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Therefore, the rate of approach of equilibrium for a given estimator has to be evaluated to determine whether or not equilibrium is a strong assumption in particular case studies.
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Retrieved geometric surface area normalised mineral dissolution rates are most rapid at the surface and at the bedrock soil interface; this behaviour is interpreted to stem from a combination of the approach to equilibrium of the soil waters with depth and more rapid dissolution rates of fresh versus weathered surfaces.
In an important work (listed in the bibliography), P. and T. Ehrenfest also offered a reading of the Boltzmann equation of approach to equilibrium that avoided recurrence objections.
The conventional approach of limit equilibrium methods provide safety factors for the slope but nothing about the stress-strain characteristics of the large dump mass.
This precludes a characterisation of the approach to equilibrium in terms of increasing Gibbs entropy, which is what one would expect if we were to treat the Gibbs entropy as the SM counterpart of the thermodynamic entropy.
Moreover, increasing temperature resulted in an increase in the rate of approach to equilibrium.
Both Maxwell and L. Boltzmann went further, and in different, but related, ways derived an equation for the approach to equilibrium of a gas.
Tests were also conducted with variable contact time to evaluate mass-transfer rates and the rate of approach to equilibrium dissolution.
This is particularly important in calculating the approach to equilibrium of the high-energy tail, or the equilibrium under the competing influences of e-e collisions, inelastic electron neutral collisions, and end losses through sheaths.
However, equilibrium applies in the long term; effect sizes and epistasis do influence the rate of approach to equilibrium.
That is, what are the salient features of the approach to equilibrium and what features of a system make it behave in this way?
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CEO of Professional Science Editing for Scientists @ prosciediting.com