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天津山岭子地热田蓟县系雾迷山组热储流体同位素特征及其指示意义

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岳冬冬, 贾小丰, 张秋霞, 冯昭龙, 李胜涛. 2023. 天津山岭子地热田蓟县系雾迷山组热储流体同位素特征及其指示意义[J]. 华北地质, 46(2): 45-50. doi: 10.19948/j.12-1471/P.2023.02.07
引用本文: 岳冬冬, 贾小丰, 张秋霞, 冯昭龙, 李胜涛. 2023. 天津山岭子地热田蓟县系雾迷山组热储流体同位素特征及其指示意义[J]. 华北地质, 46(2): 45-50. doi: 10.19948/j.12-1471/P.2023.02.07
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YUE Dongdong, JIA Xiaofeng, ZHANG Qiuxia, FENG Zhaolong, LI Shengtao. 2023. The characteristics and significance of the geothermal reservior fluid isotope characteristics of the mountain group in tianjin mountain ridge. North China Geology, 46(2): 45-50. doi: 10.19948/j.12-1471/P.2023.02.07
Citation: YUE Dongdong, JIA Xiaofeng, ZHANG Qiuxia, FENG Zhaolong, LI Shengtao. 2023. The characteristics and significance of the geothermal reservior fluid isotope characteristics of the mountain group in tianjin mountain ridge. North China Geology, 46(2): 45-50. doi: 10.19948/j.12-1471/P.2023.02.07
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天津山岭子地热田蓟县系雾迷山组热储流体同位素特征及其指示意义

  • 1. 中国地质调查局水文地质环境地质调查中心, 保定 071051;

  • 2. 自然资源部地热与干热岩勘查开发技术创新中心, 保定 071000;

  • 3. 吉林大学地下水资源与环境教育部重点实验室, 长春 130021

  • 基金项目:

    中国地质调查局项目“东部地区干热岩资源调查评价（DD20221680）”；“天津东丽区—河北牛驼镇地热资源调查与试验（DD20190127）”

详细信息
    作者简介: 岳冬冬(1991-),男,工程师,硕士,毕业于吉林大学地下水科学与工程专业,现从事地热地质调查研究工作,Email:623001782@qq.com
    通讯作者: 李胜涛(1982-),男,正高级工程师,硕士,毕业于吉林大学地下水科学与工程专业,现从事地热地质调查研究工作,E-mail:li.st@163.com

  • 中图分类号: P314

The characteristics and significance of the geothermal reservior fluid isotope characteristics of the mountain group in tianjin mountain ridge

  • 1. Center of Hydrogeology and Environmental Geology, China Geological Survey, Baoding 071051, China;

  • 2. Technical Innovation Center for Geothermal and Dry Hot Rock Exploration and Development, Ministry of Natural Resources, Baoding 071000, China;

  • 3. Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China

More Information
    Corresponding author: LI Shengtao

    摘要
  • 为分析天津山岭子地热田地热流体化学成因、赋存条件及物质来源，笔者通过采集地热流体样品和测试分析, 对天津山岭子地热田蓟县系雾迷山组地热流体同位素特征进行了研究，总结了天津山岭子地热田蓟县系雾迷山组地热流体起源与形成机理。结果表明：研究区蓟县系雾迷山组地热流体87Sr/86Sr 范围为0.7113~0.7118，指示碳酸盐岩溶解成因，表现出明显的时间累积效应；蓟县系雾迷山组热储流体的40Ar/36Ar 范围为301~412，远小于幔源40Ar/36Ar，可排除其幔源物质成因。δ34S 范围为34.1‰~34.6‰，气体组分含量以氮气和甲烷为主，指示其还原环境。本文研究结果对山岭子地热田地热资源的开发利用具有借鉴参考意义。
    Abstract: In order to analyze the chemical origin, occurrence conditions and material sources of geothermal fluids in the Shanlingzi geothermal field in Tianjin, the isotopic characteristics of the geothermal fluids in the Wumishan Formation of the Jixian system in the Shanlingzi geothermal field in Tianjin were studied by collecting and testing geothermal fluid samples, and the origin and formation mechanism of the geothermal fluids in the Wumishan Formation were summarized.The results show that the87Sr/86Sr range of geothermal fluid in Wumishan Formation of Jixian system in the study area is 0.711 3~0.711 8, indicating the origin of carbonate karst decomposition and showing obvious time accumulation effect.The40Ar/36Ar range of Wumishan Formation geothermal reservior fluid in Jixian system is 301~412, which is much smaller than the mantle source40Ar/36Ar, which can exclude the mantle source material origin.The δ34S range is 34.1‰~34.6‰, and the gas components are mainly nitrogen and methane, indicating the reduction environment.The research results have certain reference significance for the development and utilization of geothermal resources in Shanlingzi geothermal field.
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    • 参考文献(41)
  • [1]

