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| Characteristics of geothermal field and terrestrial heat flow in the northern Pingyin County of Shandong Province |
| LU Zhaoqun |
| China Chemical Geology and Mine Bureau, Shandong Geological Prospecting Institute, Shandong Ji'nan 250013,China |
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Abstract In recent years, geothermal resources were explored in the structural fissures of metamorphic rocks of Taishan Group in the northern Pingyin County of Shandong Province. It is of great significance to analyze and study the characteristics of geothermal field, terrestrial heat flow and radiogenic heat production rate of rocks, for predicting and evaluating the formation potential of geothermal resources. Based on the borehole temperature data and the test data of water and rock samples, the authors systematically analyzed the characteristics of the geothermal field in the study area, and calculated the terrestrial heat flow and the radiogenic heat production rate of the metamorphic rocks of Taishan Group. Besides, the silica heat flow in the study area was calculated based on to the SiO2 content in the groundwater. The research show that average geothermal gradient of the overlying strata in the study area was 2.07 ℃/100 m, and the average geothermal gradient of the metamorphic rocks of Taishan Group was 2.18 ℃/100 m, with the lateral distribution of low in the west and high in the east, and the vertical distribution of increasing with depth. The geothermal heat flow value of the metamorphic rocks of Taishan Group in the study area is lower than the average geothermal heat flow in China mainland, indicating a low heat flow background. The silicon heat flow value in the study area is slightly higher than the measured borehole data. The radiogenic heat production rate of Taishan Group is low, and Taishan Group belongs to low heat-producing rock mass. Comprehensive analysis shows that the geothermal field distribution is mainly affected by regional geological structures and stratigraphic structures. The geothermal distribution is generally within the normal range, but it has a relatively low heat flow background in the study area. The heat source is mainly conductive heat generation, followed by rock radioactive heat generation. The research results could provide some basic data and scientific basis for future research on geothermal geological conditions in the study area and subsequent exploration and development work.
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Received: 22 March 2023
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[1] 邱楠生. 中国西北部盆地岩石热导率和生热率特征[J].地质科学, 2002,37(2):196-206.
Qiu N S.Characters of thermal conductivity and radiogenic heat production rate in basins of northwest China[J].Chinese Journal of Geology,2002,37(2):196-206.
[2] 田禹. 山东及周边邻省大地热流值特征研究-热流值与计算段深度关系分析[J].国土与自然资源研究,2017(1):74-76.
Tian Y.Research on the characteristics of geothermal flux value in Shandong and its neighboring province- analysis on geothermal flux value and the relationship on the depths of calculations[J].Territory & Natural Resources Study,2017(1):74-76.
[3] 雷晓东,胡圣标,李娟,等.北京平原区西北部大地热流与深部地温分布特征[J].地球物理学报,2018,61(9):3735-3748.
Lei X D,Hu S B,Li J,et al.Characteristics of heat flow and geothermal distribution in the northwest Beijing plain[J].Chinese Journal of Geophysics,2018,61(9):3735-3748.
[4] 刘峰,王贵玲,张薇,等.江西宁都县北部大地热流特征及地热资源成因机制[J].地质通报,2020,39(12):1883-1890.
Liu F,Wang G L,Zhang W,et al.Terrestrial heat flow and geothermal genesis mechanism of geothermal resources in northern Ningdu County,Jiangxi Province[J].Geological Bulletin of China,2020,39(12):1883-1890.
[5] 张超,胡圣标,宋荣彩,等.共和盆地干热岩地热资源的成因机制:来自岩石放射性生热率的约束[J].地球物理学报,2020,63(7):2697-2709.
Zhang C,Hu S B,Song R C,et al.Genesis of the hot dry rock geothermal resources in the Gonghe basin:constraints from the radiogenic heat production rate of rocks[J].Chinese Journal of Geophysics,2020,63(7):2697-2709.
[6] 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.
Jiang G Z,Gao P,Rao S,et al.Compilation of heat flow data in the continental area of China (4th edition)[J].Chinese Journal of Geophysics,2016,59(8):2892-2910.
