Geothermal geological characteristics and genesis of hot water in the central mountain area of Shandong Province

LIU Yuanqing; ZHOU Le; Lü Lin; LI Wei; WANG Xinfeng; DENG Qijun; SONG Mian; ZHENG Yidi; MA Xuemei

2020 Vol. 39, No. 12

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Article navigation > Geological Bulletin of China > 2020 > 39(12): 1908-1918

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LIU Yuanqing, ZHOU Le, Lü Lin, LI Wei, WANG Xinfeng, DENG Qijun, SONG Mian, ZHENG Yidi, MA Xuemei. Geothermal geological characteristics and genesis of hot water in the central mountain area of Shandong Province[J]. Geological Bulletin of China, 2020, 39(12): 1908-1918.

Citation:

LIU Yuanqing, ZHOU Le, Lü Lin, LI Wei, WANG Xinfeng, DENG Qijun, SONG Mian, ZHENG Yidi, MA Xuemei. Geothermal geological characteristics and genesis of hot water in the central mountain area of Shandong Province[J]. Geological Bulletin of China, 2020, 39(12): 1908-1918.

Geothermal geological characteristics and genesis of hot water in the central mountain area of Shandong Province

Center for Hydrogeology and Environmental Geology Survey, CGS, Baoding 071051, Hebei, China

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Corresponding author: Lü Lin, lvlin0207@126.com

Received Date: 10 July 2020

Revised Date: 15 October 2020

Publish Date: 25 December 2020

Abstract

Abstract

There are hot water resources distributed in Laiwu Depression, Dongping Uplift and Xinfushan Uplift of the fifth grade structural unit in the central mountain area of Shandong Province.It is found that the burial depth of hot water, the type of thermal reservoir and the genetic mechanism are varied in different structural positions.Based on the temperature measurement data of typical geothermal wells, the hydrochemical composition and isotope comparative analysis of hot water with other types of water, the authors studied and calculated the geothermal geological characteristics, hot water genesis and thermal storage temperature value.The results show that the precipitation is the source of hot water supply.The chemical types of the hot water in this area are SO₄-Na·Ca and SO₄·R-Na·Ca(R standing for Cl or HCO₃), with low δ ¹⁸O and δ D values compared with other waters.The calculated temperature value of each heat storage is lower than 100℃, suggesting a medium low temperature heat storage.The hot water is immature water, which indicates that the water rock interaction of geothermal water has not reached the ion equilibrium state, the dissolution is still in progress, or the hot water is mixed by exogenous cold water.The Lengjiazhuang geothermal system in the basin belongs to the heat conduction type, and the Anjiazhuang and Qiaogou geothermal systems in the basin margin uplifts belong to the thermal convection type.The research results provide a theoretical basis for the development of geothermal water resources in the central mountain area of Shandong Province.
- the central mountain area of Shandong Province /
- geotherm /
- Zhushadong Formation /
- hydrochemical characteristics /
- terrestrial heat flow

