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Historical desertification of the Mu Us Sandy Land:A perspective from the Beidachi section

         

摘要

Historical desertification of the Mu Us Sandy Land is linked to both environmental changes and anthropogenic activities. This paper reports on an analysis of grain size parameters as indicative of such changes in the southwestern area of the Mu Us Sandy Land. Combined with analysis of chronologies and historical records, our results indicate that Beidachi Lake and a nearby seasonal river have retreated continuously in history and that sand dunes appeared at approximately the end of the Ming dynasty. This study sheds new light on the understanding of spatial-temporal changes of the interior Mu Us Sandy Land in history and has great significance in revealing environmental changes of the interior region of the Mu Us Sandy Land.

著录项

  • 来源
    《寒旱区科学(英文版)》 |2013年第3期|293-300|共8页
  • 作者单位

    College of Earth & Environmental Sciences, Lanzhou University, Lanzhou, Gansu 730000, China;

    Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    College of Earth & Environmental Sciences, Lanzhou University, Lanzhou, Gansu 730000, China;

    College of Earth & Environmental Sciences, Lanzhou University, Lanzhou, Gansu 730000, China;

    College of Earth & Environmental Sciences, Lanzhou University, Lanzhou, Gansu 730000, China;

    College of Earth & Environmental Sciences, Lanzhou University, Lanzhou, Gansu 730000, China;

  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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