[7] 杨义栋,刘彦兵,赵盼,等.周口凹陷区地温场特征及影响因素分析[J].中国矿业,2021,30(3):231-236.
Yang Y D,Liu Y B,Zhao P,et al.Analysis of geothermal field characteristics and influencing factors in Zhoukou Depression area[J].China Mining Magazine,2021,30(3):231-236.
[8] 张伟,蔡铁刚,王瑞君.新安煤田中深部地温场特征及其影响因素[J].地质与勘探,2020,56(4):802-808.
Zhang W,Cai T G,Wang R J.Characteristics and influencing factors of geothermal field in the middle and deep part of Xin'an Coalfield[J].Geology and Exploration,2020,56(4):802-808.
[9] 黄起伟,刘金辉,刘峰,等.江西主要产热岩体岩石放射性生热率特征初探[J].矿产与地质,2021,35(5):918-922.
Huang Q W,Liu J H,Liu F,et al.Study on the characteristics of radioactive heat generation rate of some heat-producing rock masses in Jiangxi[J].Mineral Resources and Geology,2021,35(5):918-922.
[10] 谭现锋,王浩,张震宇.山东省陈庄潜凸起区地温场特征与泰山岩群放射性元素生热率[J].科技导报,2015,33(19):58-61.
Tan X F,Wang H,Zhang Z Y.Geothermal field characteristics and heat generation rate of radioactive elements in Taishan rock group at Chenzhuang uplift,Shandong Province[J].Science & Technology Review,2015,33(19):58-61.
[11] 刘道荣,林荣吉.浙江燕山期花岗岩类放射性生热率特征研究[J].华东地质,2019,40(1):19-26.
Liu D R,Lin R J.Characteristic study of radioactive heat generation of the Yanshanian granitoids in Zhejiang[J].East China Geology,2019,40(1):19-26.
[12] 卢兆群,彭明章,董妍,等.山东平阴地热水水文地球化学特征及成因分析[J].中国地质调查,2022,9(1):104-114.
Lu Z Q,Peng M Z,Dong Y,et al.Hydrogeochemical characteristics and genesis analysis of geothermal water in Pingyin of Shandong Province[J].Geological Survey of China,2022,9(1):104-114.
[13] 王朱亭,张超,姜光政,等.雄安新区现今地温场特征及成因机制[J].地球物理学报,2019,62(11):4313-4322.
Wang Z T,Zhang C,Jiang G Z,et al.Present-day geothermal field of Xiongan New Area and its heat source mechanism[J].Chinese Journal of Geophysics,2019,62(11):4313-4322.
[14] 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.
Wang J Y,Huang S P.Compilation of heat flow data in the China continental area (2nd edition)[J].Seismology and Geology,1990,12(4):351-366.
[15] 孙猛,刘峰,陆川,等.河北省承德地区大地热流[J].科学技术与工程,2020,20(25):10144-10150.
Sun M,Liu F,Lu C,et al.Terrestrial heat flow in Chengde,Hebei Province[J].Science Technology and Engineering,2020,20(25):10144-10150.
[16] 李文. 北京通州地温场特征及其影响因素[J].地质通报,2021,40(7):1189-1194.
Li W.Geothermal field in Tongzhou District of Beijing and its influencing factors[J].Geological Bulletin of China,2021,40(7):1189-1194.
[17] 韩昱,颜丙生,丁冠涛,等.平阴县玫瑰镇大孙庄地区氡泉地热资源潜力调查评价报告[R].济南:山东省地矿工程勘察院,2019.
Han Y,Yan B S,Ding G T,et al.Investigation and Evaluation Report On the Potential of Radon Spring Geothermal Resources in Dashunzhuang Area,Rose Town,Pingyin County[R].Jinan:Shandong Geological and Mineral Engineering Survey Institute,2019.
[18] 徐军祥,刘桂仪,任书才.山东省地热资源及其开发利用的生态环境意义[C]//刘时彬,李宝山,郑克棪.全国地热产业可持续发展学术研讨会论文集.北京:化学工业出版社,2005:81-87.
