Work

Temporal Dynamics of Reactive CO 2 Flow in Carbonate Rock: Insights from 4D Synchrotron Imaging

Year: 2025
Type: article
Abstract: -saturated brine through the sample with in situ scanning to track the different stages of chemical dissolution. Analysis of the images shows a channelled dissolution pattern which corresponds with a gradual increase in porosity due to pore structure changes. Pore network models were generated from the segmented images to carry out a sequence of drainage and imbibition simulations. The result demonstrated that reduced capillary entry pressure with increased pore connectivity after dissolution. Furthermore, the trapping efficiency was quantified to predict a slight decrease in dissolution as the pores become broader and better connected.
Language: English
Open Access status: hybrid
Estimated APC paid: $4,500
OpenAlex ID: W4414976573
FWCI: 3.408
Cites: 60
Cited by: 12
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