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物探与化探  2019, Vol. 43 Issue (4): 741-748    DOI: 10.11720/wtyht.2019.1400
     地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
武汉城市圈岩溶热储水化学特征及水—岩作用研究
牛俊强1, 范威1, 郭昆1,2
1. 湖北省地质环境总站,湖北 武汉 430034
2. 中国地质大学(武汉) 环境学院,湖北 武汉 430074
A study of chemical characteristics and water-rock interaction of karstic geothermal reservoir in Wuhan city circle
Jun-Qiang NIU1, Wei FAN1, Kun GUO1,2
1. Geological Environmental Center of Hubei Province,Wuhan 430034,China
2. China University of Geosciences,School of Environmental Studies,Wuhan 430074,China
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摘要 

根据武汉城市圈岩溶热储地热田的地下热水水化学数据,总结了岩溶热水的水化学类型,分析了岩溶热水中主要组分随温度的变化特征,重点研究了水—岩作用程度和作用时间的关系,系统分析了热水中主要离子的水化学作用过程。研究结果表明,热水中主要组分含量受温度和水岩作用过程控制,TDS含量随水岩作用时间的增加而增加,随着TDS含量的增加,水岩作用受碳酸盐溶解控制逐渐转变为受硫酸盐溶解控制,高TDS时,盐岩溶解作用加强;浪口、五洪山、蛇屋山地热田属同一个岩溶水流系统,汤池地热田、马口地热井属同一个水流系统,其他地热田属各自独立的水流系统。

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牛俊强
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关键词 岩溶热储水化学特征水—岩作用;武汉城市圈    
Abstract

Based on the geothermal water hydrochemical data of karst geothermal fields of Wuhan urban agglomeration, the authors summarized the hydrochemical type of karst hot mineral water, analyzed the variation characteristics of main components of karst hot mineral water with temperature, studied the relationship between the degree and time of water-rock action, and analyzed the hydrochemical processes of the main ions in hot water. The results show that the content of main components in hot water is controlled by temperature and water-rock interaction process, the total dissolved solids content increases with the increase of water-rock action time. As the total dissolved solids content increases, the water-rock interaction was gradually transformed from carbonate dissolution to sulfate dissolution, at high total dissolved solids, the dissolution of salt rocks is enhanced. the Langkou geothermal field, the Wuhongshan geothermal field and the Shewushan geothermal field belong to the same water flow system, the Tangchi geothermal field and the Makou geothermal well belong to the same water flow system, and other geothermal fields belong to separated water flow systems.

Key wordskarstic geothermal reservoir    chemical characteristics    water-rock interaction    Wuhan city circle
收稿日期: 2018-11-02      出版日期: 2019-08-15
:  P632  
基金资助:2017年度湖北省国土资源科学技术研究计划(ETZ2017A03)
作者简介: 牛俊强(1981-),男,高级工程师,水文地质、工程地质专业,主要从事地热地质研究工作。Email: 524279545@qq.com
引用本文:   
牛俊强, 范威, 郭昆. 武汉城市圈岩溶热储水化学特征及水—岩作用研究[J]. 物探与化探, 2019, 43(4): 741-748.
Jun-Qiang NIU, Wei FAN, Kun GUO. A study of chemical characteristics and water-rock interaction of karstic geothermal reservoir in Wuhan city circle. Geophysical and Geochemical Exploration, 2019, 43(4): 741-748.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2019.1400      或      https://www.wutanyuhuatan.com/CN/Y2019/V43/I4/741
序号 地热田 补给区 相对补给区位置 水温/℃ 热储岩性 水质资料/份
1 咸宁市温泉 大幕山区 北西9 km 51 奥陶系硅化灰岩 79
2 嘉鱼蛇屋山 大幕山区 北西50 km 57 奥陶系白云质灰岩 5
3 赤壁五洪山 大幕山区 北西40 km 57 奥陶系中统硅化灰岩 8
4 黄石市胡家湾煤矿 黄荆山 北西1.5 km 35 三叠—石炭系灰岩、炭质灰岩 1
5 大冶章山 37 寒武系白云岩、白云质灰岩 2
6 应城汤池 大洪山区 南东20 km 55 震旦系白云岩、硅质白云岩 2
7 洪湖乌林 大药姑山区 北西40 km 60 二叠系白云质灰岩 10
8 崇阳浪口 大幕山区 西15 km 47 寒武系硅化白云岩 14
9 武汉三门湖 青龙山 南西2 km 27 石炭—二叠系的碳酸盐岩 1
10 通山西坑 大幕山区 南西0.5 km 27 寒武系和奥陶系灰岩 2
11 汉川马口地热井 大洪山区 南东70 km 52 寒武—奥陶系碳酸盐岩 2
12 天门张港地热井 大洪山区 南西40 km 65 震旦—寒武系碳酸盐岩 1
13 武汉武5井 封存水 37.5 寒武—奥陶系碳酸盐岩 1
Table 1  武汉城市圈岩溶热储地热田基本情况[9,10,11,12]
Fig.1  岩溶热水与冷泉水三线图(下文中各图图例同本图)
Fig.2  岩溶热水主要组分与温度关系
Fig.3  Na-K-Mg平衡图
Fig.4  14C表观年龄与TDS关系图
Fig.5  岩溶热水主要组分与TDS关系
Fig.6  岩溶热水HCO3-与Ca2+、Mg2+浓度对比
Fig.7  岩溶热水Ca2+与Mg2+浓度对比
Fig.8  岩溶热水SO42-与Ca2+浓度对比
Fig.9  岩溶热水Cl-与Na+浓度对比
Fig.10  岩溶热水Sr2+与Ca2+浓度对比
Fig.11  岩溶热水F-与HCO3-浓度对比
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