摘要
本文首先从地貌形态结构对喀斯特峰丛洼地(谷地)流域的产流及汇流机制进行了研究,然后结合喀斯特流域结构的水文特点,提出了喀斯特峰丛洼地(谷地)流域的产流量计算模式和地貌水文汇流模型。
In this paper, using morphological analysis the mechanism of the run- off yield and flow concentration in the drainage basin of the karst fengcong -depression is discassed. Considering the hydrological Characteristics of the structure of the karst basin,we present the calculating pattern of the run- off-yield and the flow concentration model of the basin of karst fengcong -depression district.
出处
《贵州师范大学学报（自然科学版）》
CAS
1992年第1期10-17,共8页
Journal of Guizhou Normal University：Natural Sciences
基金
贵州省教委自然科学基金
关键词
峰丛
洼地
产流
汇流
模型
Fengcong-Depression, Runoff yield, Flow concentration,Model
