重庆南温泉背斜地下热水系统的探讨

System of the Geothermal Water in the Nanwenquan Anticline

为了科学开发和保护地下热水资源环境的可持续发展,对南温泉背斜及邻近地区地下热水的水化学和水动力特征进行系统研究,结果表明:南温泉地下热水起源于大气降水,补给区在与南温泉背斜为一个统一的地下热水系统的褶皱构造的铜锣峡背斜北端大巴山地区,地下热水由北往南流,南温泉背斜两翼、南北端的地下热水均有水力联系,整个南温泉背斜地下热水为一个统一的地下热水系统.背斜各地下热水开发点,应统一规划热水的开采量,避免由于各自为政过量开采地下热水,从而导致地下热水资源生态环境遭到不可逆转的破坏.此研究为科学开发和保护地下热水资源环境可持续发展提供理论依据.

In order to exploit and protect the geothermal water scientifically, the chemistry and isotope of geothermal water are studied in Nanwenquan anticline. It is show that the geothermal water comes from atmosphere precipitation in the north of Tongluoxia anticline, in which the Tongluoxia anticline and Nanwenquan anticline are whole geothermal water system. The geothermal water flows from north to south. The geothermal water has hydraulic contact from north to south, from the western limb to eastern limb. The geothermal waters in Nanwenquan anticline are whole geothermal water system. Every exploration of the geothermal water in Nanwenquan anticline should layout. So it can avoid that the yield is higher than pondage, and the geothermal water source environment is destroyed. The study provides theoretical gist for exploiting and utilizing rationally and protecting geothermal water resource effectively.