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Spatial Distribution Patterns and Type Structure of the Deserts in Xinjiang

  • ZHANG Zhi-wei ,
  • YANG Fa-xiang ,
  • WU Ji-long ,
  • ZHOU Jie ,
  • YIN Hui-yan
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  • 1. Qira National Station for Field Scientific Observation and Research of Steppe Ecosystem, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, Xinjiang, China;
    2. University of the Chinese Academy of Sciences, Beijing 100049, China;
    3. Chinese Academy of Forestry, Beijing 100091, China

Received date: 2013-09-25

  Revised date: 2014-03-06

  Online published: 2014-08-11

Abstract

This paper was designed to compile the piece-wise figures of deserts and their types in Xinjiang and to analyze the spatial distribution and structure of the deserts in Xinjiang based on the digital geomorphologic map (1∶1 000 000) and TM image data using Google Earth or GIS. The results were as follows: ① There are 577 desert fragments in Xinjiang, and they can be divided into 35 subareas. The deserts can be divided into six areas, i.e. the desert area in the Tarim Basin, desert area in the Junggar Basin, desert area in the Altay Mountains, west Junggar mountainous desert area, the Kunlun Mountain-Altun Mountain desert area, and Tianshan Mountain desert area; ② Area of the deserts in Xinjiang is 428 977.14 km2 and occupies a quarter (26.12%) of the total area of Xinjiang. Deserts are distributed widely in the plains, hilly regions and mountains. Spatially, the deserts are mainly distributed in the Tarim Basin and Junggar Basin. There is an obvious spatial heterogeneity of desert landscapes. The fragmentation degree of desert landscapes is high in the two large deserts in the Tarim Basin and Junggar Basin, and it is low in the two large basins but high in the mountain-basin ecotone; ③ There are the peculiar landforms dominated by dunes, longitudinal dunes, dune-chains and sand ridges in Xinjiang, and the desert vegetation coverage is low.

Cite this article

ZHANG Zhi-wei , YANG Fa-xiang , WU Ji-long , ZHOU Jie , YIN Hui-yan . Spatial Distribution Patterns and Type Structure of the Deserts in Xinjiang[J]. Arid Zone Research, 2014 , 31(4) : 763 -770 . DOI: 10.13866/j.azr.2014.04.27

References

〔1〕 朱震达,陈治平,吴正,等.塔克拉玛干沙漠风沙地貌研究〔M〕.北京:科学出版社,1981:1-110.〔Zhu Zhenda,Chen Zhiping,Wu Zheng,et al.Aeolian Geomorphology Research of Taklimakan Desert〔M〕.Beijing:Science Press,1981:1-110.〕
〔2〕 钱亦兵,吴兆宁,杨海峰,等.古尔班通古特沙漠环境研究〔M〕.北京:科学出版社,2010:1-4.〔Qian Yibing,Wu Zhaoning,Yang Haifeng,et al.Environments of Gurbantunggut Desert〔M〕.Beijing:Science Press,2010:1-4.〕
〔3〕 Qu J J,Liao K T,Dong G R,et al.Feathered sand ridges in the Kumtagh desert and their position in the classification system〔J〕.Science China Earth Sciences,2011,54(8):1 215-1 225.
〔4〕 杨尧军,袁宏波,刘淑娟,等.库姆塔格沙漠沙生柽柳种群与环境因子分析〔J〕.干旱区研究,2013,30(5):827-831.〔Yang Yaojun,Yuan Hongbo,Liu Shujuan,et al.Tamarix taklamakanensis population sand their environmental factors in the Kumtag desert〔J〕.Arid Zone Research,2013,30(5):827-831.〕
〔5〕 Wang X M,Eerdun H,Zhou Z J,et al.Significance of variations in the wind energy environment over the past 50years with respect to dune activity and desertification in arid and semiarid northern China〔J〕.Geomorphology,2007,86:252-266.
〔6〕 杨发相,雷加强,岳健,等.昆仑山北麓地貌过程对风沙危害形成的影响〔J〕.山地学报,2010,28(6):718-724.〔Yang Faxiang,Lei Jiaqiang,Yue Jian,et al.Influence of geomorphologic processes on formation of the blown sand disaster in the north piedmont of Kunlun Mountains〔J〕.Journal of Mountain Science,2010,28(6):718-724.〕.
〔7〕 杨发相,新疆地貌及其环境效应〔M〕.北京:地质出版社,2011.〔Yang Faxiang.Landforms and Their Environmental Effects in Xinjiang〔M〕.Beijing:Geologic Press,2011.〕
〔8〕 雷加强,王雪芹,王德.塔里木沙漠公路风沙危害形成研究〔J〕.干旱区研究,2003,20(1):1-6.〔Lei Jiaqiang,Wang Xueqing,Wang De.The formation of the blown sand disaster to the Tarim desert highway,Xinjiang,China〔J〕.Arid Zone Research,2003,20(1):1-6.〕
〔9〕 穆桂金.塔克拉玛干沙漠灌草丘的发育特征及环境意义〔J〕.干旱区研究,1994,11(1):34-41.〔Mu Guijin.The environmental significance of vegetation cones of the Taklimakan desert,China〔J〕.Arid Zone Research,1994,11(1):34-41.〕
〔10〕康向光,李生宇,王海峰,等.高立式沙障不同叠加模式的阻沙量对比分析〔J〕.干旱区研究,2013,30(3):550-555.〔Kang Xiangguang,Li Shengyu,Wang Haifeng,et al.Deposited-sand volume of high vertical sand barrier under different stacking modes〔J〕.Arid Zone Research,2013,30(3):550-555.〕
〔11〕杨兴华,何清,霍文,等.策勒绿洲-荒漠过渡带风沙前沿近地面不同方向的输沙特征〔J〕.干旱区研究,2011,29(6):1 100-1 104.〔Yang Xinghua,He Qing,Huo Wen,et al.Study onwind-blown sand characteristics at different directions near the surface in the frontier of an oasis-desert ecotone Qira county,Xinjiang〔J〕.Arid Zone Research,2011,29(6):1 100-1 104.〕
〔12〕钟德才.中国沙海动态演化〔M〕.兰州:甘肃文化出版社,1998:12-20.〔Zhong Decai,Dynamic Evolution of China Desert〔M〕.Lanzhou:Gansu Culture Press,1998:12-20.〕
〔13〕中国科学院寒区旱区环境与工程研究所.1∶4 000 000中国沙漠与沙漠化图〔M〕.北京:中国地图出版社,2005.〔Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Acandemy of Sciences.The 1∶4 000 000 Map of the Desert and Aeolian Desertification in China〔M〕.Beijing:China Cartographic Publishing House,2005.〕
〔14〕中华人民共和国地貌图编辑委员会.中华人民共和国地貌图集1∶1 000 000〔M〕.北京:科学出版社,2009.〔Editorial Board of Geomorphological Atlas of The People’s Republic of China.The 1∶1 000 000 Map of Geomorphological Atlas of the People’s Republic of China〔M〕.Beijing:Science Press,2009.〕
〔15〕吴正.中国沙漠及其治理〔M〕.北京:科学出版社,2009.〔Wu Zheng.Sandy Deserts and Its Control in China〔M〕.Beijing:Science Press,2009.〕
〔16〕周成虎,程维明,钱金凯.数字地貌遥感解析与制图〔M〕.北京:科学出版社,2009:53-88.〔Zhou Chenghu,Cheng Weiming,Qian Jinkai.Digital Geomorphological Interpretation and Mapping from Remote Sensing〔J〕.Beijing:Science Press,2009:53-88.〕
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