五十年代末以来,对童家院和飞水岩矿床进行过水文地质分析,结论为简单水文地质类型,基本查明了矿床水文地质条件。随着矿山生产坑道不断加深和扩展,井下长期疏排地下水,对矿床水文地质条件的认识,很多方面存在局限性,有些结论欠妥。1993年之后分别对飞水岩矿床和童家院矿床按补勘与详 Since the late 1950s, the hydrogeological analysis has been carried out on Tongjiasheng and Feishui rock deposits. The conclusions are of simple hydrogeological types, and the hydrogeological conditions of the deposits are basically ascertained. With the deepening and expansion of mine production tunnels and long-term underground drainage of underground water, the understanding of hydrogeological conditions of the deposit has limitations in many aspects and some conclusions are not satisfactory. After 1993, the Feishui rock deposit and Tongjiatuan deposit should be compensated and detailed respectively