Grain-size to effective pore-size transformation derived from electrokinetic theory
By P. Glover, E. Walker. 2009
168 citations recorded by the source corpus.
Subfields: Geophysics, Mechanics of Materials, Nuclear and High Energy Physics
View Paper: https://www.semanticscholar.org/paper/15b366af7a4644c8f0cb239947d2711fef42cee0
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In Geophysics
In Mechanics of Materials
In Nuclear and High Energy Physics
Citations in the corpus
- What determines drying rates at the onset of diffusion controlled stage‐2 evaporation from porous media? (2011, methodology): “Additionally, we used 0.67 mm as a typical pore size of sandstone with particle size of 2 mm according to a � d/3 [ Glover and Walker, 2009 ].”
- Geophysical Properties of the Near Surface Earth: Electrical Properties (2015, methodology): “Pore diameter and grain diameter are related by the theatre transformation (Glover and Walker, 2009), and the pore size is related to the pore throat size using empirical methods (Glover and Déry, 2010).”
- Combined evaporation and salt precipitation in homogeneous and heterogeneous porous media (2011, methodology): “Pore sizes were calculated from measurements of soil water retention curves [Hillel, 1998] and from grain dimensions [Glover and Walker, 2009].”