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随着乌苏市经济社会的进一步发展,耕地面积不断扩大,增加了对水资源的需求,使得乌苏市农灌用水紧缺,特别是季节性供需水矛盾十分突出,为提高本项目区供水保证率,本次利用乌苏市平原区已有的水井和地质勘察资料及卫片等前人工作成果,综合研究乌苏市地下水形成的地质及水文地质等条件,分析区域地下水补径排条件,得到项目区含水层富水性分布。结果表明:含水层为单一结构的潜水含水层,富水性极强,含水层逐步形成多层结构含水层即上部潜水含水层、下部承压含水层,富水性逐渐变弱。
With the further economic and social development of Wusu City, the area of cultivated land is constantly expanding, increasing the demand for water resources, making the shortage of irrigation water for irrigation in Usu City, especially the contradiction between seasonal supply and demand water. In order to improve the water supply guarantee in this project area, Rate, the use of wells in the plain area of Wusu City and the geological survey data and satellite and other predecessors work results, a comprehensive study of the geological and hydrogeological conditions of groundwater formation in Wusu City, analysis of regional groundwater recharge conditions, Aquifer water distribution of the project area is obtained. The results show that the aquifer is a single subsurface aquifer with extremely rich water. The aquifer gradually forms a multi-layer aquifer, ie, an upper sub aquifer and a lower confined aquifer, and the water-richness gradually becomes weaker.