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| Study on evolution of permeability characteristics of oil shale under in-situ exploitation |
| ZHAO Jing1,2,LIU Zengqi1,KANG Zhiqin2,3,YANG Dong2,3 |
| (1. College of Mining Engineering,Taiyuan University of Technology,Taiyuan,Shanxi 030024,China;2. State Center for Research and Development of Oil Shale Exploitation,Beijing 100083,China;3. Key Laboratory of In-situ Property-improving Mining of Ministry of Education,Taiyuan University of Technology,Taiyuan,Shanxi 030024,China) |
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Abstract In order to study the evolution of the permeability characteristics of oil shale under in-situ exploitation,permeability tests on the oil shale from Fushun west open pit mine were performed by high temperature triaxial permeability testing machine,and the pore microstructure of the oil shale was characterized by the mercury injection apparatus. The evolution mechanism of the permeability was discussed. The results show that the porosity and the permeability of the oil shale have a good correlation with each other. With increasing the temperature,the oil shale specimens evolve from the dense state to the porous medium,and both the porosity and the permeability increase. The pore pressure fluid has multiple physical effects on the variation of the pore structure,especially at the stage of oil and gas production due to pyrolysis of the organic matter. The pore characteristic parameters of the oil shale after high temperature permeability tests are significantly improved compared with those heated in muffle furnace. The porosities of the oil shale samples at the temperature of 300 ℃,400 ℃,500 ℃ and 600 ℃ increase by 0.6%,8.62%,1.82% and 7.83%,respectively. At 600 ℃,the macropore and mesopore volumes increase by about 1.3 and 2.4 times,respectively. Before 300 ℃,the permeability of the oil shale samples is mainly affected by the thermal stress caused by uneven thermal expansion of mineral particles and water precipitation. At 300 ℃﹣400 ℃,the complex reaction inside the oil shale occurs and many impermeable pores form,resulting in an uncoordinated change between the porosity and the permeability. 400 ℃﹣600 ℃ is the main pyrolysis stage of the oil shale. In this stage,the pyrolysis pores in the oil shale are continuously generated and connected,forming the flow channel of oil and gas products and increasing the porosity by 25.77%,and the permeability increases by about 9.06 times when the pore pressure is 1.0 MPa.
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