长江科学院院报 ›› 2015, Vol. 32 ›› Issue (12): 30-35.DOI: 10.11988/ckyyb.20140529

• 水土保持与生态建设 • 上一篇    下一篇

喀斯特石漠化景观空间分布特征分析——以贵州六枝特区为例

马士彬1a,1b,2,张勇荣1a,1b,安裕伦2,张跃红3   

  1. 1.六盘水师范学院 a.环境与资源科学系;b.乌蒙山发展研究院,贵州 六盘水 553001;2.贵州师范大学地理与环境科学学院,贵阳 550001;3.贵阳市环境信息中心,贵阳 550001
  • 收稿日期:2014-06-30 出版日期:2015-12-20 发布日期:2015-12-11
  • 通讯作者: 安裕伦(1957-),男,贵州贵阳人,教授,博士生导师,主要从事遥感与地理信息系统应用研究,(电话)0851-83227356(电子信箱)anyulun@126.com
  • 作者简介:马士彬(1982-),男,黑龙江齐齐哈尔人,副教授,博士研究生,主要从事环境遥感与信息系统应用研究,(电话)15086450053
  • 基金资助:

    贵州省科学技术基金项目(黔科合J字[2012]2309号);国家自然科学基金项目(41161002);六盘水市科技局科技创新能力建设计划项目(52020 2012-04-01-01)

Analysis on Spatial Distribution Feature of Landscape of Karst RockyDesertification in Liuzhi Special Zone of GuiZhou

MA Shi-bin 1,2,3,ZHANG Yong-rong1,2 AN Yu-lun 3, ZHANG Yue-hong 4   

  1. 1.Environmental and Chemical Engineering Department,Liupanshui Normal Univercity,Liupanshui 553001,China;2.Institute of Wumeng Mountain Area Development and Research,Liupanshui Normal University,Liupanshui553001,China;3.School of Geographic and Environmental Sciences,Guizhou Normal University,Guiyang 550001,China;4.Guiyang Environmental Information Center,Guiyang 550001,China
  • Received:2014-06-30 Published:2015-12-20 Online:2015-12-11

摘要:

为揭示石漠化空间分布及演化特征,通过遥感解译获取石漠化数据,运用地形位指数和分布指数定量分析贵州六枝特区1990—2010年间石漠化变化空间特征。结果表明:①研究区1990—2010年间石漠化景观空间分布呈现高区段为无、潜在、轻度、极强度石漠化优势分布区,中区段为中度、强度石漠化优势分布区,低区段为无石漠化景观优势分布区;②不同主导因素驱动形成的石漠化景观分布地形位区段也不同,人为因素为主驱使形成的潜在、轻度、中度石漠化主要分布于低、中地形位区,自然因素为主驱使形成的强度、极强度石漠化分布于高地形位区段;③中地形位区是石漠化分布的普遍适应地形区。由于不同地形位区段内石漠化等级分布具有较大的差异性,因此治理的重点应放在低、中地形位区段内的潜在、轻度、中度石漠化,以及中地形位区段内的中度、强度石漠化,而对自然因素驱使形成的高地形位区的强度、极强度石漠化应以自然生态恢复为主。

关键词: 喀斯特石漠化, 空间特征, 地形位指数, 分布指数, 遥感数据

Abstract:

In order to obtain spatial distribution and evolution characteristics of rocky desertification,we used topographic position index and distribution index,as well as remote sensing and GIS technologies.Liuzhi special zone of Guizhou province from 1990 to 2010 was taken as an example.Topographic position can be divided into 3 intervals according to elevation and slope:low interval,middle interval,and high interval,and there are 6 levels for rocky desertification:none,potential,slight,moderate,severe,and extra severe.The results indicate that:Firstly,none,potential,slight,and extra severe rocky desertification regions are mainly located in the high interval,whereas moderate and severe rocky desertification regions are mainly located in the middle interval,with none rocky desertification regions in the low interval.Subsequently,the distribution of topographic position interval varied with different causes such as human activities and nature which lead to rocky desertification.Potential,slight,and moderate rocky desertification regions caused by human activities are mainly located in low and middle intervals of topographic position,whereas severe and extra severe rocky desertification regions caused by nature are distributed in high interval.Furthermore,the distribution of rocky desertification is easy to be seen in middle interval of topographic position.Finally,more attention should be paid to low and middle intervals, where the levels are potential,slight,moderate,or severe, whereas natural ecological restoration should be highlighted in the severe and extra severe rocky desertification areas in the high interval driven by natural factors.

Key words: Karst rocky desertification, spatial feature, topographic position index, distribution index, remote sensing data

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