scholarly journals The impact of heterogeneity on the capillary trapping of CO2 in the Captain Sandstone.

2021 ◽  
Vol 112 ◽  
pp. 103511
Author(s):  
Catrin Harris ◽  
Samuel J. Jackson ◽  
Graham P. Benham ◽  
Samuel Krevor ◽  
Ann H. Muggeridge
2020 ◽  
Vol 83 ◽  
pp. 103588
Author(s):  
Yiran Zhu ◽  
Huilin Xing ◽  
Victor Rudolph ◽  
Zhongwei Chen

2010 ◽  
Vol 662 ◽  
pp. 329-351 ◽  
Author(s):  
C. W. MACMINN ◽  
M. L. SZULCZEWSKI ◽  
R. JUANES

Injection of carbon dioxide (CO2) into geological formations is widely regarded as a promising tool for reducing global atmospheric CO2 emissions. To evaluate injection scenarios, estimate reservoir capacity and assess leakage risks, an accurate understanding of the subsurface spreading and migration of the plume of mobile CO2 is essential. Here, we present a complete solution to a theoretical model for the subsurface migration of a plume of CO2 due to natural groundwater flow and aquifer slope, and subject to residual trapping. The results show that the interplay of these effects leads to non-trivial behaviour in terms of trapping efficiency. The analytical nature of the solution offers insight into the physics of CO2 migration, and allows for rapid, basin-specific capacity estimation. We use the solution to explore the parameter space via the storage efficiency, a macroscopic measure of plume migration. In a future study, we shall incorporate CO2 dissolution into the migration model and study the importance of dissolution relative to capillary trapping and the impact of dissolution on the storage efficiency.


2015 ◽  
Vol 51 (11) ◽  
pp. 9094-9111 ◽  
Author(s):  
Helmut Geistlinger ◽  
Iman Ataei‐Dadavi ◽  
Sadjad Mohammadian ◽  
Hans‐Jörg Vogel

Water ◽  
2020 ◽  
Vol 12 (2) ◽  
pp. 445 ◽  
Author(s):  
Tomas Princ ◽  
Helena Maria Reis Fideles ◽  
Johannes Koestel ◽  
Michal Snehota

The relationship between entrapped air content and the corresponding hydraulic conductivity was investigated experimentally for two coarse sands. Two packed samples of 5 cm height were prepared for each sand. Air entrapment was created by repeated infiltration and drainage cycles. The value of K was determined using repetitive falling-head infiltration experiments, which were evaluated using Darcy’s law. The entrapped air content was determined gravimetrically after each infiltration run. The amount and distribution of air bubbles were quantified by micro-computed X-ray tomography (CT) for selected runs. The obtained relationship between entrapped air content and satiated hydraulic conductivity agreed well with Faybishenko’s (1995) formula. CT imaging revealed that entrapped air contents and bubbles sizes were increasing with the height of the sample. It was found that the size of the air bubbles and clusters increased with each experimental cycle. The relationship between initial and residual gas saturation was successfully fitted with a linear model. The combination of X-ray computed tomography and infiltration experiments has a large potential to explore the effects of entrapped air on water flow.


2019 ◽  
Vol 59 (1) ◽  
pp. 343 ◽  
Author(s):  
Yiran Zhu ◽  
Zhongwei Chen ◽  
Huilin Xing ◽  
Victor Rudolph

The impact of water on gas production has been commonly reflected using relative permeability curves, which are obtained by measuring the flow behaviour of each phase through a core sample. This approach reflects the overall response of a core to flow but is unable to capture the capillary trapping phenomenon at the microscale, which is expected to vary significantly for coals with different microstructures. The overlook of trapping effect could potentially overestimate gas production, a topic that does not appear to be well explored. In this work, the impact of capillary trapping on gas recovery was investigated numerically through a fully coupled water-gas two-phase flow model. The characterisation of a coal microstructure, surface chemistry (e.g. coal wettability) and an isotherm curve was summarised for Bowen Basin coal. Various sensitivity studies were then conducted at coal matrix scale to quantify the amount of gas trapped by capillary forces under different reservoir conditions and production controls. Our results show that for the studied coal parameters from the Bowen Basin, the capillary trapping effect hinders gas breakthrough noticeably, causing unwanted high abandonment pressure and reduction in gas recovery rate. Among all investigated parameters, pore size has the most important effect on trapped gas percentage. If taking 3 MPa as initial reservoir pressure, 300 kPa as the abandonment pressure baseline, 63.58 kPa as the gas breakthrough pressure, then the trapped gas accounts up to 4.02% of the total predicted gas; the trapped gas percentage will increase considerably if the saturation of gas is very low, although this variability is largely dependent on reservoir condition.


2019 ◽  
Vol 55 (11) ◽  
pp. 9905-9925 ◽  
Author(s):  
Ayaz Mehmani ◽  
Shaina Kelly ◽  
Carlos Torres‐Verdín ◽  
Matthew Balhoff

2019 ◽  
Author(s):  
Anna Herring ◽  
Dorthe Wildenschild ◽  
Linnéa Andersson ◽  
Vanessa Robins ◽  
Adrian Sheppard

2011 ◽  
Vol 688 ◽  
pp. 321-351 ◽  
Author(s):  
C. W. MacMinn ◽  
M. L. Szulczewski ◽  
R. Juanes

AbstractThe large-scale injection of carbon dioxide (CO2) into saline aquifers is a promising tool for reducing atmospheric CO2 emissions to mitigate climate change. An accurate assessment of the post-injection migration and trapping of the buoyant plume of CO2 is essential for estimates of storage capacity and security, but these physical processes are not fully understood. In Part 1 of this series, we presented a complete solution to a theoretical model for the migration and capillary trapping of a plume of CO2 in a confined, sloping aquifer with a natural groundwater through-flow. Here, we incorporate solubility trapping, where CO2 from the buoyant plume dissolves into the ambient brine via convective mixing. We develop semi-analytical solutions to the model in two limiting cases: when the water beneath the plume saturates with dissolved CO2 very slowly or very quickly (‘instantaneously’) relative to plume motion. We show that solubility trapping can greatly slow the speed at which the plume advances, and we derive an explicit analytical expression for the position of the nose of the plume as a function of time. We then study the competition between capillary and solubility trapping, and the impact of solubility trapping on the storage efficiency, a macroscopic measure of plume migration. We show that solubility trapping can increase the storage efficiency by several-fold, even when the fraction of CO2 trapped by solubility trapping is small.


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