    刘前进,黄迅,董毓,等.江西邵武-河源断裂带会昌断裂控热机理研究[J].地质调查与研究,2019,42(02):154-160.

    [2]

    杨吉龙,汪大明,牛文超,等.天津地热资源开发利用前景及存在问题[J].华北地质,2022,45(03):1-6.

    [3]

    张百鸣,王心义,林建旺.天津地热田地热水的同位素特征分析[J].西部探矿工程,2006,(03):85-88.

    [4]

    高宝珠,聂瑞平,黎雪梅,等.环境同位素技术在研究天津地热流体补给和迳流中的应用[J].地下水,2009,31(04):1-3+134.

    [5]

    张锡根.天津地区地热水成因及运移特征的同位素论证[J].中国地质科学院院报,1990,(01):152-154.

    [6]

    宋美钰,刘杰,秦莉红,等.天津地热流体水化学特征及同位素分析[J].地质调查与研究,2018,41(02):138-144.

    [7]

    阮传侠,林黎,于彦,等.天津市南部平原区地热流体同位素特征[A].地温资源与地源热泵技术应用论文集(第三集)[C].北京:地质出版社,2009:25-30.

    [8]

    张素凤,高宝珠.天津地热流体形成机制及补给的环境同位素特征[A].北京地热国际研讨会论文集[C].北京:地质出版社,2002:260-265.

    [9]

    岳冬冬,李胜涛,贾小丰,等.天津山岭子地热田雾迷山组热储流体水化学特征[J].科学技术与工程,2020,20(36):14847-14853.

    [10]

    王坤,王东升.应用环境同位素研究地热水起源和补给机制[J].地质论评,2002,48(S1):203-209.

    [11]

    王啸,高亮,段喜贵,等.天津市地下水和地热流体中天然放射性核素调查与评价[J].辐射防护,2012,32(04):248-253.

    [12]

    付昌昌.淮河流域沿海平原深层地下水水化学特征及咸水成因[D].吉林大学,2015.

    [13]

    赵琪.长江下游沿海平原地下水补径排条件与水化学形成机理研究[D].吉林大学,2016.

    [14]

    马致远,范基姣.陕西渭北东部岩溶地下水中硫酸盐的形成[J].煤田地质与勘探,2005,(03):45-48.

    [15]

    朱家玲,王坤,王东升.环境同位素在研究地热资源形成过程中的应用[J].太阳能学报,2008,(03):263-266.

    [16]

    岳冬冬.沂沭河下游沿海平原地下水化学形成演化与水文地球化学模拟[D].吉林大学,2017.

    [17]

    岳冬冬,苏小四.沂沭河下游平原地下水化学及氢氧稳定同位素特征[J].科学技术与工程,2016,16(16):13-19.

    [18]

    袁利娟,张进平,何云成,等.北京市通州区地热流体水化学和同位素特征及其地热学意义[J].地质论评,2021,67(05):1545-1556.

    [19]

    PEDRONI A, HAMMERSCHMIDT K, FRIEDRICHSEN H.He, Ne, Ar, and C isotope systematics of geothermal emanations in the Lesser Antilles Islands Arc[J].Geochimica et Cosmochimica Acta, 1999, 63(3):515-532.

    [20]

    天娇,庞忠和,李义曼,等.地热气体研究进展[J].地质学报,2022,96(05):1752-1766.

