Experimental Study of CO2 Residual Gas Sequestration Applied to Ordovician Reef Limestone of Tarim Basin
详细信息   
摘要

 The geological storage of CO2 is widely accepted as an effective method to reduce the release of greenhouse gases to the atmosphere. In this study, an experimental method applied to a rock sample taken from Ordovician reef limestone of Tarim Basin was used to measure the residual gas saturation. Through simulating water flooding supercritical CO2 saturated core under 40 strata temperature, 8 MPa strata pressure, the pressure and flux change with time were observed during the course, and residual gas saturation was measured as 0.368.

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