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Pore-scale permeability prediction for Newtonian and non-Newtonian fluids
2019
Solid Earth Discussions
<p><strong>Abstract.</strong> The flow of fluids through porous media such as groundwater flow or magma migration are key processes in geological sciences. Flow is controlled by the permeability of the rock, thus an accurate determination and prediction of its value is of crucial importance. For this reason, permeability has been measured across different scales. As laboratory measurements exhibit a range of limitations, the numerical prediction of permeability at conditions where laboratory
doi:10.5194/se-2019-84
fatcat:wrqne3trprc7hbtpeshp2d2hki