    [21]

    蔺文静,刘志明,王婉丽,等.中国地热资源及其潜力评估[J].中国地质,2013,40(01):312-321.

    [22]

    李胜涛,岳冬冬,冯昭龙,等.天津东丽湖深部岩溶热储探测与储层参数研究及其开发利用潜力分析[J].中国地质,2022,49(06):1732-1746.

    [23]

    SHAND P, DARBYSHIRE D P F, LOVE A J, et al.Sr iso-topes in natural waters:Applications to source characterisation and water-rock interaction in contrasting landscapes[J].Applied Geochemistry, 2009, 24(4):574-586.

    [24]

    翟远征,王金生,左锐,等.北京平原区第四系含水层中水-岩作用的锶同位素示踪[J].科技导报,2011,29(06):17-20.

    [25]

    GAILLARDET J, Dupré B, LOUVAT P, et al.Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers[J].Chemical Geology, 1999, 159(1):3-30.

    [26]

    Négrel P.Water-granite interaction: Clues from strontium, neodymium and rare earth elements in soil and waters[J].Applied Geochemistry, 2006, 21(8):1432-1454.

    [27]

    WEN T, PINTI D L, CASTRO M C, et al.A noble gas and 87Sr/86Sr study in fluids of the Los Azufres geothermal field, Mexico-Assessing impact of exploitation and constraining heat sources[J].Chemical Geology, 2018, 483:426-441.

    [28]

    MIN M, PENG X, ZHOU X, et al.Hydrochemistry and isotope compositions of groundwater from the Shihongtan sandstone-hosted uranium deposit, Xinjiang, NW China[J].Journal of Geochemical Exploration, 2007, 93(2):91-108.

    [29]

    KARAKU, Hüseyin.Helium and carbon isotope composition of gas discharges in the Simav Geothermal Field, Turkey: Implications for the heat source[J].Geothermics, 2015, 57:213-223.

    [30]

    PANICHI C , FERRARA G C , GONFIANTINI R.Isotope geothermometry in the larderello geothermal field[J].Geothermics, 1977, 5(1-4):81-88.

    [31]

    MOORE J G, BACHELDER J N, CUNNINGHAM C G..CO 2-filled vesicles in mid-ocean basalt[J].Journal of Volcanology and Geothermal Research, 1977, (2):309 -327.

    [32]

    Veizer J ,Hoefs J.The nature of 18O/16 Oand 13C/12C secular trends in sedimentary carbonate rocks [J].Geochimica et Cosmochimica Acta, 1976, 40(11):1387-1395.

    [33]

    Hoef J.Stable Isotope Geochemistry(sixth edition)[M].Springer-Verlag.2009.

    [34]

    陶兰初,朱星强,马一奇,等.滇东老厂地区地热水成因:来自水化学和碳氢氧硫同位素的约束[J].沉积与特提斯地质,2023,43(02):295-310.

    [35]

    王松山,桑海清,裘冀.大气40Ar/36Ar 端元值及其地质意义[J].地球学报,1997,(03):90-94.

    [36]

    胡瑞忠.成矿流体氦、氩同位素地球化学[J].矿物岩石地球化学通报,1997,(02):52-56.

    [37]

    杨吉龙,柳富田,贾志,等.河北牛驼镇与天津地热田水化学和氢氧同位素特征及其环境指示意义[J].地球学报,2018,39(01):71-78.

    [38]

    洪业汤,张鸿斌,朱詠煊,等.中国大气降水的硫同位素组成特征[J].自然科学进展,1994,(06):103-107.

    [39]

    马致远,李嘉祺,翟美静,等.沉积型和火山型地热流体的同位素水文地球化学对比研究[J].水文地质工程地质,2019,46(06):9-18.

    [40]

    史杰,汪美华,马小军,等.新疆塔什库尔干县曲曼地热田地下热水同位素研究[J].地球学报,2022,43(05):645-653.

    [41]

    SIQI W, ZHAO L, JINGLI S.Hydrochemistry and H-O-CS Isotopic Geochemistry Characteristics of Geothermal Water in Nyemo-Nagqu, Tibet[J].Acta Geologica Sinica(English Edition), 2017, 91(02):644-657.

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