Spontaneous switching of permeability changes in a limestone fracture with net dissolution
By A. Polak, Derek Elsworth, Jishan Liu, A. Grader. 2002
139 citations recorded by the source corpus.
Subfields: Environmental Engineering, Mechanical Engineering, Mechanics of Materials
View Paper: https://www.semanticscholar.org/paper/687727f1bdc081d4f341a45f712cdfb968e251cd
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In Environmental Engineering
In Mechanical Engineering
In Mechanics of Materials
Citations in the corpus
- Dissolution and deformation in fractured carbonates caused by flow of CO2-rich brine under reservoir conditions (2013, background): “ecreasing and then increasing permeability are attributed to issolution of contacting asperities at early time followed by disolution of the fracture surfaces in open regions of the fracture at ater time (Polak et al., 2004; Liu et al., 2006).”
- Impact of coating development on the hydraulic and transport properties in argillaceous limestone fracture (2007, background): “Positive feedback can occur, leading to instability and dissolution fingering, as observed in experimental [Detwiler et al., 2003; Durham et al., 2001; Polak et al., 2004] and numerical studies [Békri et al., 1997; Cheung and Rajaram, 2002; Hanna and Rajaram, 1998].”