Non-Fickian diffusion affects the relation between the salinity and hydrate capacity profiles in marine sediments
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Fick’s law expresses the proportionality of solute flux with respect to concentration gradient. Similar relations are Darcy’s law for the fluid flow in porous media, Ohm’s law for the electric flux and Fourier’s law for heat transfers. When introduced in the corresponding balance equations, these flux laws yield diffusion equations of parabolic character. Different attempts have been made to ob...
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ژورنال
عنوان ژورنال: Comptes Rendus Mécanique
سال: 2013
ISSN: 1631-0721
DOI: 10.1016/j.crme.2013.01.014