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波尔兹曼数字岩芯致密砂岩渗透率研究

朱伯靖 石耀霖

朱伯靖, 石耀霖. 波尔兹曼数字岩芯致密砂岩渗透率研究[J]. 力学学报, 2013, 45(3): 384-394. doi: 10.6052/0459-1879-12-273
引用本文: 朱伯靖, 石耀霖. 波尔兹曼数字岩芯致密砂岩渗透率研究[J]. 力学学报, 2013, 45(3): 384-394. doi: 10.6052/0459-1879-12-273
Zhu Bojing, Shi Yaolin. STUDY OF TIGHT SANDSTONE PERMEABILITY FROM LATTICE BOLTZMANN & DIGITAL ROCK MODEL[J]. Chinese Journal of Theoretical and Applied Mechanics, 2013, 45(3): 384-394. doi: 10.6052/0459-1879-12-273
Citation: Zhu Bojing, Shi Yaolin. STUDY OF TIGHT SANDSTONE PERMEABILITY FROM LATTICE BOLTZMANN & DIGITAL ROCK MODEL[J]. Chinese Journal of Theoretical and Applied Mechanics, 2013, 45(3): 384-394. doi: 10.6052/0459-1879-12-273

波尔兹曼数字岩芯致密砂岩渗透率研究

doi: 10.6052/0459-1879-12-273
基金项目: 国土资源部深部探测Sinoporbe-07基金(0819011A90)和国家自然科学面上基金(D0408/4097409)资助项目
详细信息
    通讯作者:

    朱伯靖,副教授,主要研究方向:断裂力学、地球物理学.E-mail:cynosureorion@ucas.ac.cn

    石耀霖,中国科学院院士,第三世界科学院院士,主要研究方向:地球物理学.E-mail:shiyl@ucas.ac.cn

  • 中图分类号: O0357.2; O0373; P313.1

STUDY OF TIGHT SANDSTONE PERMEABILITY FROM LATTICE BOLTZMANN & DIGITAL ROCK MODEL

Funds: The project was supported by the project was supported by the SINOPROBE-07 (0819011A90) and the National Natural Science Foundation of China (D0408/4097409).
  • 摘要: 致密砂岩渗透率在油气勘探开发、地应力测量及水库地质灾害等领域具有重要意义,但鉴于目前实验技术局限性,温压耦合渗透率测量尚无法通过实验手段实现. 在已有研究工作基础上,首次建立了基于D3Q27数字岩芯模型,并计算了高温压耦合低渗砂岩渗透率问题. 首先,以鄂尔多斯盆地某油田延长组致密砂岩为例,利用X射线CT断层成像技术岩芯获取10μm, 5μm, 2μm分辨率致密砂岩内部结构数据,应用基于量子力学第一性原理的D3Q27格子波尔兹曼数字岩芯模型建立数值模型. 进而,利用自编3DLBM程序分别计算了不同分辨率渗透率随围压(0~200MPa)、孔隙压(0~65MPa)和温度(25℃~180℃)变化规律,通过与Inc AUTOLAB2 000C岩石测试分析系统实验结果对比,验证了程序的可靠性,得到低渗砂岩断层最佳分辨率;最后,在并行CPU-GPU平台上计算了高温高压耦合(0℃~400℃, 0~1.4 GPa)下致密砂岩渗透率值及其各向异性随温压变化规律,并讨论了致密砂岩中水在达到超临界状态后对致密岩石内部结构的影响.

     

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出版历程
  • 收稿日期:  2012-10-11
  • 修回日期:  2012-11-22
  • 刊出日期:  2013-05-18

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