2019
DOI: 10.1007/s12517-019-4852-8
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Experimental study on the mechanical properties weakening mechanism of siltstone with different water content

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Cited by 23 publications
(11 citation statements)
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“…After the soaking time of 48 h, the water content exhibits no significant change, indicating that the coal specimen is in a saturation condition. is phenomenon is in good agreement with the results of previous studies on rock and coal specimens [6,21,31]. As shown in Figure 2, the water content of this coal under saturation conditions is approximately 3.6%.…”
Section: Coal Sample Preparationsupporting
confidence: 92%
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“…After the soaking time of 48 h, the water content exhibits no significant change, indicating that the coal specimen is in a saturation condition. is phenomenon is in good agreement with the results of previous studies on rock and coal specimens [6,21,31]. As shown in Figure 2, the water content of this coal under saturation conditions is approximately 3.6%.…”
Section: Coal Sample Preparationsupporting
confidence: 92%
“…On one hand, water injection is an effective method for mitigating and preventing rockburst [1][2][3], coal bumps [4], and coal and gas outburst disasters [5]. On the other hand, water can change the microstructure of rock [6][7][8], induce stress redistribution around a tunnel, and lead to damage or failure of the rock due to a change in its mechanical properties [9]. For example, heavy rains in the summer months may result in landslides [10], water bursting in mines [11], roof fall, and pillar instability [12].…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, the physicochemical reactions between the phyllosilicates present in these stones and water might cause their swelling, promoting the growth of initial microcracks and the formation of new cracks, which reduce the values of σpeak of the saturated specimens. Particularly, although no significant macroscopic changes in geometry of the specimens were found during saturation, illite can increase its volume by 50 or 60% when encounters water, causing microcracks [64]. These effects could have happened with greater intensity in R-3, which is the stone with higher clay minerals (chlorite and illite) contents.…”
Section: Impact Of Water On Peak and Residual Compressive Strength And Tangent Young´s Modulusmentioning
confidence: 94%
“…The increase of hydroxyl ion concentration can accelerate the cracking speed of microcracks under stress. [64], [65].…”
Section: Impact Of Water On Peak and Residual Compressive Strength And Tangent Young´s Modulusmentioning
confidence: 99%
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