to sediment concentration in the runoff of slope erosion

坡面侵蚀中径流含沙量测量方法研究与展望

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Under the experimental condition, splash erosion of slope surface and sediment of runoff have good linear relationship.

相同雨强、坡度、时间段下,坡面溅蚀与径流泥沙二者速率之间有着较好的线性关系。

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Influence of slope gradient on runoff erosion of purple soil slope in the Three Gorges Reservoir area

坡度对三峡库区紫色土坡面径流侵蚀的影响分析

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11、

A dual box system ( one is rill box and the other is feeder box) with 15 gradient and clay loess is used to quantify effects of runoff and sediment from up slope on down slope rill erosion and sediment under different sediment concentrations and rainfall intensities.

利用双土槽系统径流小区(供沙土槽和试验土槽),定量研究了不同上方来水含沙量和不同降雨强度下15°坡面上方来水来沙对坡下方细沟侵蚀产沙过程的影响。

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Dividing out four drainage basins, and on the basis of the achievement of three water changes, applying runoff coefficient formula from ShanDong water conservancy's academy and USLE, respectively counting and assessment in average surface runoff average supply to groundwater and average soil erosion;

划分出四个小流域,根据三水转化研究成果,采用山东省水科院变径流系数经验公式法和美国通用水土流失方程,分别对该地多年平均地表径流、地下水补给和水土流失进行计算评价;

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