Environmental Chemistry

ISSN 0254-6108

CN 11-1844/X

Vol. 38 No. 5
May  2019
Article Contents

Citation:

Hydrochemical characterization of thermal spring waters in the deep fault region in western Guangdong

  • Received Date: 2018-10-18
    Fund Project:

    Supported by the National Natural Science Foundation of China(41572241).

  • Through the study of the hydrogeochemical characteristics of the hot springs in the deep fault of the western Guangdong (namely Xinyi-Lianjiang deep fault zone), it was revealed that the water chemical components were mainly the dissolution control of silicate minerals, and the Na-K-Mg diagram showed that the hot spring water-rocks interactions were in an unbalanced state. Meanwhile, the thermal storage temperature was estimated to be between 63.2-122.5℃, and the circulation depth was in the range of 1453-3430 m. Our results could provide a basis for further exploration of the relationship between geothermal water and deep faults, as well as shallow geological structures, hydrogeological conditions, and geothermal resource development.
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  • [1] 严克涛,卢国平.温泉流量变化反映固体潮对深大断裂导水性的影响[J].地质科技情报,2017,36(2):229-235. YAN K T, LU G P. The variation of hot spring flow reflects the influence of solid tide on the water conductivity of deep faults[J]. Geological Science and Technology, 2017,36(2):229-235(in Chinese).
    [2] LU G, LIU R. Aqueous chemistry of typical geothermal springs with deep faults in Xinyi and Fengshun in Guangdong Province, China[J]. Journal of Earth Science, 2015, 26(1):60-72.
    [3] BAI Y Z, ZHOU Q, XU X W. The effect of fault slide velocity on the strong earthquake recurrence:A case study on Kusaihu and Xidatan segment of east Kunlun fault zone[J]. Progress in Geophysics, 2013, 28(3):1320-1328.
    [4] 黄元敏,杜龙,邵叶,等.信宜-廉江断裂地震活动状态分析[J].华南地震,2016,36(4):14-19. HUANG Y M, DU L, SHAO Y et al. Analysis of seismic activity status of Xinyi-Lianjiang fault[J]. South China Journal of Seismology, 2016, 36(4):14-19(in Chinese).
    [5] 袁建飞.广东沿海地热系统水文地球化学研究[D].武汉:中国地质大学,2013. YUAN J F. Hydrogeochemical study of coastal geothermal system in Guangdong[D]. Wuhan:China University of Geosciences, 2013(in Chinese).
    [6] 南颐,周国强.广东省岩石地层[M].武汉:中国地质大学出版社,1996. NAN Y, ZHOU G Q. Rock strata in Guangdong Province[M]. Wuhan:China University of Geosciences Press, 1996(in Chinese).
    [7] 广东省地质矿产局.广东省区域地质志[M].北京:地质出版社,1988. Guangdong Bureau of Geology and Mineral Resources. Regional geology of Guangdong Province[M]. Beijing:Geological Publishing House, 1988(in Chinese).
    [8] 朱长生.广东省断裂构造对地下热水的控制作用[J].水文地质工程地质,1982,26(6):17-41. ZHU C S. Controlling effect of fault structure on underground hot water in Guangdong Province[J]. Hydrogeology and Engineering Geology, 1982, 26(6):17-41(in Chinese).
    [9] LI J, SAGOE G, YANG G et al. Evaluation of mineral-aqueous chemical equilibria of felsic reservoirs with low-medium temperature:A comparative study in Yangbajing geothermal field and Guangdong geothermal fields[J]. Journal of Volcanology and Geothermal Research, 2018, 352:92-105.
    [10] LU G, WANG X, LI F et al. Deep geothermal processes acting on faults and solid tides in coastal Xinzhou geothermal field, Guangdong, China[J]. Physics of the Earth and Planetary Interiors, 2017, 264:76-88.
    [11] 林云存.广东信宜1,2号井水温的同震响应及机理初步探讨[J].华南地震,2012,32(2):133-137. LIN Y C. Study on the coseismic response and mechanism of water temperature in No.1 and No.2 wells in Xinyi, Guangdong[J].South China Earthquake,2012,32(2):133-137(in Chinese).
    [12] 杜秀荣,唐建军.中国地图集[M].北京:中国地图出版社,2012. DU X R, TANG J J. China Atlas[M]. Beijing:China Map Press, 2012(in Chinese).
    [13]
    [14] 杨雷,肖琼,沈立成,等.不同地质背景地热系统水-岩作用下温泉水的地球化学特征——以重庆市温塘峡背斜温泉、滇东小江断裂带温泉为例[J].中国岩溶,2011,30(2):209-215. YANG L, XIAO Q, SHEN L C et al. Geochemical characteristics of hot spring water under the action of water-rock under different geological background geothermal processes:taking the Wentangxia anticline hot spring in Chongqing and the Xiaojiang fault zone of Diandong as an example[J]. China Karst, 2011, 30(2):209-215(in Chinese).
