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灌江流域岩溶环境与石漠化
引用本文:李兆林,杜毓超,陈宏峰.灌江流域岩溶环境与石漠化[J].广西师范大学学报(自然科学版),2006,24(3):103-106.
作者姓名:李兆林  杜毓超  陈宏峰
作者单位:中国地质科学院,岩溶地质研究所,广西,桂林,541004
基金项目:国家科技攻关计划 , 国家地调项目基金
摘    要:石漠化是岩溶地区脆弱的岩溶地质基础上形成的一种荒漠化现象,它的产生与岩溶环境条件直接相关。通过对流域内的岩性、地貌、岩溶形态、表层岩溶带、地下管道在岩溶水系统中构成的水文网络及动态变化等岩溶环境特征的调查研究,论述了不同环境条件下,对生态环境影响程度及其产生的后果。根据石漠化的分布现状与岩溶环境特征之间的关系,分析石漠化的发展趋势。

关 键 词:环境地学  岩溶环境  表层岩溶带  地下水系统  生态环境  石漠化
文章编号:1001-6600(2006)03-0103-04
收稿时间:2005-12-23
修稿时间:2005年12月23

Karst Environment and Rock Desertification in Guan Jiang Basin
LI Zhao-lin,DU Yu-chao,CHEN Hong-feng.Karst Environment and Rock Desertification in Guan Jiang Basin[J].Journal of Guangxi Normal University(Natural Science Edition),2006,24(3):103-106.
Authors:LI Zhao-lin  DU Yu-chao  CHEN Hong-feng
Institution:Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China
Abstract:Rock desertification is a certain desertification phenomenon developing in the Karst areas with vulnerable environments,the involvement of which has direct correlation with Karst environment conditions.The influence degree and the subsequent posteffect of rock desertification to entironments were discussed by means of investigation on such characteristics of Karst environments as lithology,physiognomy,Karst configuration,epikarst development and regime change of hydrologic networks formed by subterranean conduits.Moreover,the development trend of rock desertification was analyzed according to the connection between its present distribution situation and characteristics of Karst environments.
Keywords:enviromental geology  Karst environment  epikarst zone  ground water systems  environment  rock desertification
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