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To comply with this criterion, a polycrystal line with large and uniform grains (if not a bamboo line or even a single crystal line) with small variation in grain boundary diffusivities should be pursued.
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From the basis of diffusion in air, oxygen diffusivity should be equivalent to 0.176 cm2/s in the air pore of cementitious materials.
The oxygen diffusivity should be based on the pore structure properties of cementitious materials.
Thus, in principle, during the intercalation process Li+ diffusivity should be higher in FeF3·3H2O than in HTB-FeF3·0.33H2O.
In theory, the anisotropic features of thermal diffusivity should be similar to those of thermal conductivity because the volumetric heat capacity is a scalar.
From the emphasis on boundary planes, 'grain boundary plane engineering' should be promoted.
Ideally the boundary itself should be easy to spot.
The geometrical properties and boundary conditions should be mapping accurate.
Regardless of the nature of the boundary, the documentation of the boundary position should be sufficient to allow the boundary to be relocated should it somehow be destroyed.
A pre-determined network boundary should be established and reported.
To protect the structure in a diffusion process, the diffusivity parameter should be made dependent on some characterization of image structure.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com