4.7 Article

Evolution of permeability and microscopic pore structure of sandstone and its weakening mechanism under coupled thermo-hydro-mechanical environment subjected to real-time high temperature

期刊

ENGINEERING GEOLOGY
卷 280, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.enggeo.2020.105955

关键词

Coupled thermal-hydrological-mechanical processes; Micro-pore structures; High temperature; In-situ coal gasification

资金

  1. Natural Science Funds for Young Scholars [51904195]
  2. Scientific and Technological Innovation Programs of Higher Education Institutions in Shanxi [2019L0640]
  3. Key Research and Development Project of Shanxi Province [201903D121025, 20191102004]
  4. Shanxi Province Science Foundation for Youths [201901D211300, 20191142]
  5. Outstanding Doctoral Award Fund in Shanxi Province [20192032]
  6. TYUST-SRIF [20172018]

向作者/读者索取更多资源

This study observed the permeability evolution in sandstone under real-time high temperature and triaxial stress using a self-developed universal tester with high temperature and high pressure capabilities. The results show that the microscopic structures within the sandstone under the coupled thermo-hydro-mechanical condition are vastly different from those subjected to heat treatment only.
Thermal damage mechanisms and the characteristics of performance deterioration of a repository host rock is critical for evaluating the potential of an underground coal gasification project. Previously, many studies have primarily focused on the microstructural evolution of various rock types after high-temperature treatment only. However, relatively little is known regarding the coupled thermo-hydro-mechanical (THM) behavior of rock, which is frequently encountered in geo-engineering underground regions with high-temperatures. In this study, using a self-developed universal tester with the ability of THM coupling of high temperature and high pressure, permeability evolution in sandstone under real-time high temperature (20-700 degrees C) and triaxial stress (hydrostatic pressure = 25 MPa) were observed. The microphysical parameters of these specimens subjected to the THM environment were then measured, and the corresponding morphological evolution processes were also assessed using micro-computed tomography (MCT). Further, for the purpose of contrast, we have also determined the microphysical parameters for the sandstone after heat treatment only. The results show that the evolution of the microscopic structures within the sandstone under the coupled THM condition is vastly different from those subjected to heat treatment only. The experimental results in this study can provide theoretical guidance for the stability of surrounding rock of a combustion cavity during in-situ coal gasification.

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