中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Barchans of Minqin: Sediment transport

文献类型:期刊论文

作者Zhen-Ting, Wang1; Zhang, Jia-Wu1; Zhang, Qian-Hua2; Qiang, Ming-Rui1; Chen, Fa-Hu1; Ling, Yu-Quan2
刊名GEOMORPHOLOGY
出版日期2008-04-01
卷号96期号:1-2页码:233-238
关键词barchan sand flux spanwise brink
ISSN号0169-555X
DOI10.1016/j.geomorph.2007.07.018
通讯作者Zhen-Ting, Wang(wangzht@lzu.edu.cn)
英文摘要Spatial changes in the rates of sand transport are a fundamental control of dune morphology. A detailed field measurement of sand flux along the brink of a barchan was performed to explore the spanwise property of sand flux on the barchan surface. Setting the arc length of the brink at the tip of the longer horn to zero, it was found that the value of sand flux increases with the arc length of the brink at first and then decreases at both low and high wind speeds. The maximum occurs at the crest. Our result suggests that the spanwise distribution of sand flux cannot be neglected in the study of transverse dunes.
收录类别SCI
WOS关键词SAND DUNES ; TRANSVERSE DUNES ; SOUTHERN PERU ; AEOLIAN DUNES ; LOW HILLS ; WIND ; FLOW ; MIGRATION ; MOVEMENT ; MODEL
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000254789200015
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2556039
专题寒区旱区环境与工程研究所
通讯作者Zhen-Ting, Wang
作者单位1.Lanzhou Univ, Minist Educ, Key Lab Western Chinas Environm Syst, CAEP, Lanzhou 730000, Peoples R China
2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Zhen-Ting, Wang,Zhang, Jia-Wu,Zhang, Qian-Hua,et al. Barchans of Minqin: Sediment transport[J]. GEOMORPHOLOGY,2008,96(1-2):233-238.
APA Zhen-Ting, Wang,Zhang, Jia-Wu,Zhang, Qian-Hua,Qiang, Ming-Rui,Chen, Fa-Hu,&Ling, Yu-Quan.(2008).Barchans of Minqin: Sediment transport.GEOMORPHOLOGY,96(1-2),233-238.
MLA Zhen-Ting, Wang,et al."Barchans of Minqin: Sediment transport".GEOMORPHOLOGY 96.1-2(2008):233-238.

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来源:寒区旱区环境与工程研究所

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