对矿区进行了为期一年多的地下水长期动态观测，观测结果证明，深部矿坑涌水来源仍以含水层的静储量为主。
After a long-term dynamic observation of groundwater in more than one year in the mining area , the results show that groundwater static reserves is the main resource to deep mine water gushing .
静储量