基于GIS的喀斯特高原山区石漠化景观格局变化分析

    Analysis of rocky desertification landscape pattern change in Karst plateau area based on GIS

    • 摘要: 石漠化是广泛存在于中国西南地区的一种生态-地质灾害,目前已成为备受关注的研究热点和难点。为了解喀斯特高原山区石漠化景观的时空变化,以贵州省普定县南部的典型喀斯特高原山区后寨河流域为例,以3期遥感影像(1987年和1995年的TM影像与2004年的SPOT-5影像)作为数据源,借助于ArcGIS9.0等软件和数理统计分析方法,从石漠化强度分级的角度对近18 a来石漠化的动态变化进行了研究。结果表明:从整体上来看,整个流域的石漠化出现扩展的趋势,其中前期(1987-1995年)的扩展速度为6.55 hm2/a,后期(1995-2004年)的扩展速度为29.64 hm2/a,扩展速度呈现增加的趋势。其中,轻度石漠化的面积呈现出先减少后增加的趋势;而中度石漠化和强度石漠化的面积均呈现出逐渐增加的趋势。

       

      Abstract: As one of the most serious geo-ecological disasters in Karst areas in Southwestern China, rocky desertification has become one of the key and difficult research issues. Taking the Houzhaihe Valley in Puding County, Guizhou Province, Southwestern China as an example, the landscape pattern changes of Karst rocky desertification in the recent 18 years in Karst plateau area were studied from the perspective of different rocky desertification levels, based on 3 series of remote sensing images (TM images of 1987 and 1995 and SPOT-5 image of 2004), and applying GIS technique and statistics analysis methods. Results indicated that, as a whole landscape, the intensity and rate of rocky desertification land were increasing in the recent 18 years. The increasing rate of rocky desertification were 6.55 hm2/a from 1987 to 1995, and 29.64 hm2/a from 1995 to 2004. Different rocky desertification levels had shown different change tendencies. The area of light rocky desertification land reduced at first (from 1987 to 1995) and then increased (from 1995 to 2004), while the area of moderate and severe rocky desertification land increased continuously from 1987 to 2004.

       

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