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雄安新区高阳地热田热储高于庄组碳酸盐岩不同围压下破碎规律研究

李燕燕, 张保建, 邢一飞, 王贵玲. 2023. 雄安新区高阳地热田热储高于庄组碳酸盐岩不同围压下破碎规律研究[J]. 中国地质, 50(4): 1138-1148. doi: 10.12029/gc20210220002
引用本文: 李燕燕, 张保建, 邢一飞, 王贵玲. 2023. 雄安新区高阳地热田热储高于庄组碳酸盐岩不同围压下破碎规律研究[J]. 中国地质, 50(4): 1138-1148. doi: 10.12029/gc20210220002
LI Yanyan, ZHANG Baojian, XING Yifei, WANG Guiling. 2023. Fragmentation law of carbonate rocks under different confining pressure in Gaoyuzhuang Formation, Gaoyang geothermal field, Xiong'an New Area[J]. Geology in China, 50(4): 1138-1148. doi: 10.12029/gc20210220002
Citation: LI Yanyan, ZHANG Baojian, XING Yifei, WANG Guiling. 2023. Fragmentation law of carbonate rocks under different confining pressure in Gaoyuzhuang Formation, Gaoyang geothermal field, Xiong'an New Area[J]. Geology in China, 50(4): 1138-1148. doi: 10.12029/gc20210220002

雄安新区高阳地热田热储高于庄组碳酸盐岩不同围压下破碎规律研究

  • 基金项目:
    国家重点研发项目(2019YFB1504102)、中国地质科学院基本科研业务项目(JKY202018,YWF201903-01)及中国地质调查局项目(DD20189114)联合资助
详细信息
    作者简介: 李燕燕, 女, 1988年生, 博士, 副研究员, 主要从事地热地质学等研究工作; E-mail: liyanyan@cags.ac.cn
  • 中图分类号: P314

Fragmentation law of carbonate rocks under different confining pressure in Gaoyuzhuang Formation, Gaoyang geothermal field, Xiong'an New Area

  • Fund Project: Supported by National Key Research and Development Projects (No.2019YFB1504102), Chinese Academic Geological Sciences Project (No.JKY202018, YWF201903-01) and the project of China Geological Survey (No.DD20189114)
More Information
    Author Bio: LI Yanyan, female, born in 1988, Ph.D, assistant researcher, mainly engaged in geothermal geology; E-mail: liyanyan@cags.ac.cn .
  • 研究目的

    雄安新区高阳地热田D34钻孔为中国地质调查局中国地质科学院于2020年钻获的华北盆地最高温地热井,井口温度达123.4℃,出水量为94.5 m3/h,为使温度如此高的地热井的地热开发利用程度最大化,开展压裂增产是其重要举措。因此,为获取相关参数,以制定最优的压裂增产方案,本次研究拟厘清储层岩石在不同围压下的破碎规律。

    研究方法

    本文在前人研究的基础上,以D34井钻获的深部高于庄组热储碳酸盐岩为研究对象,开展了常规三轴抗压及抗拉实验。

    研究结果

    实验结果表明:(1)高于庄组碳酸盐岩拉伸强度特征与压缩强度特征相近,且表现出明显的压缩破坏特征。随着围岩压力的增加,抗压强度具有典型的二次增高特征。(2)抗压强度及裂隙展布形态随深度变化呈现出差异性,其中均匀发育的多裂缝和单一主缝为主要形式扩展。在20 MPa、40 MPa围压下,屈服强度分别与弹性模量、泊松比协同变化。(3)储层不同深度拉伸裂隙的扩展方式有所差异,较浅部拉伸裂隙主要以小幅度多级扩展为主,而较深部岩石则表现出均匀扩展态势。

    结论

    结合抗压和抗拉实验结果,认为热储高于庄组压裂增产效果较好,且储层浅部形成复杂压裂网络的可能性高于深部储层,但总体脆性指数分布差异较小,故认为无需对储层不同深度采取不同的压裂施工方案。

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  • 图 1  岩石试样照片

    Figure 1. 

    图 2  常规三轴实验装置图

    Figure 2. 

    图 3  实验破坏前照片

    Figure 3. 

    图 4  拉伸实验装置及实验前后样品照片

    Figure 4. 

    图 5  D34井高于庄组热储碳酸盐岩三轴抗压缩试验结果

    Figure 5. 

    图 6  D34井高于庄组热储碳酸盐岩微观尺度天然裂缝发育情况

    Figure 6. 

    图 7  D34井高于庄组热储碳酸盐岩不同围压下的屈服强度

    Figure 7. 

    图 8  D34井高于庄组热储碳酸盐岩不同围压下弹性模量和泊松比变化趋势

    Figure 8. 

    图 9  D34井高于庄组热储碳酸盐岩抗拉特征

    Figure 9. 

    表 1  D34井高于庄组热储碳酸盐岩全岩及黏土矿物X-射线衍射定量分析结果

    Table 1.  Quantitative X-ray diffraction analysis results of whole rock and clay minerals of reservoir carbonate rock in D34 well, Gaoyuzhuang Formation

    下载: 导出CSV

    表 2  D34井高于庄组热储碳酸盐岩单、三轴抗压强度实验结果及相关计算参数

    Table 2.  Experimental results and calculated parameter of uniaxial and triaxial compressive strength of reservoir carbonate rock in D34 well, Gaoyuzhuang Formation

    下载: 导出CSV

    表 3  D34井高于庄组热储碳酸盐岩抗拉实验结果

    Table 3.  Tensile test results of the reservoir carbonate rock in the Gaoyuzhuang Formation of D34 well

    下载: 导出CSV
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出版历程
收稿日期:  2021-02-20
修回日期:  2021-04-18
刊出日期:  2023-08-25

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