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CO2基增强型地热系统中流体-花岗岩相互作用研究进展及展望

薛卉,  舒彪,  陈科平,  路伟,  张森,  胡永鹏

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文章导航 > 地质科技通报  > 2021 >  40(3): 45-53
薛卉, 舒彪, 陈科平, 路伟, 张森, 胡永鹏. CO2基增强型地热系统中流体-花岗岩相互作用研究进展及展望[J]. 地质科技通报, 2021, 40(3): 45-53. doi: 10.19509/j.cnki.dzkq.2021.0021
引用本文: 薛卉, 舒彪, 陈科平, 路伟, 张森, 胡永鹏. CO2基增强型地热系统中流体-花岗岩相互作用研究进展及展望[J]. 地质科技通报, 2021, 40(3): 45-53. doi: 10.19509/j.cnki.dzkq.2021.0021
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Xue Hui, Shu Biao, Chen Keping, Lu Wei, Zhang Sen, Hu Yongpeng. Research progress of fluid-granite interaction in CO2 based enhanced geothermal system[J]. Bulletin of Geological Science and Technology, 2021, 40(3): 45-53. doi: 10.19509/j.cnki.dzkq.2021.0021
Citation: Xue Hui, Shu Biao, Chen Keping, Lu Wei, Zhang Sen, Hu Yongpeng. Research progress of fluid-granite interaction in CO2 based enhanced geothermal system[J]. Bulletin of Geological Science and Technology, 2021, 40(3): 45-53. doi: 10.19509/j.cnki.dzkq.2021.0021
shu

CO2基增强型地热系统中流体-花岗岩相互作用研究进展及展望

doi: 10.19509/j.cnki.dzkq.2021.0021
基金项目: 

国家自然科学基金面上项目 42072304

国家自然科学基金青年基金项目 41702387

详细信息
    作者简介:

    薛卉(1990-), 女, 现正攻读地质工程专业硕士学位, 主要从事水文地质与工程地质及非常规能源开采等方面的研究工作。E-mail: 422766340@qq.com

    通讯作者:

    舒彪(1986-), 男, 副教授, 硕士生导师, 主要从事岩石力学及非常规能源开采等方面的研究工作。E-mail: biaoshu@csu.edu.cn

  • 中图分类号: P588.12+1;P641.3

Research progress of fluid-granite interaction in CO2 based enhanced geothermal system

    摘要
  • 摘要: CO2与水相比，膨胀性大、黏度低、与岩石反应程度低，并且在作为增强型地热系统（EGS）渗流传热流体时，比水具有更高的换热效率。对CO2-EGS生产过程中储层岩石物性变化的研究具有重要意义，从理论研究、实验研究、数值模拟3个方面，对CO2基增强型地热系统CO2-EGS中流体-岩石相互作用的研究现状进行了总结，并且从矿物成分、微观孔结构和力学性质3个方面对储层岩石性质的变化进行了评价。结果表明，CO2-水-岩石相互作用参与反应的矿物主要为石英、长石类；而沉淀的矿物为蒙脱石、伊利石及方解石等。CO2-水-岩石相互作用会导致储层岩石的力学性质下降，孔隙结构特征改变。最后，讨论了CO2作为EGS渗流传热流体仍需攻克的难点问题，包括：CO2的热动力学特征、换热效率，CO2-水-岩石的相互作用及其对储层性质的改变，影响CO2-EGS经济性的因素，以及CO2-EGS数值模型的研究等。针对这些方面的研究可为今后CO2-EGS的开发奠定基础。

     

    Abstract: Compared with water, CO2 has larger expansibility, lower viscosity and lower reaction degree with rock.As an enhanced geothermal system (EGS) seepage heat transfer fluid, CO2 has higher heat transfer efficiency than water.This paper summarizes the research status of fluid/rock interaction in CO2-EGS from three aspects: theoretical research, experimental research and numerical simulation.The changes of reservoir rock properties are evaluated from mineral composition, micro pore structure and mechanical properties.The results show that the main reaction minerals of CO2-water-rock interaction are quartz and feldspar, and the precipitation minerals are montmorillonite, illite and calcite.The interaction of CO2-water-rock will lead to the decline of mechanical properties of reservoir rocks and the change of pore structure characteristics.Finally, the existing problems and development trend of CO2-water-rock interaction in CO2-EGS are discussed, which provides a reference for the development and research of CO2-EGS in the future.

     

    • HTML全文

  • 图 1  CO2-EGS储层区域划分示意图(据文献[24])

    Figure 1.  Schematic diagram of regional division of CO2-EGS reservoir

    下载: 全尺寸图片 幻灯片

    图 2  国内外期刊在EGS、CO2-EGS领域的研究成果

    Figure 2.  Annual publication volume of domestic and foreign journals in the fields of EGS and CO2-EGS

    下载: 全尺寸图片 幻灯片

    图 3  CO2-EGS不同研究方向的研究成果

    Figure 3.  Publications of different research directions of CO2-EGS

    下载: 全尺寸图片 幻灯片
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