4.6 Article

Macroscale Mechanical and Microscale Structural Changes in Chinese Wufeng Shale With Supercritical Carbon Dioxide Fracturing

期刊

SPE JOURNAL
卷 23, 期 3, 页码 691-703

出版社

SOC PETROLEUM ENG
DOI: 10.2118/181369-PA

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资金

  1. National Key Basic Research Program of China (973 Program) [2014CB239205]
  2. National Natural Science Foundation of China [51604232, 41728004]
  3. Research Project of Key Laboratory of Fluid and Power Machinery at Xihua University

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Waterless fracturing for shale-gas exploitation using supercritical carbon dioxide (scCO(2)) is both effective and environmentally friendly, and has become an extensive research topic. Previous researchers have focused on the chemical and physical properties and microstructure of sandstone, carbonate, and shale caprock, rather than on the properties of shale-gas formations. The macroscale mechanical properties and microscale fracture characteristics of Wufeng Shale exposed to scCO(2)(at greater than 31.8 degrees C and 7.29 MPa) are still not well-understood. To study the macroscale and microscale changes of shale subjected to scCO(2), we obtained Chinese Wufeng Shale crops (Upper Ordovician Formation) from Yibin, Sichuan Basin, China. The shale samples were divided into two groups. The first group was exposed to scCO(2), and the second group was exposed to nitrogen (N-2). Scanning-electron-microscope (SEM) and X-ray-diffraction (XRD) images were taken to study the original microstructure and mineral content of the shale. To study the macroscale mechanical changes of Wufeng Shale immersed in scCO(2) or N-2 for 10 hours, triaxial tests with controlled coring angles were conducted. SEM and XRD images were taken after the triaxial tests. In the SEM images, tight bedding planes and undamaged minerals (with sharp edges and smooth surfaces) were found in N-2 -treated samples both before and after testing, indicating that exposure to N-2 did not affect the microstructures. However, the SEM images for the microstructure scCO(2)-treated samples before and after testing were quite different. The bedding planes were damaged, which left some connected microfractures and corrosion holes, and some mineral types were broken into small particles and left with uneven mineral surfaces. This shows that scCO(2) can change rock microstructures and make some minerals (e.g., calcite) fracture more easily. The complex microscale fractures and the decrease in strength for scCO(2) -treated shale aid the seepage and gathering of gas, enhancing shale-gas recovery. Knowledge of the multiscale physical and chemical changes of shale exposed to scCO(2) is not only essential for scCO(2) fracturing, but it is also important for scCO(2), jets used to break rock and for the geological storage of CO2.

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