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Metamorphism results from a complex interplay between physical and chemical processes that operate on a scale ranging from micrometres (e.g., fine mineral grain sizes, thickness of intergranular fluid, diffusion distances for chemical species) to tens or hundreds of kilometres (e.g., crustal thickness, width of collision zone between lithospheric plates, depth to subducting plate).
Slip transfer involves dilatational opening of linking extension fractures and associated fluid diffusion.
TP is composed of frictional heating, thermal diffusion, and fluid diffusion.
In general, frictional heating with fault slip is accompanied by thermal diffusion and fluid diffusion.
The proposed adaptive penalty scheme targets to recover normal fluid diffusion rates for later time stages.
Since fluid diffusion parameters such as permeability vary by several orders of magnitude on faults (e.g. Tsutsumi et al, 2004), the effectiveness of TP is considered to be controlled mainly by fluid diffusion parameters (e.g., Lachenbruch, 1980).
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The fluid-diffusion in the 3rd and 4th chambers mainly happens after the buffer period.
Analytic solutions for the dynamic response of an adiabatic adsorption column based on the rectangular isotherm approximation are derived for fluid film diffusion control and for the case in which both fluid film and intraparticle diffusion resistances are comparable.
Dynamic swelling studies were performed in the simulated intestinal fluid and diffusion coefficients were calculated by considering the spherical geometry of the matrices.
Dynamic boundary conditions are very natural in many mathematical models such as heat transfer in a solid in contact with a moving fluid, thermoelasticity, diffusion phenomena, heat transfer in two mediums, problems in fluid dynamics (see [1 4, 6 11]).
Due to the fact, that in the initial state the resin can be characterized as a fluid, the diffusion coefficient can be described based on the Stokes Einstein equation.
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