石油勘探与开发 >

2021 , Vol. 48 >Issue 3: 666 - 676

DOI: https://doi.org/10.11698/PED.2021.03.22

新能源新领域

渤海湾盆地北部新近系馆陶组地热田特征及开发实践——以河北省唐山市曹妃甸地热供暖项目为例

  • 董月霞 ,
  • 黄红祥 ,
  • 任路 ,
  • 李洪达 ,
  • 杜志强 ,
  • 鄂俊杰 ,
  • 王琦 ,
  • 张晓明
展开
  • 1.中国石油天然气集团有限公司咨询中心,北京 100724;
    2.中国石油冀东油田公司,河北唐山 063004
董月霞（1968-）,女,安徽亳州人,博士,中国石油天然气集团有限公司咨询中心教授级高级工程师,主要从事油气田勘探地质综合研究与勘探生产实践工作。地址:北京市西城区六铺炕街6号,中国石油天然气集团有限公司咨询中心,邮政编码:100724。E-mail: dongyuexia@petrochina.com.cn

收稿日期: 2020-09-20

  网络出版日期: 2021-05-21

收起

Geology and development of geothermal field in Neogene Guantao Formation in northern Bohai Bay Basin: A case of the Caofeidian geothermal heating project in Tangshan, China

  • DONG Yuexia ,
  • HUANG Hongxiang ,
  • REN Lu ,
  • LI Hongda ,
  • DU Zhiqiang ,
  • E Junjie ,
  • WANG Qi ,
  • ZHANG Xiaoming
Expand
  • 1. CNPC Advisory Center, Beijing 100724, China;
    2. Jidong Oilfield Company of PetroChina, Tangshan 063004, China

Received date: 2020-09-20

  Online published: 2021-05-21

Fold

摘要

选取渤海湾盆地南堡凹陷高尚堡—柳赞地热田为研究对象,系统探讨了研究区馆陶组地热资源地质条件与地热资源潜力,并介绍了曹妃甸地热能供暖的开发实践。研究表明,研究区馆陶组平均埋深1 500~2 500 m,岩性以砂砾岩为主,热储厚度平均为120~300 m,热储平均孔隙度28%~35%,渗透率（600~2 000）×10-3 μm2,热储温度70~110 ℃。地热资源量为13.79×1018 J,折合标准煤4.70×108 t。利用以往油气勘探开发积累的大量地震、钻井资料,开展地热供暖开发目标选区、砂岩热储模拟和同层采灌技术试验,采用分散式采灌布井方式建设曹妃甸新城230×104 m2地热供暖试验项目,自2018年项目完成建设以来平稳运行两个供暖季,年均节约标准煤6.06×104 t,减排二氧化碳15.87×104 t,取得了良好的经济效益和社会效益。曹妃甸地热供暖试验项目证实了东部地区新近系砂岩热储利用同层采灌均衡技术可实现持续规模开发,为中国东部含油气盆地地热资源勘探和开发提供了有效借鉴。图8表4参42

关键词： 地热田; 砂岩热储; 地热供暖; 同层采灌均衡技术; 渤海湾盆地; 地热资源

本文引用格式

董月霞 , 黄红祥 , 任路 , 李洪达 , 杜志强 , 鄂俊杰 , 王琦 , 张晓明 . 渤海湾盆地北部新近系馆陶组地热田特征及开发实践——以河北省唐山市曹妃甸地热供暖项目为例[J]. 石油勘探与开发, 2021 , 48(3) : 666 -676 . DOI: 10.11698/PED.2021.03.22

