首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Time and Spatial Variation Features of Sediment Yield Intensity on the Loess Plateau
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Time and Spatial Variation Features of Sediment Yield Intensity on the Loess Plateau

机译:黄土高原沉积物强度的时空变化特征。

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摘要

Based on the distribution of hydrological stations and it's observation series of sediment information, and the different soil erosion type areas on the loess Plateau, the study area was divided into 292 soil erosion units. The time and spatial variation of sediment yield intensities on the loess plateau were analyzed. The results are showed that sediment intensities have changed evidently because of rainfall factor and the effects of soil and water conservation, and the sediment area with erosion modulus > 10,000t/(km~2 · a) reduced rapidly. And taking sediment yield intensity > 10,000t/(km~2 · a) as a criterion, there are 7 sediment yield centers on the Loess Plateau.
机译:根据黄土高原水文站的分布及其泥沙信息观测序列,以及黄土高原土壤侵蚀类型不同的区域,将研究区分为292个土壤侵蚀单元。分析了黄土高原沉积物产量强度的时空变化。结果表明,由于降雨因素和水土保持的影响,沉积物强度发生了明显变化,侵蚀模量> 10,000t /(km〜2·a)的沉积物面积迅速减少。以黄土高原产沙强度> 10,000t /(km〜2·a)为标准,黄土高原地区有7个产沙中心。

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