Influence of CO2-rock interaction and storage of CO2 in reservoirs
(1) Research of influence of permeability by CO2-rock interaction
Tuff matter sandstone was selected in imitation of reservoir
rock, a kind of sandstone, containing the anorthite (CaAl2Si2O8) and high permeability.
CO2 dissolution water (4.7wt%) flowed through the core-rock sample by pressure at 80°C during about 2 month. Permeability was monitored by flow rate, and the alteration of chemical property.
In the result, the permeability decreased one-tenth. This result seemed to require further research and discuss. The ions of K, Na, Ca, Mg and Si were leached from the rock. It was found that leaching of Na, Ca and Mg ions are promoted by CO2 solution. Alterations of mineral component and physical properties (porosity etc.) were not observed.
Also, the dissolution of anorthite was observed at the surface and its dissolution rate was estimated to be less than 7.1E-16 mol/cm2/sec.
(2) Study of assessment techniques of seal performance by seismic tomography.
We developed a CO2-rock experimental system for the investigation of seal performance and influence of CO2-rock interaction. In this system, CO2 behavior in rock sample can be observed by seismic tomography, and threshold pressure can be measured by control of injection and pore-water pressure.
Preliminary test was performed using the calcareous silt rock from Nagaoka test site. The behavior of injected CO2 was monitored by seismic tomography. Also, the threshold pressure was measured.
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