Hydrogeological characteristics and water yield pattern of the Paleogene Zhujiagou formation in south-central Shandong Province
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摘要: 朱家沟组集中分布在鲁中南坳陷盆地边缘地带，为一套陆源碎屑沉积的灰质砾岩。以汶口盆地、新汶盆地朱家沟组为研究对象，通过1：50000水文地质调查、水文地质钻探、地球物理勘探、抽水试验、水质分析等技术方法，分析其水文地质特征。研究结果表明：朱家沟组裂隙岩溶形态以溶蚀裂隙、溶孔、溶洞为主，主要发育在150 m以浅；富水性受断裂控制明显，裂隙岩溶发育段单井涌水量可超过300 m3/d，具有显著实际供水意义；朱家沟组富水模式为断裂型灰质砾岩裂隙岩溶蓄水构造模式，以断裂构造为主控因素，该模式在鲁中南地区具有普遍性和适用性，对于寻找新的供水目标含水层及找水定井工作具有指导意义。Abstract: The Zhujiagou formation, a set of calcareous conglomerates of terrigenous clastic deposition, is mainly distributed along the edge of the depression basins in south-central Shandong. Taking the Zhujiagou formation in the Wenkou basin and the Xinwen basin as the study area, the hydrogeological characteristics are analyzed through 1:50000 hydrogeological survey, hydrogeological drilling, geophysical exploration, pumping test, water quality analysis and other technical methods. The results show that the karst morphology of the Zhujiagou formation is dominated by corrosion fissure, karst hole and karst cave, which are mainly developed in the shallow layer of 150 m. The water yield property is obviously controlled by the fracture, and the water inflow of a single well in the fracture karst development area can be more than 300 m3/d, indicating practical water supply significance. The water yield pattern of the Zhujiagou formation features fracture-karst water storage structure of fractured calcareous conglomerate and fracture structure is the main controlling factor. This pattern has universality and applicability in south-central Shandong Province, which is of guiding significance for new water supply aquifers exploration and site selection and layout for wells.
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图 2 汶口盆地朱家沟组水文地质及调查点分布图
Figure 2. Hydrogeology and survey spots of the Zhujiagou formation in the Wenkou basin
图 3 磁窑镇北部地面塌陷高密度电法和CSAMT剖面图
Figure 3. High density electrical method and CSAMT profile of the surface collapse in the north of Ciyao Town
图 4 朱家沟组内发育的大规模洞穴沉积物照片(东杏山村)
Figure 4. Large scale cave sediments developed in the Zhujiagou formation (Dongxingshan Village)
图 5 研究区地下水样品piper图
Figure 5. Piper diagram of groundwater samples in the research area
图 7 汶口盆地DWZK03钻孔水文地质剖面图
Figure 7. Hydrogeological profile of the borehore DWZK03 in the Wenkou basin
表 1 汶口盆地朱家沟组调查点统计表
Table 1. Statistical table of survey spots of the Zhujiagou formation in the Wenkou basin
编号 位置 井深/m 地下水水位埋深/m 单井涌水量/(m3/d) 所处构造位置 J125 山东省泰安市宁阳县磁窑镇泊家庄村 16 3.62 2880 高村断裂以东 J165 山东省泰安市宁阳县华丰镇乔家庄村 60 21.07 192 磁窑断裂以东 J207 山东省泰安市宁阳县华丰镇胜天庄村 205 9.80 192 顺义庄断裂以东 J211 山东省泰安市宁阳县中韩家庄村 15 5.23 120 无 J213 山东省泰安市宁阳县东庄镇北石崮村 120 4.90 192 无 J214 山东省泰安市宁阳县东庄镇北石崮村 9 2.15 120 无 J215 山东省泰安市宁阳县东庄镇北石崮村 7 1.50 96 无 DWZK03 山东省泰安市宁阳县磁窑镇国家庄村 150.3 13.30 1251.6 磁窑断裂以西 
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表 2 新汶盆地朱家沟组调查点统计表
Table 2. Statistical table of survey spots of the Zhujiagou formation in the Xinwen basin
编号 位置 井深/m 地下水水位埋深/m 单井涌水量/(m3/d) 含水层段厚度/m XWZK02 新泰市青云街道东杏山村 155 26.92 927 16.7 XTZK03 蒙阴县常路组白杨庄村 152 18.70 4944 41.7 XTJ36 蒙阴县常路镇杏泉村 187 32.54 768 32 XTJ175 新泰市汶南镇大官庄村 156 28.64 720 45.6 XTJ177 新泰市汶南镇双山村 225 24.30 840 28.9 XTJ179 新泰市汶南镇北岙阳村 200 23.20 960 50 XWJ186 新泰市翟镇富全庄村 3 1.20 120 1.5 XWJ197 新泰市泉沟镇高崖头村 40 10.43 144 36 XWJ199 新泰市泉沟镇新官庄村 8 2.20 72 8 XWJ200 新泰市泉沟镇新官庄村 5 1.50 72 4 XWJ201 新泰市泉沟镇小官庄村 50 14.75 72 48 XWJ239 新泰市翟镇王家寨村 10 1.35 240 8 XWJ240 新泰市翟镇小王家寨村 8 3.85 24 8 XWJ243 新泰市翟镇井家庄村 350 29.65 480 50
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表 3 朱家沟组地下水化学数据
Table 3. Groundwater hydrochemical data table of the Zhujiagou formation
构造单元 样品编号 阳离子/(mg·L-1) 阴离子/(mg·L-1) TDS/(mg·L-1) pH值 水化学类型 K+ Na+ Ca2+ Mg2+ Cl- SO42- HCO3- NO3- 汶口盆地 DWZK03 1.67 97.78 281.96 29.90 310.57 216.14 297.72 73.36 1230 7.6 Cl·HCO3-Ca型 J165 0.56 74.01 493.79 50.43 279.37 576.36 239.07 498.07 2100 7.5 SO4-Ca型 J211 2.48 58.94 244.29 32.33 177.27 304.51 177.77 195.05 1110 7.7 SO4·Cl-Ca型 J207 3.15 53.48 347.89 21.75 163.08 428.91 220.68 236.20 1370 7.5 SO4-Ca型 新汶盆地 XWZK02 1.22 26.96 177.96 28.19 47.51 163.78 341.95 113.00 735 7.7 HCO3·SO4-Ca型 XTZK03 0.58 9.61 126.05 22.36 26.59 97.50 253.82 113.29 530 7.9 HCO3-Ca型 XTJ36 0.50 9.46 137.88 24.55 30.49 107.11 253.36 122.90 570 7.7 HCO3-Ca型 XTJ175 0.50 9.60 154.51 15.68 24.82 102.78 279.87 101.60 560 7.7 HCO3-Ca型 XTJ177 1.19 19.18 174.35 24.79 42.54 137.85 137.85 123.24 684 7.5 HCO3·SO4-Ca型 XWJ197 0.57 22.99 217.63 23.46 38.64 221.90 423.36 77.16 828 7.5 HCO3·SO4-Ca型
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