Imperial College London
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ProfessorMartinBlunt

Faculty of Engineering, Department of Earth Science & Engineering

Chair in Flow in Porous Media
 
 
 
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Contact

 

+44 (0)20 7594 6500m.blunt Website

 
 
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Location

 

2.38ARoyal School of MinesSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Moghadasi:2023:10.1016/j.advwatres.2023.104499,
author = {Moghadasi, R and Goodarzi, S and Zhang, Y and Bijeljic, B and Blunt, MJ and Niemi, A},
doi = {10.1016/j.advwatres.2023.104499},
journal = {Advances in Water Resources},
pages = {1--8},
title = {Pore-scale characterization of residual gas remobilization in CO2 geological storage},
url = {http://dx.doi.org/10.1016/j.advwatres.2023.104499},
volume = {179},
year = {2023}
}
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RIS format (EndNote, RefMan)

TY  - JOUR
AB  - A decrease in reservoir pressure can lead to remobilization of residually trapped CO2. In this study, the pore-scale processes related to trapped CO2 remobilization under pressure depletion were investigated with the use of high-resolution 3D X-ray microtomography. The distribution of CO2 in the pore space of Bentheimer sandstone was measured after waterflooding at a fluid pressure of 10 MPa, and then at pressures of 8, 6 and 5 MPa. At each stage CO2 was produced, implying that swelling of the gas phase and exsolution allowed the gas to reconnect and flow. After production, the gas reached a new position of equilibrium where it may be trapped again. At the end of the experiment, we imaged the sample again after 30 hours. Firstly, the results showed that an increase in saturation beyond the residual value was required to remobilize the gas, which is consistent with earlier field-scale results. Additionally, Ostwald ripening and continuing exsolution lead to a significant change in fluid saturation: transport of dissolved gas in the aqueous phase to equilibriate capillary pressure led to reconnection of the gas and its flow upwards under gravity. The implications for CO2 storage are discussed: an increase in saturation beyond the residual value is required to mobilize the gas, but Ostwald ripening can allow local reconnection of hitherto trapped gas, thus enhancing migration and may reduce the amount of CO2 that can be capillary trapped in storage operations.
AU  - Moghadasi,R
AU  - Goodarzi,S
AU  - Zhang,Y
AU  - Bijeljic,B
AU  - Blunt,MJ
AU  - Niemi,A
DO  - 10.1016/j.advwatres.2023.104499
EP  - 8
PY  - 2023///
SN  - 0309-1708
SP  - 1
TI  - Pore-scale characterization of residual gas remobilization in CO2 geological storage
T2  - Advances in Water Resources
UR  - http://dx.doi.org/10.1016/j.advwatres.2023.104499
UR  - https://www.sciencedirect.com/science/article/pii/S0309170823001343
UR  - http://hdl.handle.net/10044/1/105837
VL  - 179
ER  -
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