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Findings indicate that residual NAPL saturation is influenced by the shapes of grains of the porous medium more than their sizes.
The calculation of fractional conversion can be very difficult in certain cases of nucleation and growth transformations (Mampel assumptions): it has only been developed for a few shapes of grains (spheres, cylinders) and only in isobaric and isothermal conditions.
DI analysis is proving to be a useful tool and can capture the three dimensional shapes of grains using different image orientations [ 15, 19].
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Diffusion contrast of boundaries and bended shapes of grain boundaries in the crystallites, presented in Fig. 1, confirm such conclusion.
In sedimentary rocks, the amount of pore space depends on the degree of compaction of the sediment (with compaction generally increasing with depth of burial), on the packing arrangement and shape of grains, on the amount of cementation, and on the degree of sorting.
It reflects the shape of grains.
Microscope images were grouped as intergranular properties (shape of grains, shape of grain aggregates, grain boundary type and pressure solution), intragranular properties (twinning and alteration) and deformation.
These findings indicated that OsWOX3B/NUDA/GL-1 RNAi did not affect the size and shape of grains (Figure7a,Additional file 2: Figure S1).
The influence of the magnetic processing of the epitaxial La2Zr2O7 buffer film on the shape of grains has been found.
An atomic force microscopical study has shown that after magnetic processing the shape of grains improved significantly.
This technique makes it possible to solve the coupled partial differential equations for all physical shape of grains.
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