Abstract

Taking the Gaoshangpu-Liuzan geothermal field in the Nanpu sag of the Bohai Bay Basin as the research object, this paper discusses the geological conditions and potential of the geothermal resources of the Guantao Formation in the study area, and introduces the development practice of geothermal energy heating in Caofeidian. The average buried depth of the Guantao Formation is 1500-2500 m, the lithology is dominated by sandy conglomerate, and the average thickness of thermal reservoir is 120-300 m. The average porosity of thermal reservoir is 28%-35%, the permeability is (600-2000)×10-3 μm2, and the temperature of thermal reservoir is 70-110 ℃. The formation has total geothermal resources of 13.79×1018 J, equivalent to 4.70×108 t of standard coal. Based on a large amount of seismic and drilling data from oil and gas exploration, this study carried out high quality target area selection, simulation of sandstone thermal reservoir, and production and injection in the same layer. The geothermal heating project with distributed production and injection well pattern covering an area of 230×104 m2 was completed in the new district of Caofeidian in 2018. The project has been running steadily for two heating seasons, with an average annual saving of 6.06×104 t of standard coal and a reduction of 15.87×104 t of carbon dioxide, achieving good economic and social benefits. This project has proved that the Neogene sandstone geothermal reservoir in eastern China can achieve sustainable large-scale development by using the technology of "balanced production and injection in the same layer". It provides effective reference for the exploration and development of geothermal resource in oil and gas-bearing basins in eastern China.

Key words： geothermal field; sandstone thermal reservoir; geothermal heating; balanced production and injection in the same layer; Bohai Bay Basin; geothermal resources