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References

[1]	Rybach L.Geothermal energy:sustainability and the environment[J].Geothermics, 2003, 32(4/6):463-470. Google Scholar
[2]	Lund J W, Bjelm L, Bloomquist G, et al.Characteristics, development and utilization of geothermal resources[J].Episodes, 2008, 31(1):140-147. doi: 10.18814/epiiugs/2008/v31i1/019 CrossRef Google Scholar
[3]	Lund J W, Toth A N.Direct utilization of geothermal energy 2020 worldwide review[C]//Proceedings World Geothermal Congress 2020, Reykjavik, Iceland, 2020: 1-39. Google Scholar
[4]	Zhao X G, Wan G.Current situation and prospect of Chinas geothermal resources[J].Renewable and Sustainable Energy Reviews, 2014, 32(4):651-661. Google Scholar
[5]	王贵玲, 张薇, 梁继运, 等.中国地热资源潜力评价[J].地球学报, 2017, 38(4):449-459. Google Scholar
[6]	王贵玲, 刘彦广, 朱喜, 等.中国地热资源现状及发展趋势[J].地学前缘, 2020, 27(1):1-9. Google Scholar
[7]	周总瑛, 刘世良, 刘金侠.中国地热资源特点与发展对策[J].自然资源学报, 2015, 30(7):1210-1221. Google Scholar
[8]	Jaupart C, Labrosse S, Lucazeau F, et al.Temperatures, heat, and energy in the mantle of the Earth[J].Earth Systems and Environmental Sciences, 2015, 7:223-270. Google Scholar
[9]	毛小平.地热田高温异常成因机理及温度分布特征[J].地球学报, 2018, 39(2):216-224. Google Scholar
[10]	徐军祥, 康凤新.山东省地热资源[J].中国地质, 1999, (9):30-31. Google Scholar
[11]	栾光忠, 刘红军, 刘冬雁, 等.山东半岛温泉的地热属性及其特征[J].地球学报, 2002, 23(1):79-84. doi: 10.3321/j.issn:1006-3021.2002.01.014 CrossRef Google Scholar
[12]	杨询昌, 康凤新, 王学鹏, 等.砂岩孔隙热储地温场水化学场特征及地热水富集机理——鲁北馆陶组热储典型案例[J].地质学报, 2019, 93(3):738-750. Google Scholar
[13]	蔡有兄, 钟秀燕.山东省鲁中南地区典型地热田概述[J].山东国土资源, 2015, 31(5):24-30. Google Scholar
[14]	高宗军, 孙智杰, 杨永红, 等.山东省地热水水化学研究及赋存特征[J].科学技术与工程, 2019, 19(20):85-90. Google Scholar
[15]	吴立进, 赵季初, 李艾银, 等.鲁北坳陷区地热资源开发利用关键性问题研究[J].地质与勘探, 2016, 52(2):300-306. Google Scholar
[16]	刘志涛, 刘帅, 宋伟华, 等.鲁北地区砂岩热储地热尾水回灌地温场变化特征分析[J].地质学报, 2019, 93(s1):149-157. Google Scholar
[17]	冯守涛, 王成明, 杨亚宾, 等.砂岩热储回灌对储层影响评价——以鲁西北坳陷地热区为例[J].地质学报, 2019, 93(s1):158-167. Google Scholar
[18]	刘元晴, 周乐, 李伟, 等.鲁中山区下寒武统朱砂洞组似层状含水层成因分析[J].地质论评, 2019, 65(3):653-663. Google Scholar
[19]	李少俊, 李三忠, 李玺瑶, 等.鲁西地块新生代断裂体系活动性与深部动力机制[J].海洋地质与第四纪地质, 2018, 38(4):123-134. Google Scholar
[20]	李守军, 郑德顺, 蔡进功, 等.鲁北和鲁西南地区古近纪盆地沉积特征与控制因素探讨[J].地质论评, 2003, 49(3):225-232. doi: 10.3321/j.issn:0371-5736.2003.03.001 CrossRef Google Scholar
[21]	刘元晴, 周乐, 李伟, 等.山东莱芜盆地西北缘古近系半固结含水岩组的特征及其成因[J].地球学报, 2018, 39(6):737-748. Google Scholar
[22]	康凤新, 徐军祥, 张中祥.山东省地下水资源及其潜力评价[J].山东国土资源, 2010, 26(8):4-12. doi: 10.3969/j.issn.1672-6979.2010.08.002 CrossRef Google Scholar
[23]	张增奇, 张成基, 王世进, 等.山东省地层侵入岩构造单元划分对比意见[J].山东国土资源, 2014, 30(3):1-23. doi: 10.3969/j.issn.1672-6979.2014.03.001 CrossRef Google Scholar
