中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Field investigation of surface sand and dust movement over different sandy grasslands in the Otindag Sandy Land, China

文献类型:期刊论文

作者Liu, Shulin; Wang, Tao; Chen, Guangting; Guo, Jian; Xue, Xian; Ma, Shaoxiu
刊名ENVIRONMENTAL GEOLOGY
出版日期2008
卷号53期号:6页码:1225-1233
关键词Otindag Sandy Land sandy grasslands threshold wind speed sand and dust movement vegetation cover sand transport rate
ISSN号0943-0105
DOI10.1007/s00254-007-0711-0
通讯作者Liu, Shulin(liusl@lzb.ac.cn)
英文摘要The characteristics of sand and dust movement over different sandy grasslands in China's Otindag Sandy Land were explored based on field observations and laboratory analyses. Threshold wind speeds (the speed required to initiate sand movement) at a height of 2 m above the ground were estimated in the field for different surface types. Threshold wind speed above shifting dunes in the study area is about 4.6 m s(-1) at this height. This value was smaller than values observed above other surfaces, resulting in a greater risk of blowing sand above these dunes. Differences in sand transport rates (STR) as a function of the severity of desertification resulted primarily from differences in surface vegetation cover and secondarily from the soil's grain-size distribution. STR increased exponentially with increasing near-bed wind velocity. Under the same wind conditions, STR increased with increasing severity of desertification: from 0.08 g cm(-2) min(-1) above semi-fixed dunes to 8 g cm(-2) min(-1) above semi-shifting dunes and 25 g cm(-2) min(-1) above shifting dunes. Vegetation's affect on STR was clearly large. Different components of sand and dust were trapped over different lands: mostly sand grains but little dust were trapped above shifting dunes, but much dust was collected over semi-shifting and semi-fixed dunes. Human disturbance is likely to produce dust even from fixed dunes as a result of trampling by animals and vehicle travel. In addition, spring rainfall decreased the risk of sand and dust movement by accelerating germination of plants and the formation of a soil crust.
收录类别SCI
WOS关键词WIND ; TRANSPORT ; EROSION
WOS研究方向Environmental Sciences & Ecology ; Geology ; Water Resources
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary ; Water Resources
语种英语
WOS记录号WOS:000252191400007
出版者SPRINGER
URI标识http://www.irgrid.ac.cn/handle/1471x/2556083
专题寒区旱区环境与工程研究所
通讯作者Liu, Shulin
作者单位Chinese Acad Sci, Lanzhou Inst Chem Phys, Inst Cold & Arid Reg Environm & Engn Res, Key Lab Desert & Desertificat, Lanzhou 730000, Gansu, Peoples R China
推荐引用方式
GB/T 7714
Liu, Shulin,Wang, Tao,Chen, Guangting,et al. Field investigation of surface sand and dust movement over different sandy grasslands in the Otindag Sandy Land, China[J]. ENVIRONMENTAL GEOLOGY,2008,53(6):1225-1233.
APA Liu, Shulin,Wang, Tao,Chen, Guangting,Guo, Jian,Xue, Xian,&Ma, Shaoxiu.(2008).Field investigation of surface sand and dust movement over different sandy grasslands in the Otindag Sandy Land, China.ENVIRONMENTAL GEOLOGY,53(6),1225-1233.
MLA Liu, Shulin,et al."Field investigation of surface sand and dust movement over different sandy grasslands in the Otindag Sandy Land, China".ENVIRONMENTAL GEOLOGY 53.6(2008):1225-1233.

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来源:寒区旱区环境与工程研究所

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