典型岩溶温泉群水文地球化学特征

doi:10.7523/j.issn.2095-6134.2016.03.018

中国科学院大学学报 ›› 2016, Vol. 33 ›› Issue (3): 403-411.DOI: 10.7523/j.issn.2095-6134.2016.03.018

典型岩溶温泉群水文地球化学特征

雷琨¹, 何守阳^1,2, 安艳玲^1,2

1. 贵州大学喀斯特环境与地质灾害防治教育部重点实验室, 贵阳 550025;
2. 贵州大学资源与环境工程学院, 贵阳 550025

收稿日期:2015-07-10 修回日期:2015-11-23 发布日期:2016-05-15
通讯作者: 何守阳
基金资助:
贵州省科技厅重点基金(黔科合JZ字[2014]2006号、黔科合计Z字[2012]4012号、黔科合J字[2011]2037号)和贵州大学人才引进项目(贵大人基合字(2010)046号)资助

Hydrogochemical characteristics of thermal spring group in typical karst region

LEI Kun¹, HE Shouyang^1,2, AN Yanling^1,2

1. Key Laboratory of Karst Environmentand Geohazard Prevention of Ministry of Education, Guizhou University, Guiyang 550025, China;
2. College of Resources and Environmental Engineering,Guizhou University,Guiyang 550025, China

Received:2015-07-10 Revised:2015-11-23 Published:2016-05-15

摘要/Abstract

摘要：

石阡县岩溶温泉群因富含矿物质和微量元素蕴涵着极高的商业价值.采集和收集不同时期石阡岩溶温泉群的水化学分析数据进行综合分析.研究表明:石阡温泉群主要的阳离子为Ca²⁺和Mg²⁺,主要的阴离子为HCO₃^-和SO₄^2-,水化学类型为HCO₃-Ca·Mg型、HCO₃·SO₄-Ca·Mg型和SO₄·HCO₃-Ca·Mg型,水质偏碱性,温泉群的补给源为大气降水.水文地球化学特征受控于大气降水入渗深循环过程中的水-岩相互作用.HCO₃-Ca·Mg型温泉由白云岩和方解石等碳酸盐矿物溶解所致;HCO₃·SO₄-Ca·Mg型和SO₄·HCO₃-Ca·Mg型则受控于岩溶含水层中的膏盐层溶解.

关键词: 温泉群, 岩溶, 水文地球化学, 石阡县

Abstract:

Karst thermal spring group in Shiqian county has a high commercial value due to the rich minerals and trace elements. The water chemistry data in different periods are collected and analyzed to study hydrogochemical characteristics of the thermal spring group in Shiqian county. The results indicate that Ca²⁺and Mg²⁺ are the major cations and the major anions are SO^2-₄ and HCO^-₃. The thermal springs are alkaline water and recharged by precipitation. The hydrochemical types are SO₄ ·HCO₃-Ca ·Mg, HCO₃ ·SO₄-Ca ·Mg, and HCO₃-Ca ·Mg. Water chemistry types of thermal spring group are controlled by the water-rock interaction in the process of precipitation infiltration into deep water cycle. The thermal spring of the HCO₃-Ca · Mg type is predominated by carbonate minerals dissolution, and the HCO₃ · SO₄ -Ca · Mg or the SO₄ · HCO₃-Ca · Mg types are controlled by the dissolution of sulfate evaporates in karst aquifer.

Key words: thermal spring group, karst, hydrogeochemistry, Shiqian county

中图分类号:

P592

雷琨, 何守阳, 安艳玲. 典型岩溶温泉群水文地球化学特征[J]. 中国科学院大学学报, 2016, 33(3): 403-411.

LEI Kun, HE Shouyang, AN Yanling . Hydrogochemical characteristics of thermal spring group in typical karst region[J]. , 2016, 33(3): 403-411.

