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(b) Distribution of two-dimensional self-diffusion coefficients of oxygen parallel to the forsterite surface.
(c) Distribution of two-dimensional self-diffusion coefficients of oxygen parallel to the forsterite surface at 1,673 K.
Figure 10b gives the distribution of two-dimensional self-diffusion coefficients of oxygen parallel to the forsterite surface, and Figure 10c shows the calculated viscosities.
(c) Distribution of two-dimensional self-diffusion coefficients of oxygen parallel to the forsterite surface at 1,673 K. Figure 12 Mg/Si ratios, elements, and self-diffusion coefficients of oxygen for forsterite-MgSiO 3 with 28-nm liquid film.
Figure 6b gives a distribution of the two-dimensional self-diffusion coefficients of oxygen parallel to the forsterite surface, and Figure 6c shows the calculated viscosities determined using the Einstein-Stokes relation with the effective radius obtained by Lacks et al. ( 2007).
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(b) Distribution of Q-species perpendicular to the forsterite surface.
Figure 8b gives the distribution of Q-species perpendicular to the forsterite surface at 1,673 K.
Figure 5 Distribution of the direction of Si-O-Si bridging perpendicular to the forsterite surface.
Figure 9 shows the distribution of the direction of the Si-O-Si bridging perpendicular to the forsterite surface.
Figure 4b gives a distribution of Q-species of Si atoms perpendicular to the forsterite surface at 1,773 K.
Figure 5 shows a distribution of the direction of the Si-O-Si bridging perpendicular to the forsterite surface as a square of the cosine between the z-axis and the vector Si-Si calculated as an inner product.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.
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CEO of Professional Science Editing for Scientists @ prosciediting.com