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忻定盆地,位于晋北偏南,地形平坦,出露的地层为第四纪的松散沉积物和第三纪的红粘土,根据调查资料该区在第四纪的松散沉积物中有较丰富的地下水源。在盆地的中心,地形低洼,地下水的埋深1—6米,土地的盐渍化很严重,使很大一部分土地不能耕种。为了开发深层水改良该区的盐碱地,在该地区利用电探寻找深层水,以便制定开发深层地下水计划。由于测区,地形平坦,岩性的各方向变化不大,所以布极方向可以任意选择,地
The Xinding basin, located in the south of north Shanxi, has a flat topography. The exposed strata are loose Quaternary sediments and Tertiary red clay. According to the survey, the area is rich in loose sediments of Quaternary period Underground water source. In the center of the basin, the landform is low and the depth of groundwater is 1-6 meters. The salinization of the land is so serious that a large part of the land can not be cultivated. In order to develop deep water to improve the saline-alkali land in the area, deep-water exploration using electric prospecting in the area was conducted in order to develop a plan for the development of deep groundwater. Due to the measuring area, the terrain is flat and the lithology has little change in all directions, so the orientation of the cloth can be chosen arbitrarily