参考文献

[1] 郑人瑞, 周平, 唐金荣. 欧洲地热资源开发利用现状及启示[J]. 中国矿业, 2017, 26(5): 13-19.
ZHENG Renrui, ZHOU Ping, TANG Jinrong. Current status and enlightenments of geothermal development in Europe[J]. China Mining Magazine, 2017, 26(5): 13-19.
[2] 国家发展和改革委员会, 国家能源局, 国土资源部. 地热能开发利用“十三五”规划[EB/OL]. (2017-01-23)[2020-07-20]. http://www.nea.gov.cn/2017-02/06/c_136035635.htm.
National Development and Reform Commission, National Energy Administration, Ministry of Land and Resources. The 13th Five-Year Plan for the Development and Utilization of Geothermal Energy[EB/OL]. (2017-01-23)[2020-07-20]. http://www.nea.gov.cn/2017-02/06/c_136035635.htm.
[3] 马峰, 王贵玲, 魏帅超, 等. 2018年地热勘探开发热点回眸[J]. 科技导报, 2019, 37(1): 134-143.
MA Feng, WANG Guiling, WEI Shuaichao, et al. Review of hot spots of geothermal exploration and development in 2018[J]. Science and Technology Review, 2019, 37(1): 134-143.
[4] 王社教, 闫家泓, 李峰, 等. 地热能[M]. 北京: 石油工业出版社, 2017.
WANG Shejiao, YAN Jiahong, LI Feng, et al. Geothermal energy[M]. Beijing: Petroleum Industry Press, 2017.
[5] 董月霞, 周海民, 夏文臣, 等. 南堡凹陷第三系层序地层研究与油气成藏的关系[J]. 石油与天然气地质, 2003, 24(1): 39-49.
DONG Yuexia, ZHOU Haimin, XIA Wenchen, et al. Relationship between Tertiary sequence stratigraphy and oil reservoiring in Nanpu depression[J]. Oil and Gas Geology, 2003, 24(1): 39-49.
[6] 梁宏斌, 钱铮, 辛守良, 等. 冀中坳陷地热资源评价及开发利用[J]. 中国石油勘探, 2010, 15(5): 63-69.
LIANG Hongbin, QIAN Zheng, XIN Shouliang, et al. Assessment and development of geothermal resources in Jizhong Depression[J]. China Petroleum Exploration, 2010, 15(5): 63-69.
[7] 李克文, 王磊, 毛小平, 等. 油田伴生地热资源评价与高效开发[J]. 科技导报, 2012, 30(32): 32-41.
LI Kewen, WANG Lei, MAO Xiaoping, et al. Evaluation and efficient development of geothermal resource associated with oilfield[J]. Science and Technology Review, 2012, 30(32): 32-41.
[8] 汪集暘, 邱楠生, 胡圣标, 等. 中国油田地热研究的进展和发展趋势[J]. 地学前缘, 2017, 24(3): 1-12.
WANG Jiyang, QIU Nansheng, HU Shengbiao, et al. Advancement and developmental trend in the geothermics of oil fields in China[J]. Earth Science Frontiers, 2017, 24(3): 1-12.
[9] 刘金侠, 谷雪曦, 李欣, 等. 我国地热能开发利用现状、问题与展望[J]. 建设科技, 2015(8): 27-30.
LIU Jinxia, GU Xuexi, LI Xin, et al. Current situation, problems and prospects of geothermal energy development and utilization in China[J]. Construction Science and Technology, 2015(8): 27-30.
[10] 汪集旸. 地热学及其应用[M]. 北京: 科学出版社, 2015.
WANG Jiyang. Geothermal science and application[M]. Beijing: Science Press, 2015.
[11] 李郡, 张志刚. 河北省平原区地热资源开发利用现状及问题研究[J]. 环境与发展, 2018, 29(10): 17-18.
LI Jun, ZHANG Zhigang. Status quo and problems of geothermal resource development and utilization in plain area of Hebei province[J]. Environment and Development, 2018, 29(10): 17-18.
[12] 董月霞, 周海民, 夏文臣. 南堡凹陷火山活动与裂陷旋回[J]. 石油与天然气地质, 2000, 21(4): 304-307.
DONG Yuexia, ZHOU Haimin, XIA Wenchen. Volcanic activities and rift-subsidence cycles in Nanpu sag[J]. Oil and Gas geology, 2000, 21(4): 304-307.
[13] 董月霞, 夏文臣, 周海民. 南堡凹陷第三系火山岩演化序列研究[J]. 石油勘探与开发, 2003, 30(2): 24-26.
DONG Yuexia, XIA Wenchen, ZHOU Haimin. Evolvement sequence of Tertiary volcanic rocks in the Nanpu sag, Eastern China[J]. Petroleum Exploration and Development, 2003, 30(2): 24-26.
[14] 董月霞, 汪泽成, 郑红菊, 等. 走滑断层作用对南堡凹陷油气成藏的控制[J]. 石油勘探与开发, 2008, 35(4): 424-430.
