Physics
Scientific paper
Mar 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30e..30g&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 5, pp. 30-1, CiteID 1226, DOI 10.1029/2002GL015905
Physics
Physical Properties Of Rocks: Permeability And Porosity, Physical Properties Of Rocks: Fracture And Flow, Physical Properties Of Rocks: General Or Miscellaneous
Scientific paper
The temporary pressure drop observed during post-peak dilatant slip in axi-symmetric testing of a porous aeolian sandstone is modeled using a simple function of opening caused by sliding along the fault surface. Results suggest dilatancy of 0.02 mm accompanying frictional sliding, less than 10% of the typical grain diameter of 0.25-0.50 mm. The rapid void opening, under nominally undrained conditions at constant upstream flow rate, causes a strong `suction pump' effect. A theoretical maximum pressure drop of 0.09 MPa or more, consistent with the experimentally measured results, can occur without a change in permeability properties.
Grueschow Eric
Kwon Ohmyoung
Main Ian. G.
Rudnicki John W.
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