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苏08井位于江苏兴化县戴窑镇东,苏北溱潼凹陷,戴窑局部构造。井深2680米,7吋油层套管下入深度2228米,以下为裸跟。所测含水层为古生界白云岩、灰岩,岩层天然裂隙十分发育,其上复盖巨厚的隔水性能良好均白垩系、第三系泥岩。井孔四周由水泥固井。该井使用HCJ-1型水位仪观测。记录资料表明:水位反映地球固体潮汐十分清晰,朔望日井潮潮
Su 08 Well located in Xinghua County, Jiangsu Province, east of the kiln, Tongbei Depression, northern part of the structure. Well 2680 meters deep, 7-inch casing under the depth of 2228 meters, the following is naked with. The measured aquifers are Paleozoic dolomites and limestones. The natural fractures of the rock formations are well developed. Cretaceous and Tertiary mudstones are all well covered by the aquifer which is covered by a thick layer of water. Wells are cemented by cement around the well. The well was surveyed using the HCJ-1 water level meter. Records show that: the water level reflects the Earth’s solid tide is very clear, the new moon tide