The water temperature is a well natural tracer for studying the behavior of groundwater. 摘要地下水溫度場(chǎng)是研究地下水運動(dòng)的一種良好的天然示蹤劑。
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. 闡述巖溶地下水運動(dòng)特點(diǎn)，分別討論南方巖溶地下水與北方巖溶地下水運動(dòng)特征，在此基礎上建立了概念性模型。
