To better understand trapping mechanisms of CO
2 in reservoir, we try to elucidate the effect of thin and low-porosity lamina in porous Tako sandstone on CO
2 flow by experiments and numerical simulations. Tako sandstone is characterized by the well-developed and low porosity lamina, where the intergranular space is filled with precipitated iron-rich minerals. We measure P-wave velocities (
Vp) in three channels which are crossing through high porosity zone (Ch.A), on a lamina (Ch.B), and beneath the lamina (Ch.C) during CO
2 injection stage (drainage) and water re-injection stage (imbibition). In drainage, all channels show large
Vp-reduction over 10 %. In imbibition, they indicate
Vp-increases but different recovery patterns with injecting CO
2-saturated water. After 250 ml water injection,
Vp of Ch.A and Ch.B almost recover from
Vp-reduction in drainage. On the other hand,
Vp of Ch.C still has a reduction about 4%. We then try 2D core-scale flow-simulations by using TOUGH-2 to confirm the effect of lamina on fluid flow and pattern of CO
2 distribution. In drainage, CO
2 has large mobility and moves upward vigorously to the top-end of core at 20ml CO
2-injection. After reaching the top-end, CO
2 invades lamina zone and raises CO
2-saturation during drainage. In enhanced case of difference between porosity-permeability relation, the result of simulation indicates the strong heterogeneity of CO
2-distribution pattern, which shows clear low-CO
2 saturation of the lamina zone and obvious high-CO
2 saturation of the zone of direct beneath of lamina. In imbibition, CO
2 saturation decreases rapidly after 40ml water injection. However, the zone of beneath the lamina keeps high CO
2 saturation after 100ml water injection. These results suggest that the lamina in Tako sandstone behave as barriers of CO
2 flow. This assumption is supported by results of
Vp-measurement, because the channel of beneath a lamina still shows a
Vp-reduction about 4% after 250 ml water injection.
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