DONG Yuexia, WANG Zecheng, ZHENG Hongju, et al. Control of strike-slip faulting on reservoir formation of oil and gas in Nanpu sag[J]. Petroleum Exploration and Development, 2008, 35(4): 424-430.
[15] 汪洋, 邓晋福, 汪集旸, 等. 中国大陆热流分布特征及热-构造分区[J]. 中国科学院研究生院学报, 2001, 18(1): 51-58.
WANG Yang, DENG Jinfu, WANG Jiyang, et al. Terrestrial heat flow pattern and thermo-tectonic domains in the continental area of China[J]. Journal of University of Chinese Academy of Sciences, 2001, 18(1): 51-58.
[16] 龚育龄. 中国东部渤海湾盆地热结构和热演化[D]. 南京: 南京大学, 2003.
GONG Yuling. Geothermal structure and evolution of Bohai Bay Basin in eastern China[D]. Nanjing: Nanjing University, 2003.
[17] 邱楠生. 不同类型沉积盆地热演化成因模式探讨[J]. 石油勘探与开发, 2000, 27(2): 15-17.
QIU Nansheng. Thermal evolution models for different types of basin[J]. Petroleum Exploration and Development, 2000, 27(2): 15-17.
[18] 陈墨香, 汪集旸, 邓孝. 中国地热系统类型图及其简要说明[J]. 地质科学, 1996, 31(2): 114-121.
CHEN Moxiang, WANG Jiyang, DENG Xiao. The map of geothermal system types in China and its brief explanation[J]. Scientia Geologica Sinica, 1996, 31(2): 114-121.
[19] 邱楠生, 苏向光, 李兆影, 等. 郯庐断裂中段两侧坳陷新生代构造-热演化历史研究[J]. 地球物理学报, 2007, 50(5): 1497-1507.
QIU Nansheng, SU Xiangguang, LI Zhaoying, et al. The Cenozoic tectono-thermal evolution of depressions along both sides of mid-segment of Tancheng-Lujiang Fault Zone, East China[J]. Chinese Journal of Geophysics, 2007, 50(5): 1497-1507.
[20] 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. Moderate and low temperature convective geothermal system[M]. Beijing: Science Press, 1993.
[21] 汪集旸, 黄少鹏. 中国大陆地区大地热流数据汇编[J]. 2版. 地震地质, 1990(4): 351-366.
WANG Jiyang, HUANG Shaopeng. Compilation of heat flow data in the continental area of China[J]. 2nd ed. Seismology and Geology, 1990(4): 351-366.
[22] 王钧. 中国地温分布的基本特征[M]. 北京: 地震出版社, 1990.
WANG Jun. Basic characteristics of geothermal distribution in China[M]. Beijing: Seismological Press, 1990.
[23] 张英, 冯建赟, 何治亮, 等. 地热系统类型划分与主控因素分析[J]. 地学前缘, 2017, 24(3): 190-198.
ZHANG Ying, FENG Jianyun, HE Zhiliang, et al. Classification of geothermal systems and their formation key factors[J]. Earth Science Frontier, 2017, 24(3): 190-198.
[24] 陈墨香, 汪集旸, 汪缉安, 等. 华北断陷盆地热场特征及其形成机制[J]. 地质学报, 1990(4): 80-90.
CHEN Moxiang, WANG Jiyang, WANG Ji’an, et al. The characteristics of the geothermal field and its formation mechanism in the north China down-faulted basin[J]. Acta Geologica Sinica, 1990(4): 80-90.
[25] 何治亮, 冯建赟, 张英, 等. 试论中国地热单元分级分类评价体系[J]. 地学前缘, 2017, 24(3): 168-179.
HE Zhiliang, FENG Jianyun, ZHANG Ying, et al. A tentative discussion on an evaluation system of geothermal unit ranking and classification in China[J]. Earth Science Frontiers, 2017, 24(3): 168-179.
[26] 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.
CHEN Moxiang, WANG Jiyang, DENG Xiao. Geothermal resources in China: Formation characteristics and potential assessment[M]. Beijing: Science Press, 1994.
[27] QIU N S, ZUO Y H, CHANG J, et al. Geothermal evidence of Meso-Cenozoic lithosphere thinning in the Jiyang sub-basin, Bohai Bay Basin, eastern North China Craton[J]. Gond-wana Research, 2014, 26: 1079-1092.
[28] 邱楠生. 中国大陆地区沉积盆地热状况剖面[J]. 地球科学进展, 1998, 13(5): 447-451.
QIU Nansheng. Thermal status profile in terrestrial sedimentary basins in China[J]. Advances in Earth Sciences, 1998, 13(5): 447-451.
