新疆三塘湖盆地水文地质条件较为复杂,水文地质研究程度低。通过对控制地下水赋存及其富水性的机制进行分析,确定了控制盆地地下水的赋存及其富水性的主要因素有补给源、控水构造、地层厚度和地形地貌。盆地内地下水富集区均与控水构造活动密切相关,在盆地内非储水构造分布地段,地下水富水性较弱或无地下水赋存。
Hydrogeological conditions of the Santanghu basin of Xinjiang are complex and are seldom examined in the past. The mechanism of controlling groundwater occurrence and storage are analyzed in this paper. Results indicate that the recharge source, water controlling structure, formation thickness and landform are the main factors affecting groundwater occurrence and storage. Groundwater enrichment area is related to the active controlling water structures. Groundwater is poor or absent in the no-water-storing areas.