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The current model forms the building block in upscaling colloid transport from pore scale to Darcy scale using Pore-Network Modeling.
Different methods to obtain a digital model of the pore space from pore scale images are presented, and the strengths and weaknesses of the different methods are discussed.
Most of the experimental and numerical studies done on this subject in the past have been limited in their observations because they only considered the dissolution process at a small scale (from pore scale to core scale).
As a result, water flooding is controlled by various factors from pore scale to reservoir scale.
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In addition, permeability and porosity relations are constructed from pore-scale simulations which account for a range of reaction regimes characterized by the Da and Pe numbers.
The functional relationships obtained from pore-scale simulations can be used in a continuum scale model that may account for large-scale phenomena mimicking lateral migration of surface CO2 seeps.
We additionally examine the accuracy of the commonly used empirical memory functions against those directly calculated from pore-scale simulations, finding that none of these functions can accurately describe the mass exchange process.
We verify the model by first showing that it is an improvement and able to reproduce what the spherical model describes, and then testing it against the average oxygen reductions directly calculated from pore-scale simulations of oxygen diffusion and reaction in the two catalyst layers.
Solute dispersion is one of the major mixing mechanisms in transport through porous media, originating from velocity variations at different scales, starting from the pore scale.
In this paper, we aim at discovering the roles of these rheological properties in non-Newtonian fluid displacement from the pore scale.
The constitutive relationships of the non-drainable residual NAPL system are based on qualitative fluid behavior derived from a pore scale model.
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