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AEOLIAN TRANSPORT AND SANDY DESERTIFICATION IN SEMIARID CHINA:A WIND TUNNEL APPROACH

机译:半干旱地区的风沙运输和沙漠化:一种风洞方法

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摘要

By using surface samples collected in areas under high desertification risk in semiarid China, the roles of aeolian transport and the surface characteristics on sandy desertification were analysed. The results show that vegetation cover may not play the key role in the aeolian processes. However, the content of silt and clay decrease the aeolian transport rates even when the surfaces are moderately crushed. The low moisture content of the surface soils (< 1 %) did not play an important role in the aeolian transport rate. The intensity of aeolian transport was mainly determined by the availability of the erodible material. Considering that human activities may not result in the surfaces being completely crushed, moderate human activities may not trigger severe desertification.
机译:利用半干旱地区高荒漠化风险地区收集的地表样品,分析了风沙运输和地表特征在沙质荒漠化中的作用。结果表明,植被覆盖在风沙过程中可能没有起到关键作用。但是,即使表面被适度压碎,淤泥和粘土的含量也会降低风沙的输送速度。表层土壤的低水分含量(<1%)在风沙运输速率中没有发挥重要作用。风沙运输的强度主要取决于易蚀物质的可用性。考虑到人类活动可能不会导致表面完全被压碎,中等程度的人类活动可能不会引发严重的荒漠化。

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