“含羞泉”水文地质特征及形成机理

Hydrogeological Characteristics and Genetic Mechanism of the Shame Spring

开展“含羞泉”地质调查、地质雷达、地下水化学分析以及观察试验,探明泉点原位位置,分析其水文地质特征及“含羞”机理。探明了公路压覆原位泉点位置;含羞泉为断层下盘单斜储水构造出露间隙泉,间隙周期变化较大,地下水补给充裕或贫乏时,泉水出现排或断流、倒流现象。

This study does geological survey,geological radar detection,chemical analysis of groundwater for the Shame Spring.The location of the spring source covered by the highway was found.The results indicate that the Shame Spring is a periodic spring originated from the monoclinic water storage structure in footwall of a fault.This spring water appears to discharge or stop flow,reverse flow phenomenon when groundwater supplies are abundant or scarce.