期刊文献+

淅川县石质荒漠化土地空间分布特征研究 被引量:2

Spatial Distribution Characteristic of Rocky Desertification in Xichuan County
下载PDF
导出
摘要 淅川县是南水北调中线工程的核心水源区,也是主要淹没区及渠首所在地,全县石质荒漠化土地面积745.539 3 km^2,占土地总面积的26.44%,水土流失和区域生态资源环境问题十分严重。为有效防治石质荒漠化,以淅川县为研究区,基于高分辨率遥感影像、DEM、地形图、土地利用现状成果等基础信息数据,利用"3S"技术对淅川县石质荒漠化土地的海拔和坡向分布特征进行了分析。结果表明:石质荒漠化土地主要分布在海拔200~500 m高程带和S、SE、SW坡向上,S坡向上分布面积最大,N坡向上分布面积最小。因此,在淅川县石质荒漠化防治措施选择、配置、实施等工程实践中应充分考虑海拔和坡向的影响。 Xichuan County is the core source area,main flooded area and location of the head work of the Middle Route of South-to-North Water Transfer Project,which the rocky desertification area of the whole county is 745. 539 3 km^2,making up 26.44% of the total land area,causing serious soil and water loss and regional ecological resources and environmental problems. In order to effectively prevent and control the rocky desertification,the paper analyzed the characteristics of the elevation and slope direction distribution of rocky desertification land by taking Xichuan County as a studied area,based on basic information data of the high resolution remote sensing images,DEM,topographic maps and results of land use status and by using 3 S technology. The outcomes show that the rocky desertification land is mainly distributed on the elevation zone of 200-500 m and mainly distributed on the slope directions of south,southeast and southwest. The distribution area of the south slope direction is the largest and the north slope direction is the smallest. Thus,the influence of elevation and slope direction should be fully considered in the practice of measures selection,allocation and implementation of stone desertification prevention and control of the county.
出处 《中国水土保持》 2018年第11期33-35,共3页 Soil and Water Conservation in China
基金 河南省水利厅水利科技攻关计划项目(GG201544)
关键词 石质荒漠化 空间分布特征 南水北调中线工程 水源区 淅川县 rocky desertification spatial distribution characteristic the Middle Route of South-to-North Water Transfer water source area Xichuan County
  • 相关文献

参考文献5

二级参考文献19

  • 1丰茂森.遥感图像数字处理[M].北京:地质出版社,1991,7..
  • 2李新民.把贵州定位为“世界岩溶公园”[EB].http://ww.gog.com.cn,2003-12-09.
  • 3石明 李芬 张文芳.土地荒漠化成因分析及防治对策[J].中国水利,2003,484(5):55-57.
  • 4WangXiaodong, WangHongmei, DangAnrong. Research on large - scale dynamic monitoring of landuse with RS, GPS and G/S[ A]. International Geoscience and Remote Sensing Symposium(IGARSS) [ C ]. 2000. 2134-2136.
  • 5Yuan Daoxian. Rocky desertification in the subtropical karst of South China. In: Webmaster. Copyrights by Karst Dynamics Laboratory and Network Center of Guangxi Normal University, 1995- 1999
  • 6Yuan Daoxian. Karst environment systems. Proceedings of the international geographical Union Study Group [J]. Man' s Impact on Karst , 1989:149-163.
  • 7熊康宁 等.喀斯特石漠化的遥感-GIS典型研究[M].北京:地质出版社,2002..
  • 8Wang Qian, Wang Wenjie, Zheng Binghui et al. The remote sensing investigation of eco-environment status in Western China [J].Journal of Remote Sensing. 2003,7 (6): 490 - 497. [ 王桥, 王文杰,郑丙辉,等.中国西部地区生态环
  • 9Zhou Zhongfa. Application of RS & GIS technology on land rocky desertification of Guizhou karst area [J]. Chinese Journal of Waterand Soil Conseruation 2001. 21(3):52-54. [周忠发. 遥感和GIS技术在贵州喀斯特地区土地石
  • 10Tan Jizhong, Zhang Bing. Preliminary study on the rocky desertification land, Yunnan Province [J]. Journal of Geological Hazardsand Environment Preservation 14(1): 32 - 37. [谭继中, 张兵.云南省土地石漠化特征初步研究[J].

共引文献141

同被引文献41

引证文献2

二级引证文献12

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部