    [15] 姚永仲.弥渡温泉地质特征及成因模式分析[D].昆明:昆明理工大学,2010. YAO Y Z. Analysis of geological characteristics and genetic model of Midu Hot Spring[D]. Kunming:Kunming University of Science and Technology, 2010(in Chinese).
    [16] 王皓,柴蕊.地热温标在地热系统中的应用研究[J].河北工程大学学报,2009,26(3):54-58. WANG H, CHAI R. Application of geothermal temperature scale in geothermal system[J]. Journal of Hebei University of Engineering, 2009,26(3):54-58(in Chinese).
    [17] REED M, SPYCHER N. Calculation of pH and mineral equilibria in hydrothermal waters with application to geothermometry and studies of boiling and dilution[J]. Geochimica et Cosmochimica Acta, 1984, 48(7):1479-1492.
    [18] 许万才.饱和指数法在地下热水化学研究中的应用[J]. 西安地质学院学报,1992,14(3):66-70. XU W C. Application of saturated index method in chemistry research of underground hot water[J]. Journal of Xi'an Institute of Geology, 1992, 14(3):66-70(in Chinese).
    [19]
    [20] 张保建.鲁西北地区地下热水的水文地球化学特征及形成条件研究[D].北京:中国地质大学,2011. ZHANG B J. Hydrogeochemical characteristics and formation conditions of underground hot water in northwestern Shandong[D]. Beijing:China University of Geosciences, 2011(in Chinese).
    [21] 沈照理,朱宛华,钟佐燊.水文地球化学基础[J].水文地质工程地质,1983,27(6):56-60. SHEN Z L, ZHU W H, ZHONG Z S. Hydrogeochemical foundation[J]. Hydrogeology and Engineering Geology, 1983, 27(6):56-60(in Chinese).
    [22] 赵江涛,周金龙,梁川,等.新疆焉耆盆地平原区地下水演化的主要水文地球化学过程分析[J].环境化学,2017,36(6):1397-1406. ZHAO J T, ZHOU J L, LIANG C et al. Analysis of main hydrogeochemical processes of groundwater evolution in the plain area of Yanqi Basin, Xinjiang[J]. Environmental Chemistry, 2017, 36(6):1397-1406(in Chinese).
    [23] 田西昭,单强,宋利震.唐山沿海地区地下水化学特征及演化趋势分析[J].南水北调与水利科技, 2011, 9(1):139-144. TIAN X Z, SHAN Q, SONG L Z. Analysis of groundwater chemical characteristics and evolution trends in coastal areas of Tangshan[J]. South-to-North Water Transfer and Water Conservancy Technology, 2011, 9(1):139-144(in Chinese).
    [24] 徐国芳,马致远.锶同位素演化对深层地下热水的指示意义[J].地下水,2013,35(4):20-23. XU G F, MA Z Y. Indicative significance of strontium isotope evolution to deep underground hot water[J]. Groundwater, 2013, 35(4):20-23(in Chinese).
    [25] 叶萍,金勤胜,周爱国等.河北平原地下水锶同位素形成机理[J].地球科学:中国地质大学学报, 2008,3(1):137-144. YE P, JIN Q S, ZHOU A G et al. Formation mechanism of strontium isotope in groundwater in Hebei Plain[J]. Earth Science:Journal of China University of Geosciences, 2008, 3(1):137-144(in Chinese).
    [26] FISHER R S, STUEBER A M. Strontium isotopes in selected streams within the Susquehanna River basin[J]. Water Resources Research, 1976, 12(5):1061-1068.
    [27] MILLOT R, GAILLARDET J, DUPRÉ B et al. The global control of silicate weathering rates and the coupling with physical erosion:new insights from rivers of the Canadian Shield[J]. Earth and Planetary Science Letters, 2002, 196(1-2):83-98.
    [28] VEIZER J. Strontium isotopes in seawater through time[J]. Annual Review of Earth and Planetary Sciences, 1989, 17(1):141-167.
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Hydrochemical characterization of thermal spring waters in the deep fault region in western Guangdong

  • Institute of Groundwater and Earth Sciences, Jinan University, Guangzhou, 510632, China
Fund Project:  Supported by the National Natural Science Foundation of China(41572241).

Abstract: Through the study of the hydrogeochemical characteristics of the hot springs in the deep fault of the western Guangdong (namely Xinyi-Lianjiang deep fault zone), it was revealed that the water chemical components were mainly the dissolution control of silicate minerals, and the Na-K-Mg diagram showed that the hot spring water-rocks interactions were in an unbalanced state. Meanwhile, the thermal storage temperature was estimated to be between 63.2-122.5℃, and the circulation depth was in the range of 1453-3430 m. Our results could provide a basis for further exploration of the relationship between geothermal water and deep faults, as well as shallow geological structures, hydrogeological conditions, and geothermal resource development.

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