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滇池流域石漠化特征分析

张华 王宇 柴金龙

中国岩溶2011,Vol.30Issue(2):181-186,6.
中国岩溶2011,Vol.30Issue(2):181-186,6.

滇池流域石漠化特征分析

Analysis on the desert's characteristics in Dianchi watershed

张华 1王宇 1柴金龙1

作者信息

  • 1. 云南省地质环境监测院,云南昆明650216
  • 折叠

摘要

Abstract

Dianchi watershed is located in Kunming basin, Yunnan Province. Karst rocky desert is comparatively developed, with 225. 56 km2 of rocky desert that accounting for about 7. 71% of the total area and 32.69% of the karst area in Dianchi watershed. The deserts mainly locate in Wanghaishan, DabanqiaoChenggong, Heilinpu. Haikou, Liangwangshan and Shangsuan etc. Among them, the most serious desertification area is the district in the northeast of Dabanqiao. The desertification has led to detriment as serious soil loss, arable land decrease and soil moisture retention capacity reducing as well as environmental degradation. Through field survey and ETM interpretation, it is found that the desertification is intimately related with natural factors as lithology, karstification, geomorphology and climate, and with human factor, as well as with industrial pollution. To against the genesis of the desertification, the governing measures are put forth, such as ecological restoration, farmland capital construction, water resource exploitation, rural power source construction and small town build as well as reasonable use of land.

关键词

石漠化/分布特征/石漠化成因/治理措施/滇池流域/云南

Key words

rocky desertification/ distribution characteristics/ genesis of the desertification/ governing measures/ Dianchi watershed/ Yunnan

分类

农业科技

引用本文复制引用

张华,王宇,柴金龙..滇池流域石漠化特征分析[J].中国岩溶,2011,30(2):181-186,6.

基金项目

国土资源大调查项目——云南重点岩溶流域水文地质及环境地质调查(编码:1212010634801) (编码:1212010634801)

中国岩溶

OACSCDCSTPCD

1001-4810

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