[24]	高宗军, 吴立进, 曹红.山东省地热资源及其开发利用[J].山东科技大学学报(自然科学版), 2009, 28(2):1-7. doi: 10.3969/j.issn.1672-3767.2009.02.001 CrossRef Google Scholar
[25]	龚育龄, 王良书, 刘绍文, 等.济阳坳陷大地热流分布特征[J].中国科学(D辑), 2003, 33(4):384-391. Google Scholar
[26]	汪集旸, 黄少鹏.中国大陆地区大地热流数据汇编(第二版)[J].地震地质, 1990, 12(4):351-366. Google Scholar
[27]	胡圣标, 何丽娟, 汪集旸.中国大陆地区大地热流数据汇编(第三版)[J].地球物理学报, 2001, 44(5):611-624. doi: 10.3321/j.issn:0001-5733.2001.05.005 CrossRef Google Scholar
[28]	姜光政, 高堋, 饶松, 等.中国大陆地区大地热流数据汇编(第四版)[J].地球物理学报, 2016, 59(8):2892-2910. Google Scholar
[29]	汪洋, 汪集旸, 熊亮萍, 等.中国大陆主要地质构造单元岩石圈地热特征[J].地球学报, 2001, 22(1):17-22. doi: 10.3321/j.issn:1006-3021.2001.01.004 CrossRef Google Scholar
[30]	刘春华, 王威, 卫润政.山东省水热型地热资源及其开发利用前景[J].中国地质调查, 2018, 5(2):51-56. Google Scholar
[31]	刘明亮, 何曈, 吴启帆, 等.雄安新区地热水化学特征及其指示意义[J].地球科学, 2020, 45(6):2221-2231. Google Scholar
[32]	史猛, 张杰, 殷焘, 等.胶东半岛中低温对流型地热资源水化学特征分析[J].地质学报, 2019, 93(s1):138-148. Google Scholar
[33]	Giggenbach W F.Geothermal solute equilibria.Derivation of Na-K-Mg-Ca geoondicators[J].Geochimica et Cosmochimica Acta, 1988, 52(12):2749-2765. doi: 10.1016/0016-7037(88)90143-3 CrossRef Google Scholar
[34]	袁利娟, 孔祥军, 高剑, 等.北京市延庆地热田成因模式[J].地质论评, 2020, 66(4):933-941. Google Scholar
[35]	李泓泉, 张树胜, 谢明忠, 等.冀西北蔚县盆地地热资源赋存特征及勘查开发方向[J].地质论评, 2020, 66(4):919-932. Google Scholar
[36]	Fournier R O.Chemical geothermometers and mixing models for geothermal systems[J].Geothermics, 1977, 5:31-40. Google Scholar
[37]	袁利娟, 杨峰田.北京迭断陷内蓟县系热储层温度分布特征[J].吉林大学学报(地球科学版), 2017, 47(1):179-188. Google Scholar
[38]	Langelier W F, Ludwig H F.Graphical methods for indicating the mineral character of natural waters[J].Journal of the American water works association, 1942, 34(3):335-352. Google Scholar
[39]	Vaselli O, Minissable A, Tassi F, et al.A geochemical traverse across the Eastern Carpathians(Romania):constraints on the origin and evolution of the mineral water and gas discharges[J].Chemical Geology, 2002, 182(2):637-654. Google Scholar
[40]	柯柏林, 林天懿, 李文, 等.北京西山谷积山背斜地热系统成因模式及远景区预测[J].地质通报, 2019, 38(8):1378-1385. Google Scholar
[41]	王贵玲, 蔺文静.我国主要水热型地热系统形成机制与模式[J].地质学报, 2020, 94(7):1923-1937. Google Scholar
[42]	Muffler L J P.Tectonic and hydrological control of the nature and distribution of geothermal resources[C]//Proceedings, second U.N.symposium on the development and use of geothermal resources, Washington D.C: Government Printing Office, 1976: 499-507. Google Scholar
①	山东省地矿工程勘察院.山东省泰莱盆地地热资源成热预测研究报告.2010. Google Scholar
②	山东省地质矿产局第一地质队.山东省肥城市安驾庄地热田详查地质报告.1995. Google Scholar
③	山东省第一地质矿产勘查院.山东省泰安市岱岳区徂徕镇地热资源普查报告.2003. Google Scholar