2:30 PM - 2:45 PM
[HSC06-16] Relationship between CO2 storage and hydrate sealing layer in hydrate CCS

Keywords:Permeability, CCS, Core flooding test, Subsea sediment, Global warming
Three types of cores were prepared using two simulated sediments, Toyoura standard sand and Tohoku silica sand No. 8. One contained only Toyoura standard sand, another contained only Tohoku silica sand No. 8, and the last one was filled with Toyoura standard sand and Tohoku silica sand No. 8 in sequence from the bottom end of the core. The inside of the cores were maintained at 7.5 MPa and 8.5 ℃, and the same amount of liquid CO2 was injected at a constant flow rate from the bottom end of the cores. The pressure and temperature in the cores were measured and the formation behavior of CO2 hydrate was analyzed. The results of the experiments showed that hydrate formation in the core was confirmed in each experiment, but the demonstration of sealing varied from experiment to experiment. In some experiments, the formation of a hydrate sealing layer that could withstand maximum pressure difference of about 5.5 MPa was confirmed, while in other experiments only partial blockage was observed. The difference in this phenomenon can be attributed to the uneven formation of CO2 hydrate in the horizontal plane and the heterogeneity of the blockage in the flow channel. In addition, there was an experiment in which sealing was confirmed and another in which it was not, even when the same core was used. The result of the latter experiment could be attributed to the fact that the hydrate sealing layer did not form homogeneously as a result of the stochastic nature of hydrate formation and insufficient hydrate growth. From the above, it is important to form the hydrate sealing layer as homogeneously as possible to realize hydrate CCS, and it is necessary to investigate methods to achieve it.