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物探与化探  2023, Vol. 47 Issue (3): 690-699    DOI: 10.11720/wtyht.2023.1443
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
综合物探方法在矿泉水勘查中的应用——以泾县榔桥地区为例
张志1,2(), 徐洪苗2, 钱家忠1(), 谢杰2, 陈皓龙2, 朱紫祥2
1.合肥工业大学 资源与环境工程学院,安徽 合肥 230009
2.安徽省地质矿产勘查局 327地质队,安徽 合肥 230011
An application study of the comprehensive geophysical prospecting method in the exploration of mineral water: A case study of the Langqiao area, Jing County
ZHANG Zhi1,2(), XU Hong-Miao2, QIAN Jia-Zhong1(), XIE Jie2, CHEN Hao-Long2, ZHU Zi-Xang2
1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
2. No. 327 Geological Team, Bureau of Geology and Mineral Exploration of Anhui Province, Hefei 230011, China
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摘要 

安徽省泾县榔桥镇马渡桥村一带具有开发优质矿泉水的巨大潜力,然而受地质条件及含水介质非均质性影响,其分布范围勘定以及水量、水质定量评价一直是影响矿泉水开发利用的难题。基于此,以泾县榔桥地区为靶区开展了地面物探与水文测井联合的综合物探方法应用研究,取得了重要进展,主要包括:①通过地面综合物探方法实现了花岗闪长岩中断裂构造的精确定位,通过水文测井实现了构造裂隙水层位的精准识别;②成功探明单孔出水量约为50~80 m3/d的偏硅酸型饮用天然矿泉水;③指示了区内富水断裂构造为中浅埋深(约75~140 m),走向主要为NW向。研究成果揭示了该区赋存矿泉水构造的空间分布特征,对后续矿泉水范围勘定具有重要意义,同时,泾县榔桥地区综合勘查的研究思路和技术方法具备系统性,对相近地区矿泉水勘查具有指导意义。

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张志
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钱家忠
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陈皓龙
朱紫祥
关键词 综合物探地下水勘查天然矿泉水泾县榔桥地区    
Abstract

The area around Maduqiao Village, Langqiao Town, Jing County has great potential for the development of high-quality mineral water. However, due to the geological conditions and the inhomogeneity of water-bearing media, the investigation of the distribution range of the mineral water in the area and the quantitative evaluation of the water quantity and quality have always been challenges to the development and utilization of mineral water in the area. With the Langqiao area of Jing County as the target area, an application study on the comprehensive geophysical prospecting method that comprehensive ground geophysical prospecting with hydrogeological logs was conducted, achieving important progress. The major results are as follows: (1) The fault structures in granodiorites were precisely located through comprehensive ground geophysical prospecting, and the horizon of tectonic fissure water was precisely identified based on hydrogeological logs; (2) The metasilicate natural mineral water for drinking with a single well water yield of 50~80 m3/d was identified; (3) The water-rich fault structures in the study area have a medium to shallow burial depths of about 75~140 m and primarily have a NW strike. These results reveal the spatial distribution characteristics of the mineral water-bearing structures in the study area and are of great significance to the subsequent investigation of the mineral water range. Moreover, the systematic research philosophy and technical methods used for the Langqiao area of Jing County in this study can guide the mineral water exploration in similar areas.

Key wordscomprehensive geophysical prospecting    groundwater exploration    natural mineral water    Langqiao area of Jing County
收稿日期: 2022-09-19      修回日期: 2023-01-18      出版日期: 2023-06-20
ZTFLH:  P631  
基金资助:国家自然科学基金项目“基岩裂隙水非达西流与溶质非费克运移机制及其升尺度模型”(41831289);泾县人民政府公开招标项目“泾县榔桥镇马渡桥村矿泉水勘查”(JX-CG-GK-2019-066)
通讯作者: 钱家忠(1968-),男,博士,教授,主要从事水工环地质学科的教学和深层次研究工作。Email:qjiazhong@gmail.com
作者简介: 张志(1991-),男,硕士,主要从事地球物理勘查与综合研究工作。Email:2763369850@qq.com
引用本文:   
张志, 徐洪苗, 钱家忠, 谢杰, 陈皓龙, 朱紫祥. 综合物探方法在矿泉水勘查中的应用——以泾县榔桥地区为例[J]. 物探与化探, 2023, 47(3): 690-699.
ZHANG Zhi, XU Hong-Miao, QIAN Jia-Zhong, XIE Jie, CHEN Hao-Long, ZHU Zi-Xang. An application study of the comprehensive geophysical prospecting method in the exploration of mineral water: A case study of the Langqiao area, Jing County. Geophysical and Geochemical Exploration, 2023, 47(3): 690-699.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2023.1443      或      https://www.wutanyuhuatan.com/CN/Y2023/V47/I3/690
Fig.1  区域地质简图
Fig.2  研究区地质及物探工程布置
Fig.3  研究区矿泉水成因示意
水样 指标/(mg·L-1) 水化学类型
偏硅酸 总硬度 总碱度
浅层地下水 24.4~58.8 0.07~0.43 0.63~1.31 28.28~211.38 29.57~139.76 HCO3-Ca·Mg或
HCO3-Ca·Na
地表水(水库和溪流) 11.9~22.2
Table 1  研究区地下水、地表水采样分析结果
Fig.4  研究区矿泉水勘查技术线路
Fig.5  S7(a)、N3(b)综合物探剖面成果
推测断
裂构造
走向 具体展布
F1 NNE S2:1030点—S4:1110点
F2 NW S1:1400点—S4:1110点
F3 NNE S2:1420点—S5:1300点
F4 NNE S7:1600点—S4:1900点—S3:1600点
F5 NWW S6:1420点—S7:1600点—S3:1120点
F6 NWW N5:1090点—N2:1680点—
N3:1080点—N1:1080点
F7 NWW N4:1810点—N3:1520点—N1:1540点
Table 2  地面综合物探推测断裂构造
Fig.6  地面综合物探推测成果(a)及遥感解译成果(b)
Fig.7  F2断层面(a)及构造角砾岩(b)
Fig.8  ZK01、ZK02水文测井曲线及综合解释
项目 ZK01 ZK02
降深(S) S3 S3
抽水开始时刻 2021/1/4 20:30 2021/1/17 13:00
抽水结束时刻 2021/1/5 23:30 2021/1/19 12:00
抽水延续时长/h 27 47
抽水稳定时长/h 24 24
降深值/m 80 35.27
涌水量/(m3·d-1) 51.36 81.69
Table 3  ZK01、ZK02抽水试验结果
水文钻孔 取样时间 水样分析项 w(偏硅酸)
/(mg·L-1)
w(锶)
/(mg·L-1)
ZK01 40 33.50~42.70 0.09~0.10
ZK02 枯水期 38 41.50~48.10 0.17~0.19
丰水期 39 38.80~41.33 0.22~0.23
Table 4  ZK01、ZK02水质分析主要指标结果
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