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| On the sand surface stability in the southern part of Gurbantnggt Desert | |
| 作者姓名： | WANG Xueqin1 2 WANG Tao1 JIANG Jin2 & ZHAO Congju2 1. Laboratory of Blown Sand Physics and Desert Environment Cold and Arid Regions of Environmental and Engineering Research In-stitute Chinese Academy of Sciences Lanzhou 730000 China 2. Xinjiang Institute of Ecology and Geography Chinese Academy of Sciences Urmqi 830011 China Correspondence should be addressed to Wang Xueqin |
| 作者单位： | WANG Xueqin1，2，WANG Tao1，JIANG Jin2 & ZHAO Congju2 1. Laboratory of Blown Sand Physics and Desert Environment，Cold and Arid Regions of Environmental and Engineering Research In-stitute，Chinese Academy of Sciences，Lanzhou 730000，China; 2. Xinjiang Institute of Ecology and Geography，Chinese Academy of Sciences，Urmqi 830011，China Correspondence should be addressed to Wang Xueqin |
| 摘 要： | Longitudinal dunes,also known as linear dunes,are the most widespread of all dune types,which occupy1/2to2/3of the total area in the world sand seas.They mainly occur in the southern part of Africa,Arabian Peninsular,Australia,Central Asia and North Af-rica-Middle East regions[1],in China they mainly ap-pear in the Gurbantnggt Desert.Many researches have been done on wind dynamics of the sand dune and its relations with environmental conditions[2—9],but comprehensive studies on sand … |
| 关 键 词： | Gurbantnggt Desert longitudinal dune sand surface stability. |
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