scholarly journals An illustration of the effect of neglecting poroelastic physics of water-saturated glass beads in a laboratory phase speed inference process

2019 ◽  
Vol 146 (2) ◽  
pp. 1326-1334
Author(s):  
Gabriel R. Venegas ◽  
Preston S. Wilson
2010 ◽  
Vol 128 (6) ◽  
pp. 3344-3354 ◽  
Author(s):  
Guillaume Renaud ◽  
Samuel Callé ◽  
Marielle Defontaine
Keyword(s):  

2008 ◽  
Vol 321 (1) ◽  
pp. 103-117 ◽  
Author(s):  
P. Leroy ◽  
A. Revil ◽  
A. Kemna ◽  
P. Cosenza ◽  
A. Ghorbani

1985 ◽  
Vol 6 ◽  
pp. 43-47 ◽  
Author(s):  
D. Powers ◽  
S.C. Colbeck ◽  
K. O'Neill

Thermal convection is observed in snow and in a compact of water-saturated glass beads. While uncertainty in the permeability of the snow limits our ability to compare the observed and calculated onset of convection, agreement between the observed and calculated effects of convection on heat transfer in snow is good. Experimental results with glass beads agree with both the calculated onset of and heat transfer by convection. Attempts are made to assess the effects of convection on snow metamorphism. While much is still uncertain about the significance of thermal convection in snow, it is clear that the phenomenon does occur.


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