喀斯特山区“三水”转化动态配置初探——以贵州普定后寨河流域为例  

STUDY OF DYNAMIC CONFIGURATION OF 3-TYPE WATER TRANSFORMATION IN KARST REGIONS—WITH THE CASE OF HOUZHAI DRAINAGE AREA IN PUDING COUNTY,GUIZHOU PROVINCE

作　　者：张燕[1] 朱文孝[1] 鄢贵权[2] 

机构地区：[1]贵州大学,贵州贵阳550003 [2]贵州科学院,贵州贵阳550001

出　　处：《贵州科学》2006年第1期20-24,共5页Guizhou Science

基　　金：国家科技部"西部开发"重大项目(2003BA901A12)部分内容

摘　　要：开采条件下,由于地下水位下降,天然状态下的“三水”转化关系被打破。本文以贵州省普定县后寨河流域为例,运用标准化方法,提出了喀斯特水资源系统动态配置关系,并分析了各系数之间的关系、影响因素及变化原因。3-type water transformation of native state has been broken down as the water - level of underground water faUing because of exploitation, in this paper, by example of Houzhai drainage area in Puding County, Guizhou Province, standardized method is applied, the dynamic configuration relationship of karst water system is presented, and the relationship of coefficients, influencing factors and the causes of changing are analyzed.

关 键 词：“三水”转化 动态配置 标准化系数 后寨河流域 

分 类 号：P641[天文地球—地质矿产勘探]