2015
DOI: 10.1016/j.ijrmms.2015.08.021
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Swelling behavior of volcanic rocks under cyclic wetting and drying

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Cited by 39 publications
(14 citation statements)
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“…These minerals would swell after absorbing water and eventually lead to rock damage and destruction [66][67][68][69][70]. The cyclic dry-wet treatment process would cause repeated expansion and contraction of clay components, and moisture fluctuation is the main reason [71][72][73][74]. The volume of expanded clay changes with the fluctuation of water, which causes the air pressure in the pores to rise sharply, and finally ruptures to form cracks.…”
Section: Clay Content and Swellingmentioning
confidence: 99%
“…These minerals would swell after absorbing water and eventually lead to rock damage and destruction [66][67][68][69][70]. The cyclic dry-wet treatment process would cause repeated expansion and contraction of clay components, and moisture fluctuation is the main reason [71][72][73][74]. The volume of expanded clay changes with the fluctuation of water, which causes the air pressure in the pores to rise sharply, and finally ruptures to form cracks.…”
Section: Clay Content and Swellingmentioning
confidence: 99%
“…(1) maximum swelling pressure test (ISRM 1999) and (2) the cyclic swelling test with controlled deformation (Vergara and Triantafyllidis 2015). The maximum swelling pressure test was performed on both powder and intact rock specimens, whereas the cyclic oedometer test was applied on the intact rock specimen.…”
Section: Oedometer Swelling Testsmentioning
confidence: 99%
“…Apparatus for performing oedometer swelling tests (1) Rigid frame, (2) ring and specimen, (3) watering cell, (4) porous metal sintered plates, (5) manual spindle, (6) load cell and (7) dial gauges(Vergara and Triantafyllidis 2015) …”
mentioning
confidence: 99%
“…Many valuable achievements about the influence of drying and wetting cycles to various rocks have been studied by domestic and foreign researchers. Liu and Deng et al [6,7] examined the deterioration laws of sandstone under waterrock interaction, including the changes of compressive strength and rheological properties; Hua et al [8] studied the fracture toughness of sandstone subjected to cyclic wetting and drying; the swelling behavior of volcanic rocks or mudstone and stabilized expansive soils has been studied by Vergara et al, Doostmohammadi et al, and Rao et al, respectively [9][10][11]; the effects of acid rain on the mechanical properties and the stability of reservoir slope slump under the condition of acid rain were examined by Liu et al [12][13][14]; Zhao et al [15] have investigated the change laws of tensile strength of sandstone with low clay mineral content; Liu et al [16] have studied the crack growth mechanism, especially subcritical crack under water-rock interaction; and Saleh-Mbemba et al [17] examined the water retention of tailings behavior. As for altered rock, the hydromechanical properties of altered rock have been analyzed by Wang et al [18], and Kohno et al and Chen et al [19,20] have studied the relations between point load strength index and UCS (uniaxial compressive strength) of hydrothermally altered soft rock.…”
Section: Introductionmentioning
confidence: 99%