青海省贵德扎仓寺地热成因机理及开发利用建议

doi:10.13278/j.cnki.jjuese.201601206

吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (1): 220-229.doi: 10.13278/j.cnki.jjuese.201601206

青海省贵德扎仓寺地热成因机理及开发利用建议

李小林¹, 吴国禄¹, 雷玉德¹, 李重阳², 赵继昌³, 白银国¹, 曾昭发⁴, 赵振¹, 张珊珊⁵, 赵爱军¹

1. 青海省环境地质重点实验室/青海省环境地质勘查局, 西宁 810007;
2. 四川省地质矿产勘查开发局九一五水文地质工程地质队, 四川眉山 620000;
3. 中国地质环境监测院, 北京 100003;
4. 吉林大学地球探测科学与技术学院, 长春 130026;
5. 青海省地质调查局, 西宁 810001

收稿日期:2015-04-08 出版日期:2016-01-26 发布日期:2016-01-26
作者简介:李小林(1958),男,教授级高级工程师,主要从事水文地质、工程地质、灾害地质方面的研究,E-mail:lxl906@163.com
基金资助:
青海省科技支撑计划项目 (2014-GX-207);国家高技术研究发展计划("863"计划)项目(2012AA052803);中国地质调查局地质大调查项目 (水环[2013]第23号)

Suggestions for Geothermal Genetic Mechanism and Exploitation of Zhacang Temple Geothermal Energy in Guide County, Qinghai Province

Li Xiaolin¹, Wu Guolu¹, Lei Yude¹, Li Chongyang², Zhao Jichang³, Bai Yinguo¹, Zeng Zhaofa⁴, Zhao Zhen¹, Zhang Shanshan⁵, Zhao Aijun¹

1. Key Lab of Geo-Environment, Qinghai Province/Environmental Geological Prospecting Bureau of Qinghai Province, Xi'ning 810007, China;
2. Bureau of Geology and Mineral Exploration and Development 915 Hydrogeology and Engineering Geology Team, Meishan 620000, Sichuan, China;
3. China Institute of Geo-Environment Monitoring, Beijing 100003, China;
4. College of GeoExploration Science and Technology, Jilin University, Changchun 130026, China;
5. Qinghai Province Geological Bureau, Xi'ning 810001, China

Received:2015-04-08 Online:2016-01-26 Published:2016-01-26
Supported by:
Supported by Science and Technology Support Program of Qinghai Province (2014-GX-207),National High-Tech R&D Program of China ("863" Program) (2012AA052803) and Geological Survey Projects of China Geological Survey(WH[2013] No.23)

摘要/Abstract

摘要：

本文通过卫星热遥感影像及航磁、重力异常的宏观性解译热异常空间分布特征,野外实地调查温泉的出露条件和水化学特征,分析研究青海省贵德扎仓寺温泉的热源通道、入渗通道,从而讨论其成因机理和开发利用前景。研究结果表明:扎仓寺温泉泉口温度为93.5℃,与当地气压有关;大气降水和热水沟上游沟谷水为补给源,近东西向张裂为入渗通道,中三叠统砂板岩与印支期花岗闪长岩(γδ₅²)接触变质带为径流通道(热储层),中三叠统砂板岩为盖层,北北西向热光断裂(F₁)为热源通道,属断裂-深循环地热类系统类型;径流通道(热储层)温度可达136.0℃,具备蒸汽发电示范背景条件,而F₁断裂带附近2000 m深度温度可达195.0℃,具备干热岩开发利用前景。

关键词: 扎仓寺温泉, 地热成因机理, 开发利用, 干热岩

Abstract:

The regional distribution of the thermal anomaly is studied by the macroscopic interpretation of satellite remote sensing, aeromagnetic heat, and gravity anomalies. At the same time, the exposed conditions and hydrochemical characteristics of hot springs are discussed through field investigation and test. On this basis, the heat channel and infiltration channel of the hot spring are analyzed, as well as the geothermal genetic mechanism and exploitation. The temperature of Zhacang hot spring is 93.5℃, which is related to the local pressure. The precipitation, hot ditch water, and upper gully water are the recharge source of the hot springs;the east-west tension cracks are the filtration channels;the metamorphic belt between the middle Triassic sandy slates and granodiorite is the runoff channel of the hot reservoir;covering by the sandy slate, Reguang fault of NNW(F₁) is the heat source channel. It belongs to a fracture-deep cycle geothermal system. The temperature of hot reservoir could be up to 136.0℃,and could be used for generating electricity. The temperature at the depth of 2000 meters near the F₁ fault could reach 195.0℃, and the hot dry rocks are valuable for future development and utilization.