[29] QIU N S, XU W M, ZUO Y H, et al. Meso-Cenozoic thermal regime in the Bohai Bay Basin, eastern North China Craton[J]. International Geology Review, 2015, 57: 271-289.
[30] QIU N S, ZUO Y H, XU W M. Meso-Cenozoic lithosphere thinning in the eastern North China Craton: Evidence from thermal history of the Bohai Bay Basin, North China[J]. Journal of Geology, 2016, 142: 195-219.
[31] ZUO Y H, QIU N S, ZHANG Y, et al. Thermal regime and hydrocarbon kitchen evolution of the offshore Bohai Bay Basin, North China Craton[J]. AAPG Bulletin, 2011, 69(5): 749-769.
[32] HU S B, HE L J, WANG J Y. Heat flow in the continental area of China: A new data set[J]. Earth and Planetary Science Letters, 2000, 179(2): 407-419.
[33] 邱楠生, 许威, 左银辉, 等. 渤海湾盆地中—新生代岩石圈热结构与热-流变学演化[J]. 地学前缘, 2017, 24(3): 13-26.
QIU Nansheng, XU Wei, ZUO Yinhui, et al. Evolution of Meso-Cenozoic thermal structure and thermal-rheological structure of the lithosphere in the Bohai Bay Basin, eastern North China Craton[J]. Earth Science Frontiers, 2017, 24(3): 13-26.
[34] 臧绍先, 刘永刚, 宁杰远. 华北地区岩石圈热结构的研究[J]. 地球物理学报, 2002, 45(1): 56-66.
ZANG Shaoxian, LIU Yonggang, NING Jieyuan. Thermal structure of the lithosphere in north China[J]. Chinese Journal of Geophysics, 2002, 45(1): 56-66.
[35] 李郡, 张志刚. 冀中台县(河北区域)地热资源特征研究[J]. 河北工业大学学报, 2018, 47(2): 113-120.
LI Jun, ZHANG Zhigang. Characteristics of geothermal resources in Jizhong depression (Hebei region)[J]. Journal of Hebei University of Technology, 2018, 47(2): 113-120.
[36] 邱楠生, 胡圣标, 何丽娟. 沉积盆地热体制研究的理论与应用[M]. 北京: 石油工业出版社, 2004.
QIU Nansheng, HU Shengbiao, HE Lijuan. Theory and application of thermal system research in sedimentary basins[M]. Beijing: Petroleum Industry Press, 2004.
[37] 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(1): 312-321.
LIN Wenjing, LIU Zhiming, WANG Wanli, et al. The assessment of geothermal resources potential of China[J]. Geology in China, 2013, 40(1): 312-321.
[38] 王恩泽, 刘国勇, 庞雄奇, 等. 南堡凹陷中深层碎屑岩储集层成岩演化特征及成因机制[J]. 石油勘探与开发, 2020, 47(2): 321-333.
WANG Enze, LIU Guoyong, PANG Xiongqi, et al. Diagenetic evolution and formation mechanisms of middle to deep clastic reservoirs in the Nanpu sag, Bohai Bay Basin, East China[J]. Petroleum Exploration and Development, 2020, 47(2): 321-333.
[39] WANG Xinwei, MAO Xiang, MAO Xiaoping, et al. Characteristics and classification of the geothermal gradient in the Beijing-Tianjin- Hebei Plain, China[J]. Mathematical Geosciences, 2019, 52: 783-800.
[40] WANG Shejiao, YAN Jiahong, LI Feng, et al. Exploitation and utilization of oilfield geothermal resources in China[J]. Energies, 2016, 9(10): 1-13.
[41] 周念沪. 地热资源开发利用实务全书[M]. 北京: 中国地质科学出版社, 2005.
ZHOU Nianhu. Geothermal resources development and utilization practice book[M]. Beijing: China Geological Sciences Press, 2005.
[42] 章邦桐, 吴俊奇, 凌洪飞, 等. U-Th-K 放射成因热对花岗岩冷却-结晶过程影响的计算及地质意义[J]. 中国科学: 地球科学, 2007, 37(2): 155-159.
ZHANG Bangtong, WU Junqi, LING Hongfei, et al. Estimate of influence of U-Th-K radiogenic heat on cooling process of granitic melt and its geological implications[J]. SCIENCE CHINA Earth Sciences, 2007, 50(5): 672-677.
Options
文章导航

/

〈 〉

版权所有：《石油勘探与开发》编辑部；《石油勘探与开发（英文）》编辑部
地址：北京市海淀区学院路20号，中国石油勘探开发研究院数据中心605室　

京ICP备15044687号    技术支持：北京玛格泰克科技发展有限公司