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中国沙漠 ›› 2008, Vol. 28 ›› Issue (6): 1017-1021.

• 沙漠与沙漠化 • 上一篇    下一篇

近30 a来毛乌素沙地及其周边地区沙漠化动态变化过程研究

郭 坚1; 王 涛1; 韩邦帅1; 孙军喜2; 李新泉2   

  1. 1.中国科学院寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室, 甘肃 兰州 730000; 2.内蒙古自治区新巴尔虎左旗气象局, 内蒙古 新巴尔虎左旗 021200
  • 收稿日期:2007-06-25 修回日期:2007-12-19 出版日期:2008-11-20 发布日期:2008-11-20

Dynamic Process of Aeolian Desertification Land Variation in Mu Us Sandy Land and Its Surrounding Area in Recent 30 Years

GUO Jian1, WANG Tao1, HAN Bang-shuai1, SUN Jun-xi2, LI Xin-quan2   

  1. 1.Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou 730000, China; 2.Xin Barag Left Banner Weather Bureau of Inner Mongolia, Xin Barag Left Banner 021200, Inner Mongolia, China
  • Received:2007-06-25 Revised:2007-12-19 Online:2008-11-20 Published:2008-11-20

摘要: 使用1977年和1986年的沙漠化数据以及2000年和2005年的遥感影像来分析毛乌素沙地及其周边地区在不同时期的沙漠化土地空间分布以及动态变化过程。为了使各个时期的数据具有可比性,采用了与1977年和1986年相同的沙漠化程度分类方法,建立遥感判读标志,采用目视解译的方法得到了2000年和2005年的沙漠化数据。结果显示,自1977年以来毛乌素沙地及周边地区3种程度的沙漠化土地面积都呈持续下降趋势,且轻度沙漠化土地面积减少最快;总沙漠化土地面积在1986—2000年减少的最快;就沙漠化土地的空间分布而言,各个时期都主要集中分布在自然条件较差的鄂托克旗、鄂托克前旗和乌审旗;在1977—2005的近30 a间,各个旗、县的沙漠化土地面积也都持续减少,无论时间上还是空间上,研究区的沙漠化土地都处于全面逆转阶段。

关键词: 毛乌素沙地, 沙漠化, 遥感监测, 动态变化

Abstract: In this paper, the aeolian desertification land data of 1977 and 1986 and the satellite images in 2000 and 2005 are used to analyze the spatial distribution and dynamic variation process of aeolian desertification land in Mu Us sandy land and its surrounding area during different periods. In order to make the aeolian desertification land data of different periods comparable, we interpret satellite images in 2000 and 2005 visually according to the same criterions as how 1977 and 1986 data was obtained. The results show that the area of aeolian desertification land was keeping a decreasing trend in this area since 1977, and the light aeolian desertification land had the fastest decreasing speed, the moderate had the second and the severe had the slowest decreasing speed. The total area of aeolian desertification land decreased fast during 1986—2000. As for the spatial distribution of aeolian desertification land, the most concentrated in arid Otog Banner, Otog Front Banner and Wxin Banner. During 1977—2005, the area of aeolian desertification land decrease continuously in all counties or banners, which showed the status of aeolian desertification here kept reversing temporally and spatially.

Key words: Mu Us Sandy Land, aeolian desertification, remote sensing monitoring, dynamic variation

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