Key words: hot spring of Zhacang Temple, genetic mechanism of geothermal, exploitation, hot dry rock

中图分类号:

P314

李小林, 吴国禄, 雷玉德, 李重阳, 赵继昌, 白银国, 曾昭发, 赵振, 张珊珊, 赵爱军. 青海省贵德扎仓寺地热成因机理及开发利用建议[J]. 吉林大学学报(地球科学版), 2016, 46(1): 220-229.

Li Xiaolin, Wu Guolu, Lei Yude, Li Chongyang, Zhao Jichang, Bai Yinguo, Zeng Zhaofa, Zhao Zhen, Zhang Shanshan, Zhao Aijun. Suggestions for Geothermal Genetic Mechanism and Exploitation of Zhacang Temple Geothermal Energy in Guide County, Qinghai Province[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1): 220-229.

参考文献

[1] 吴国禄,李小林.青海省干热岩显示及其勘查工作部署[J].青海国土经略,2014(1):52-54. Wu Guolu,Li Xiaolin.The Study of Hot Dry Rock Manifestations and Deployment of Qinghai[J]. Management and Strategy of Qinghai Land and Resources,2014(1):52-54.

[2] 王鸿杰.青海省贵德盆地地下热水初步勘察报告[R].西宁:青海省第二水文地质大队,1977-1979. Wang Hongjie.Underground Hot Water Preliminary Investigation Report in Guide Basin, Qinghai Province[R]. Xining:Qinghai Second Hydrogeological Brigade,1977-1979.

[3] 洪文元,王华书.新街幅1:20万水文地质普查报告[R].西宁:中国人民解放军00929部队,1983. Hong Wenyuan,Wang Huashu.Hydrogeological Survey Report with a Scale of 1:200000 in New Street[R]. Xining:PLA 00929 Troops,1983.

[4] 郭万成,时兴梅.青海省(贵德县)盆地地热资源开发利用[J].水文地质工程地质,2008(3):79-92. Guo Wancheng,Shi Xingmei. The Development and Utilization of Guide Basin's Geothermal Resources of Qinghai Province[J].Hydrogeology and Engineering Geology, 2008(3):79-92.

[5] 姜春发,王宗起,李锦轶,等.中央造山带开合构造[M].北京:地质出版社,2000:107-110. Jiang Chunfa,Wang Zongqi,Li Jinyi,et al.Opening-Closing Tectonics in the Central Orogenic Belt[M].Beijing:Geological Publishing House,2000:107-110.

[6] 方斌,周训,梁四海,等.青海省贵德县扎仓寺温泉特征及其开发利用[J].现代地质,2009,23(1):57-63. Fang Bin,Zhou Xun,Liang Sihai,et al. Characteristics and Utilization of the Zhacang Hot Springs in Guide County, Qinghai[J].Modern Geology,2009, 23(1):57-63.

[7] 陈惠娟,赵振,罗银飞,等.青海省贵德盆地地热资源评价与开发利用[J].青海环境,2010,20(4):196-199. Chen Huijuan, Zhao Zhen,Luo Yinfei,et al. The Assessment and Development Utilization of Guide Basin's Geothermal Resources of Qinghai Province[J].Journal of Qinghai Environment, 2010,20(4):196-199.

[8] 刘时彬.地热资源及其开发利用和保护[M].北京:化学工业出版社,2005:171-195. Liu Shibin.Exploitation and Protection of Geothermal Resources[M]. Beijing:Chemical Industry Press, 2005:171-195.

[9] GB 8537-2008饮用天然矿泉水[S].北京:中国标准出版社,2009. GB 8537-2008 Drinking Natural Mineral Water[S].Beijing:China Standard Press,2009.

[10] 李小林,龙作元,高忠咏,等.青海地质环境[M]. 北京:地质出版社,2010:47-56. Li Xiaolin,Long Zuoyuan,Gao Zhongyong,et al. Geological Environment in Qinghai[M]. Beijing:Geological Publishing House, 2010:47-56.

[11] 薛建球,甘斌,李百祥,等.青海共和-贵德盆地增强型地热系统(干热岩)地质-地球物理特征[J].物探与化探,2013,37(1):35-41. Xue Jianqiu,Gan Bin,Li Baixiang,et al.The Geophysical Characteristics of Enhanced Geothermal Systems(Hot Dry Rock) in Gonghe-Guide Basin of Qinghai Province[J].Geophysical and Geochemical Exploration,2013,37(1):35-41.

[12] 周训,金晓媚,梁四海,等.地下水科学专论[M].北京:地质出版社,2010:57-60. Zhou Xun,Jin Xiaomei,Liang Sihai,et al. Groundwater Science Monographs[M].Beijing:Geological Publishing House, 2010:57-60.