参考文献

[1] Ellis A J, Mahon W A J. Natural hydrothermal systems and experimental hot water/rock interactions[J].Geochim Cosmochim Acta, 1964,28:1 323-1 357.
[2] Giggenbach W F. Geothermal solute equilibrium: Derivation of Na-K-Mg-Ca geoindieatiors[J]. Geochimica Cosmochimica Acta, 1988,52:2 749-2 756.
[3] Steinbruch F, Merkel B J. Characterization of a Pleistocene thermal spring in Mozambique[J]. Hydrogeology Journal, 2008,16(8):1 655-1 668.
[4] Goldscheider N, Madl-Szonyi J, Eross A, et al. Review: thermal water resources in carbonate rock aquifers[J].Hydrogeology Journal, 2010,18(6):1 303-1 318.
[5] Haile T, Abiye T A.The interference of a deep thermal system with a shallow aquifer: the case of Sodere and Gergedi thermal springs, Main Ethiopian Rift, Ethiopia[J].Hydrogeology Journal, 2012,20(3):561-574.
[6] Petrini R, Italiano F, Ponton M, et al. Geochemistry and isotope geochemistry of the Monfalcone thermal waters (northern Italy): inference on the deep geothermal reservoir[J]. Hydrogeology Journal, 2013,21(6):1 275-1 287.
[7] Busby J. Geothermal energy in sedimentary basins in the UK[J]. Hydrogeology Journal, 2014,22(1):129-141.
[8] Afsin M, Allen D M, Kirste D, et al. Mixing Processes in hydrothermal spring systems and implications for interpreting geochemical data: a case study in the Cappadocia region of Turkey[J]. Hydrogeology Journal, 2014, 22(1):7-23.
[9] 张世从,聂跃平.贵州省石阡县热矿水普查评价报告 . 六盘水:贵州省地矿局113地质大队,1985.
[10] 陈履安, 张世从.贵州石阡地区矿泉水的同位素年龄研究[J]. 贵州地质, 1997(3):274-278.
[11] 张世从, 陈履安.贵州石阡地区热矿水同位素地球化学研究[J].地质论评,1992(5):457-466.
[12] 杨荣康, 杨丽君, 王乾, 等.贵州石阡地热田地热资源量计算[J]. 贵州地质, 2014(2):154-157.
[13] 毛健全.喀斯特环境与贵州温泉.喀斯特环境研究[M].贵阳:贵州人民出版社. 1988: 51.
[14] 张世从,杨剑明.贵州省石阡县饮用矿泉水水资源评价及开发利用研究 . 贵阳:贵州省地质矿产局地质科学研究所,1988.
[15] 何守阳.石阡县温泉资源评价 . 贵阳:贵州大学,2005.
[16] Piper A M.A graphic procedure in the geochemical interpretation of water-analyses, Transactions[J]. American Geophysical Union, 1944,25:914-923.
[17] 何守阳, 朱立军, 董志芬, 等. 典型岩溶地下水系统地球化学敏感性研究[J]. 环境科学, 2010, 31(5): 1 178-1 182.
[18] 陈履安, 张世从. 贵州碳酸盐建造中热矿水有关成分的相关特征及其成因探讨[J]. 贵州地质, 1993(3):249-256.
[19] 吕金波, 车用太, 王继明, 等. 京北地区热水水文地球化学特征与地热系统的成因模式[J]. 地震地质, 2006, 28(3): 419- 429.
[20] 周海燕, 周训, 姚锦梅. 广东从化温泉的水文地球化学模拟[J]. 现代地质, 2007(4):619-623.
[21] 张卫民. 水文地球化学方法在赣南横径地区地热水成因分析中的应用[J]. 水文地质工程地质, 2001(4):45-48.
[22] 李义连, 周来茹. 地下水矿物饱和度的水文地球化学模拟分析-以娘子关泉域岩溶水为例[J]. 地质科技情报, 2002, 21(1): 32-36.
[23] Craig H. Isotopic variations in meteoric waters[J]. Science, 1961, 133(3 465):1 702-1 703.
[24] 刘进达, 赵迎昌. 中国大气降水稳定同位素时-空分布规律探讨[J]. 勘察科学技术, 1997 (3): 34-39.
[25] 于永亭, 李晓, 郭爽. 云南省龙陵地区温泉水化学特征及其成因分析[J]. 广东微量元素科学, 2008(2):39-46.
[26] 杜毓超, 吕勇,罗贵荣. 滇西潞西盆地温泉水文地球化学特征及其成因[J]. 地质通报, 2012(Z1):406-412.
[27] 沈照理, 王焰新, 郭华明. 水-岩相互作用研究的机遇与挑战[J]. 地球科学: 中国地质大学学报, 2012, 37(2): 207-219.
[28] Gibbs R J. Mechanisms controlling world water chemistry[J].Science,1970,170:1 088-1 090.
[29] Huang G X, Sun J C, Zhang Y,et al. Impact of anthropogenic and natural processes on the evolution of groundwater chemistry in a rapidly urbanized coastal area, South China[J]. Science of The Total Environment, 2013,463-464: 209-221.
[30] Pu J B, Cao M, Zhang Y Z, et al. Hydrochemical indications of human impact on karst groundwater in a subtropical karst area, Chongqing, China[J].Environmental Earth Sciences, 2014, 72(5): 1 683-1 695.
[31] 邵天杰, 赵景波,董治宝.巴丹吉林沙漠湖泊及地下水化学特征[J].地理学报, 2011(5): 662-672.

典型岩溶温泉群水文地球化学特征

Hydrogochemical characteristics of thermal spring group in typical karst region

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