The water temperature is a well natural tracer for studying the behavior of groundwater. 摘要地下水温度场是研究地下水运动的一种良好的天然示踪剂。
In this paper the character istics of karst water flow are expounded and the features of karst water movement in South China and in North China are discussed respectively. 阐述岩溶地下水运动特点,分别讨论南方岩溶地下水与北方岩溶地下水运动特征,在此基础上建立了概念性模型。