2019
DOI: 10.1016/j.coldregions.2019.03.012
|View full text |Cite
|
Sign up to set email alerts
|

Damage evolution model of sandstone under coupled chemical solution and freeze-thaw process

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
5

Citation Types

0
10
0

Year Published

2020
2020
2022
2022

Publication Types

Select...
10

Relationship

0
10

Authors

Journals

citations
Cited by 46 publications
(12 citation statements)
references
References 32 publications
0
10
0
Order By: Relevance
“…A uniaxial compression test was carried out for the rock immersed in the chemical solution, the chemical damage mechanism was analyzed, and the damage constitutive model was established [4,34]. The damage evolution model of rock under the coupled chemical-freeze-thaw action is constructed [35,36]. In order to study the damage evolution law of prefabricated cracked red sandstone samples under uniaxial cyclic compression, physical tests were carried out.…”
Section: Introductionmentioning
confidence: 99%
“…A uniaxial compression test was carried out for the rock immersed in the chemical solution, the chemical damage mechanism was analyzed, and the damage constitutive model was established [4,34]. The damage evolution model of rock under the coupled chemical-freeze-thaw action is constructed [35,36]. In order to study the damage evolution law of prefabricated cracked red sandstone samples under uniaxial cyclic compression, physical tests were carried out.…”
Section: Introductionmentioning
confidence: 99%
“…In addition to rock damage under loading (compression, tension and shear), the SDM has also been widely used in research of rock damage in the multiphysical environment [28][29][30][31][32]. The factors of porosity, temperature, or freezethaw cycles were introduced into the damage variables of SDM under the multiphysical conditions.…”
Section: Introductionmentioning
confidence: 99%
“…Guo et al [7] further carry out a series of hydraulic fracturing experiments and find that etching wormholes induced by the rock-acid reaction would change the pore structure of carbonate rocks, and gelled acid enables to increase both the width and the roughness of main fracture surfaces. Based on freeze-thaw cycles tests on sandstone immersed in different chemical solutions, Li et al [8] define a pore evolution law of sandstone and find that the porosity alteration is the most obvious in the first ten freeze-thaw cycles. Huang et al [9] state that iron ions and magnesium ions provided by the dissolution of ankerite in the acid fluid can promote the formation of chlorite, which is likely to block the pore throats and thus decrease the rock permeability.…”
Section: Introductionmentioning
confidence: 99%