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西影深井处在西安凹陷东南坡大雁塔热异常带上,位于西安电影制片厂后院。井深2000.41米。给水层有两层,分别是:1520—1527米和1560—1617米。1417米以上的环形空间用水泥封死,因之工农业取水层和地表水与该井给水层无水力学联系。从水位观测资料分析中发现,水位的升降变化与气压的升降变化同步性很强,反映了气压是水位变化的主要因素之一。
Deep in the West Shadow deep depression in the Xi’an sagittal geese tower exceptionally hot zone, located in the backyard of Xi’an Film Studio. Well depth 2000.41 meters. There are two layers of aquifer, namely: 1520-1527 meters and 1560-1617 meters. The annular space above 1,417 meters was sealed with cement because of the lack of hydraulics between the industrial and agricultural aquifers and surface water. From the analysis of water level observation data, it is found that the change of water level is in synchronicity with the change of air pressure, which reflects that air pressure is one of the main factors of water level change.