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作 者:Lianyou Liu Jianhua Wang Xiaoyan Li Yuzhang Liu Wanquan Ta Haimei Peng
机构地区:[1]Chinese Acad Sci, Desert Res Inst, Lanzhou 730000, Peoples R China [2]Lanzhou Univ, Dept Geog Sci, Lanzhou 730000, Peoples R China
出 处:《Chinese Science Bulletin》1998年第19期1646-1651,共6页
基 金:ThisworkwassupportedbytheNationalNaturalScienceFoundationofChina (GrantNo .4940 10 10 )andtheChineseAcademyofSciences
摘 要:The erodible particle size distribution, diameter range and separate content of three soils from semi-arid regions of China were determined at different wind velocities through wind tunnel simulation and dry sieving. It was demonstrated that soil erodibility by wind depends not only on the intrinsic soil properties, but also on the extrinsic erosion effect of the erosive winds. It was supposed that there existed general consistency in the mechanics of wind erosion on different soils.The erodible particle size distribution, diameter range and separate content of three soils from semi-arid regions of China were determined at different wind velocities through wind tunnel simulation and dry sieving. It was demonstrated that soil erodibility by wind depends not only on the intrinsic soil properties, but also on the extrinsic erosion effect of the erosive winds. It was supposed that there existed general consistency in the mechanics of wind erosion on different soils.
关 键 词:SOIL EROSION by WIND erodible PARTICLES PARTICLE SIZE distribution.
分 类 号:P425.6[天文地球—大气科学及气象学]
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