[13] 陈墨香,汪集旸,邓孝.中国地热资源:形成特点和潜力评估[M].北京:科学出版社,1994:1-39. Chen Moxiang,Wang Jiyang,Deng Xiao. Chinese Geothermal Resources, Formation Characteristics and Potential Assessment[M]. Beijing:Science Press, 1994:1-39.

[14] GB/T 11615-2010地热资源地质勘查规范[S].北京:中国标准出版社,2011. GB/T 11615-2010 Geologic Exploration Standard of Geothermal Resources[S].Beijing:China Standard Press,2011.

[15] 李娟,周训,方斌,等.河北秦皇岛市温泉堡温泉的形成与开发利用建议[J].地质通报,2007,26(3):344-349. Li Juan,Zhou Xun,Fang Bin,et al.Formation of Hot Springs at Wenquanpu,Qinhuangdao City,Hebei,China,and Suggestions of Their Exploitation and Utilization[J].Geological Bulletin of China,2007,26(3):344-349.

[16] 康玲,王时龙,李川.增强地热系统EGS的人工热储技术[J].机械设计与制造,2008(9):141-143. Kang Ling, Wang Shilong,Li Chuan.The Artificial Geothermal Reservoir Technology of Enhanced Geothermal Systems EGS[J].Machinery Design & Manufacture,2008(9):141-143.

[17] 刘永涛.云南省龙陵县邦腊掌温泉水文地球化学与间歇喷泉研究[D].北京:中国地质大学,2009. Liu Yongtao. A Study of Hydrochemistry and Geyser of Thermal Groundwater in the Banglazhang Geothermal Field in Longling, Yunnan[D].Beijing:China University of Geosciences,2009.

[18] 王通国,冯在敏,常允新,等.汤头温泉开发引起的环境地质问题及防治对策[J].中国地质灾害与防治学报,2002,13(1):83-88. Wang Tongguo,Feng Zaimin,Chang Yunxin,et al.Environmental Geological Problems Caused by Hot Spring Development in Tangtou and the Prevention Countermeasure[J]. The Chinese Journal of Geological Hazard and Control,2002,13(1):83-88.

[19] 方斌,杨运军,王根厚,等.藏北羌塘中部吉瓦地热田的特征及其资源评价[J].地质通报,2009,28(9):1335-1341. Fang Bin,Yang Yunjun,Wang Genhou,et al.Characteristics and Resource Evaluation of the Jiwa Geothemal Field in Central Qiangtang,Northern Tibet,China[J]. Geological Bulletin of China,2009,28(9):1335-1341.

[20] 刘春雷,王贵玲,王婉丽,等.基于现场热响应测试方法的地下岩土热物性分析[J].吉林大学学报(地球科学版),2014,44(5):1602-1608. Liu Chunlei,Wang Guiling,Wang Wanli,et al.Analysis of Soil Thermal Properties with In-Situ Thermal Response Test Method[J]. Journal of Jilin University(Earth Science Edition), 2014,44(5):1602-1608.

[21] 汪集旸,熊亮萍,庞忠和.中低温对流型地热系统[M].北京:科学出版社,1993. Wang Jiyang,Xiong Liangping,Pang Zhonghe.Low-Medium Temperature Geothermal System of Convective Type[M].Beijing:Science Press, 1993.

[22] 许天福,张延军,曾昭发,等.增强型地热系统(干热岩)开发技术进展[J].科技导报,2012,30(32):42-45. Xu Tianfu,Zhang Yanjun,Zeng Zhaofa,et al.Technology Progress in an Enhanced Geothermal System(Hot Dry Rock)[J].Science & Technology Review,2012,30(32):42-45.

[23] Grant M A, Bixley P F.Geothermal Reservoir Engineering[M].New York:Academic Press Inc,2011.

[24] 雷宏武,金光荣,李佳琦,等.松辽盆地增强型地热系统(EGS)地热能开发热-水动力耦合过程[J].吉林大学学报(地球科学版),2014,44(5):1633-1646. Lei Hongwu,Jin Guangrong,Li Jiaqi,et al.Coupled Thermal-Hydrodynamic Processes for Geothermal Energy Exloitation in Enhanced Geothermal System at Songliao Basin,China[J]. Journal of Jilin University(Earth Science Edition),2014,44(5):1633-1646.

[25] Brown D.The US Hot Dry Rock Program-20 Years of Experience in Reservoir Testing[C]//Proceeding of World Geothermal Congress,1995:2607-2611.

[26] 李怡,张启.热干岩发电系统[J].国外科技动态,1995(5):56-56. Li Yi,Zhang Qi. Hot Dry Rock Power Generation System[J].Recent Developments in Science & Technology Abroad,1995(5):56-56.

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青海省贵德扎仓寺地热成因机理及开发利用建议

Suggestions for Geothermal Genetic Mechanism and Exploitation of Zhacang Temple Geothermal Energy in Guide County, Qinghai Province

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