9 ) and experimental corrected diffusivities (black dots) show a decreasing trend with framework hydrophilicity; however, a six orders of magnitude difference is noticeable for the absolute values, even though D eff ≅ D T should approximate ΓD at low pore hydrations ( equation (3) ).
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Interplay between hydrophilicity and surface barriers on water transport in zeolite membranes.
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