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When the surface diffusivity equals the self-diffusion coefficient, (omega = 1).
are referred to as self-diffusion pressures.
Adding ACN molecules, the variation of f self-diffusion coefficient.
Calculated self-diffusion constants are shown in Fig, 8.
Experimental self-diffusion values are directly related to molecular displacement.
As a result, self-diffusion coefficient almost vanishes.
A natural question is what the difference is between the solution with self-diffusion and without self-diffusion for the same big initial values.
The latter gives the continuity of blow-up with the self-diffusion rate since the solution without self-diffusion blows up.
According to Wu and Kohlstedt (1988), magnetite formation is controlled by self-diffusion of Fe2+, which is comparable to Mg self-diffusion.
The former shows that the solution of the system with self-diffusion or without self-diffusion blows up if the initial value is large enough.
Self-diffusion is roughness dependent, while transport diffusion is not.
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