In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 122, No. 3 ( 2017-03), p. 1726-1743
Abstract:
The fluid‐solid interaction problem is solved numerically in a porous limestone core sample at several stages of dissolution Probability density functions of fluid velocity and solid stress evolve self‐similarly as porosity and flow rate is varied The unified distributions provide an additional explanation of the sensitivity of rocks to failure due to fluid flow and dissolution
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1002/2016JB013536
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13
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