摘要
新安江连续径流模型是在研究湿润地区地下水丰富流域地下水产流及汇流规律的基础上,对新安江模型的水源分划结构作了重要改进后建立的.它对地下径流比例较大的地区具有一定的通用性.近年来的实践说明,该模型还适用于我国南方岩溶地区.本文回顾了新安江连续径流模型,文中着重叙述了岩溶地区的水文特性、模型在岩溶地区应用的物理基础和实例.
In this paper, the Xinanjiang Model of Continuous Runoff is reviewed, its establishment being based on the simulation and analysis of the basins with abundant groundwater runoff and on one important improvement of the division of various components of the runoff related to the model. The model is suitable for the regions with a great proportion of groundwater in the total runoff. Recent practice shows that it is also applicable to karst regions in South China. The hydrologic characteristics of karst regions...
出处
《河海大学学报（自然科学版）》
CAS
CSCD
1989年第4期43-50,共8页
Journal of Hohai University(Natural Sciences)
关键词
岩溶地貌
岩溶地下水
水源分划
线性系统
karst geomorphy
karst groundwater
distribution curve of final constant infiltration rate
division of various components of runoff
linear system
