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• W4205156950 abstract "Abstract Mineral trapping (MT)is the most secure method of sequestering carbon for geologically significant periods of time. The processes behind MT fundamentally occur at the pore scale, therefore understanding which factors control MT at this scale is crucial. We present a finite elements advection–diffusion–reaction numerical model which uses true pore geometry model domains generated from $$upmu$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML> <mml:mi>μ</mml:mi> </mml:math> CT imaging. Using this model, we investigate the impact of pore geometry features such as branching, tortuosity and throat radii on the distribution and occurrence of carbonate precipitation in different pore networks over 2000 year simulated periods. We find evidence that a greater tortuosity, greater degree of branching of a pore network and narrower pore throats are detrimental to MT and contribute to the risk of clogging and reduction of connected porosity. We suggest that a tortuosity of less than 2 is critical in promoting greater precipitation per unit volume and should be considered alongside porosity and permeability when assessing reservoirs for geological carbon storage (GCS). We also show that the dominant influence on precipitated mass is the Damköhler number, or reaction rate, rather than the availability of reactive minerals, suggesting that this should be the focus when engineering effective subsurface carbon storage reservoirs for long term security. Article Highlights The rate of reaction has a stronger influence on mineral precipitation than the amount of available reactant. In a fully connected pore network preferential flow pathways still form which results in uneven precipitate distribution. A pore network tortuosity of <2 is recommended to facilitate greater carbon mineralisation." @default.
• W4205156950 created "2022-01-25" @default.
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• W4205156950 date "2022-01-10" @default.
• W4205156950 modified "2023-10-01" @default.
• W4205156950 title "Pore Scale Numerical Modelling of Geological Carbon Storage Through Mineral Trapping Using True Pore Geometries" @default.
• W4205156950 cites W1511313911 @default.
• W4205156950 cites W1571636227 @default.
• W4205156950 cites W1589984731 @default.
• W4205156950 cites W1840410085 @default.
• W4205156950 cites W1980447427 @default.
• W4205156950 cites W1981089961 @default.
• W4205156950 cites W1990958275 @default.
• W4205156950 cites W1995838883 @default.
• W4205156950 cites W1998743714 @default.
• W4205156950 cites W2000583490 @default.
• W4205156950 cites W2001719940 @default.
• W4205156950 cites W2005919141 @default.
• W4205156950 cites W2009736707 @default.
• W4205156950 cites W2014030308 @default.
• W4205156950 cites W2014345605 @default.
• W4205156950 cites W2019776265 @default.
• W4205156950 cites W2021174999 @default.
• W4205156950 cites W2022737008 @default.
• W4205156950 cites W2023144725 @default.
• W4205156950 cites W2026632831 @default.
• W4205156950 cites W2027064284 @default.
• W4205156950 cites W2030150540 @default.
• W4205156950 cites W2038869317 @default.
• W4205156950 cites W2040505957 @default.
• W4205156950 cites W2041228052 @default.
• W4205156950 cites W2045581122 @default.
• W4205156950 cites W2051524198 @default.
• W4205156950 cites W2054113323 @default.
• W4205156950 cites W2057461271 @default.
• W4205156950 cites W2061892033 @default.
• W4205156950 cites W2062178130 @default.
• W4205156950 cites W2063538171 @default.
• W4205156950 cites W2065585407 @default.
• W4205156950 cites W2079035077 @default.
• W4205156950 cites W2081405217 @default.
• W4205156950 cites W2081558924 @default.
• W4205156950 cites W2084193439 @default.
• W4205156950 cites W2091994363 @default.
• W4205156950 cites W2122729947 @default.
• W4205156950 cites W2126912780 @default.
• W4205156950 cites W2127013476 @default.
• W4205156950 cites W2132381759 @default.
• W4205156950 cites W2133059825 @default.
• W4205156950 cites W2136502152 @default.
• W4205156950 cites W2145275539 @default.
• W4205156950 cites W2156157987 @default.
• W4205156950 cites W2163997102 @default.
• W4205156950 cites W2288568740 @default.
• W4205156950 cites W2290822253 @default.
• W4205156950 cites W2293264440 @default.
• W4205156950 cites W2325008094 @default.
• W4205156950 cites W2347721209 @default.
• W4205156950 cites W2403547365 @default.
• W4205156950 cites W2470672803 @default.
• W4205156950 cites W2491455239 @default.
• W4205156950 cites W2538584355 @default.
• W4205156950 cites W2581553661 @default.
• W4205156950 cites W2586303775 @default.
• W4205156950 cites W2726733518 @default.
• W4205156950 cites W2748850286 @default.
• W4205156950 cites W2802037088 @default.
• W4205156950 cites W2885127862 @default.
• W4205156950 cites W2914263695 @default.
• W4205156950 cites W2917491640 @default.
• W4205156950 cites W2923077062 @default.
• W4205156950 cites W2972053215 @default.
• W4205156950 cites W2979653715 @default.
• W4205156950 cites W2998909275 @default.
• W4205156950 cites W2999923687 @default.
• W4205156950 cites W3081275211 @default.
• W4205156950 cites W3088642077 @default.
• W4205156950 cites W3112349681 @default.
• W4205156950 cites W3120775468 @default.
• W4205156950 cites W3122620110 @default.
• W4205156950 cites W3165627791 @default.
• W4205156950 cites W3168193159 @default.
• W4205156950 cites W3211159175 @default.
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• W4205156950 doi "https://doi.org/10.1007/s11242-021-01741-9" @default.
• W4205156950 hasPublicationYear "2022" @default.
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