Xu J X,Liu G Y,Ren S C.The eco-environmental significance of geothermal resources and their development and utilization in Shandong province[C]//Liu S B,Li B S,Zheng K Y.Proceedings of National Symposium on Sustainable Development of Geothermal Industry.Beijing:Chemical Industry Press,2005:81-87.
[19] 马杏垣,刘昌铨,刘国栋.江苏响水至内蒙古满都拉地学断面[J].地质学报,1991(3):199-215.
Ma X Y,Liu C Q,Liu G D.Xiangshui (Jiangsu province) to mandal (Nei Monggol) geoscience transect[J].Acta Geologica Sinica,1991(3):199-215.
[20] Swanberg C A,Morgan P.The linear relation between temperatures based on the silica content of groundwater and regional heat flow:A new heat flow map of the United States[J].Pure and Applied Geophysics,1978,117(1-2):227-241.
[21] Swanberg C A,Morgan P.The silica heat flow interpretation technique:assumptions and applications[J].Journal of Geophysical Research:Solid Earth,1980,85(B12):7206-7214.
[22] Swanberg C A,Morgan P.Heat flow map of the United States based on silica geo thermometry[M]//Touloukian W R,et al.Physical Properties of Rock and Minerals.[s.l.]:McGraw Hill,1981:540-545.
[23] 万天丰. 华南硅热流值[J].科学通报,1986,31(16):1247-1249.
Wan T F.Silica heat flow value of South China[J].Chinese Science Bulletin,1986,31(16):1247-1249.
[24] 童永福,林松生,郑蔚雯,等.福建硅热流值[J].福建地质,1986,5(3):53-59.
Tong Y F,Lin S S,Zheng W W,et al.Silica heat flow value of Fujian[J].Geology of Fujian,1986,5(3):53-59.
[25] 李学伦,刘保华,孙效功,等.山东半岛硅热流值与区域地质条件的关系[J].青岛海洋大学学报,1997,27(1):77-85.
Li X L,Liu B H,Sun X G,et al.Relationship between the silica heat flow and regional geological conditions in Shandong pen-insula[J].Journal of Ocean University of Qingdao,1997,27(1):77-85.
[26] 张知非. 川西硅热流[J].大自然探索,1987,6(1):130-135.
Zhang Z F.Silica heat flow in western Sichuan province[J].Exploration of Nature,1987,6(1):130-135.
[27] 刘鸿俊. 西安地区的硅热流[J].西安地质学院学报,1986,8(4):28-33.
Liu H J.On the silicon heat flow in Xi'an Area[J].Journal of Xi'an College of Geology,1986,8(4):28-33.
[28] 国家卫生健康委员会,国家市场监督管理总局.GB 8538—2022 食品安全国家标准饮用天然矿泉水检验方法[S].北京:中国标准出版社,2022.
National Health Commission of the People's Republic of China,State Administration for Market Regulation.National Food Safety Standard For Drinking Natural Mineral Water Inspection Method:GB 8538—2022[S].Beijing:Standards Press of China,2022.
[29] Rybach L.Radioactive heat production in rocks and its relation to other petrophysical parameters[J].Pure and Applied Geophysics,1976,114(2):309-317.
[30] 徐汇,宋华颖,肖本盛,等.浙北花岗岩体放射性地球化学特征与地热关系[C]//浙江省地质学会.资源利用与生态环境——第十六届华东六省一市地学科技论坛论文集.[出版地不详]:浙江国土资源杂志社,2020:227-237.
Xu H,Song H Y,Xiao B S,et al.Radioactive geochemical characteristics of granites from north-Zhejiang and its relationship with geothermal[C]//Zhejiang Geological Society.Resource Utilization and Ecological Environment - Proceedings of the 16th East China Six Provinces One City Geoscience Science and Technology Forum.[s.l.]:Zhejiang Land and Resources Magazine,2020:227-237.
[31] 山东省地质矿产局.山东省区域地质志[M].北京:地质出版社,1991.
Shandong Provincial Bureau of Geology and Mineral Resources.Regional Geological of Shandong Province[M].Beijing:Geological Publishing House,1991. |
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2024, Vol. 11 
