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.
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
关键词
“三水”转化
动态配置
标准化系数
后寨河流域
3-type water transformation
dynamic configuration
standardized coefficients
Houzhai drainage area
