By wind tunnel experiment, we studied the deflation rates of 8 different clastic sediments in the arid regions of China, discussed the sources of aeolian sand and their influence on the development of sand dunes and f...By wind tunnel experiment, we studied the deflation rates of 8 different clastic sediments in the arid regions of China, discussed the sources of aeolian sand and their influence on the development of sand dunes and formation of sand deserts from the view of dynamics of wind erosion. The average deflation rates of 8 typical clastic sediments in the arid regions of China can be arranged in the order of lacustrine sand 〉 alluvial sand 〉 weathered sandstone and shale 〉 pluvial sediments 〉 fluvioglacial sand 〉 weathered granite 〉 slope deposit 〉 glacial sediments. The deflation rates exhibited strong positive correlations with the erodible particle （0.063 2mm） content and sorting features. In contrast, the deflation rates had obvious negative correlations with the contents of silt clay （〈0.063 mm） and gravel （〉2 mm）. According to the deflation rates, the 8 typical clastic sediments can be divided into four categories： （1） lacustrine and alluvial sand, which are readily prone to wind erosion, assumed to be the main source of aeolian sand; （2） weathered sandstone and shale, pluvial sediments and fluvioglacial sand with considerable deflation rates, might be the secondary source of aeolian sand; （3） weathered granite and slope deposit having the lower deflation rates, could supply a little aeolian sand; and （4） glacial sediments with a strong anti-erodibility, could hardly offer any aeolian sand. In addition to the strong wind conditions, the exposure of extensive lacustrine sand induced by the desiccation of inland lake basin, as well as the pre-sorting of clastic sediments by flowing water should be the key factors influencing the development of sand deserts in China. The possible reason the sand deserts in China being mostly distributed around the inland lake basins and along riverbanks could be better understood through sand source analysis.展开更多
Electric discharge phenomenon is often observed during the passage of sandstorms over desert regions and sometimes does great damage to human beings. Based on previous researches on the electrification of sandstorms b...Electric discharge phenomenon is often observed during the passage of sandstorms over desert regions and sometimes does great damage to human beings. Based on previous researches on the electrification of sandstorms by the scholars both at home and aboard,the authors conducted the simulation experiments on the electric fields of sandstorm-triggered creeping-saltating sand, suspending sand and watered suspending sand in the large-scale wind tunnel. According to the experimental results the electric field structure and its formation mechanism were analysed and discussed, the quantity of electric charges and electric field strengthwere measured and calculated, and finally several conclusions were drawn.展开更多
基金National Natural Science Foundation of China, No.40471014 The Ministry of Science and Technology, No.2005BA517A-11
文摘By wind tunnel experiment, we studied the deflation rates of 8 different clastic sediments in the arid regions of China, discussed the sources of aeolian sand and their influence on the development of sand dunes and formation of sand deserts from the view of dynamics of wind erosion. The average deflation rates of 8 typical clastic sediments in the arid regions of China can be arranged in the order of lacustrine sand 〉 alluvial sand 〉 weathered sandstone and shale 〉 pluvial sediments 〉 fluvioglacial sand 〉 weathered granite 〉 slope deposit 〉 glacial sediments. The deflation rates exhibited strong positive correlations with the erodible particle （0.063 2mm） content and sorting features. In contrast, the deflation rates had obvious negative correlations with the contents of silt clay （〈0.063 mm） and gravel （〉2 mm）. According to the deflation rates, the 8 typical clastic sediments can be divided into four categories： （1） lacustrine and alluvial sand, which are readily prone to wind erosion, assumed to be the main source of aeolian sand; （2） weathered sandstone and shale, pluvial sediments and fluvioglacial sand with considerable deflation rates, might be the secondary source of aeolian sand; （3） weathered granite and slope deposit having the lower deflation rates, could supply a little aeolian sand; and （4） glacial sediments with a strong anti-erodibility, could hardly offer any aeolian sand. In addition to the strong wind conditions, the exposure of extensive lacustrine sand induced by the desiccation of inland lake basin, as well as the pre-sorting of clastic sediments by flowing water should be the key factors influencing the development of sand deserts in China. The possible reason the sand deserts in China being mostly distributed around the inland lake basins and along riverbanks could be better understood through sand source analysis.
基金This project was supported by the InnovationProject of the Chinese Academy of Sciences (Grant No. 210027) the Knowledge Innovation Project of Chinese Academy of Sciences (GrantNo. KZCX2-304)+1 种基金the National Natural Science Foundation of China(Grant No.39971013) the State Key Basic Research Development Planning (Grnat No.20000487).
文摘Electric discharge phenomenon is often observed during the passage of sandstorms over desert regions and sometimes does great damage to human beings. Based on previous researches on the electrification of sandstorms by the scholars both at home and aboard,the authors conducted the simulation experiments on the electric fields of sandstorm-triggered creeping-saltating sand, suspending sand and watered suspending sand in the large-scale wind tunnel. According to the experimental results the electric field structure and its formation mechanism were analysed and discussed, the quantity of electric charges and electric field strengthwere measured and calculated, and finally several conclusions were drawn.
