2020
DOI: 10.1371/journal.pone.0236335
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Fluctuation in residual strain and dissipated energy of saturated sandstone under tiered cyclic loading

Abstract: To study the influence of cyclic stress on the nonlinear behavior of saturated sandstone, the residual strain properties and energy dissipation characteristics of the sandstone under tiered cyclic loading were experimentally investigated. The axial/radial residual deformation and energy dissipation characteristics of sandstone at different cyclic stress stages were analyzed in detail. By combining the mathematical statistics, fluctuation coefficients of the residual strain and energy dissipation, and correlati… Show more

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Cited by 6 publications
(2 citation statements)
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“…The residual strain produced during cyclic loading and unloading can only reflect the plastic deformation characteristics at the loading point and unloading point. In contrast, since an obvious hysteretic effect was produced in the stress–strain curve during cyclic loading and unloading, the area encircled by the loading and unloading curves can reflect the energy dissipation characteristics in each cyclic loading and unloading cycle [ 30 ] and, thus, describe the damage characteristics of coal during cyclic loading and unloading from the perspective of energy dissipation.…”
Section: Discussionmentioning
confidence: 99%
“…The residual strain produced during cyclic loading and unloading can only reflect the plastic deformation characteristics at the loading point and unloading point. In contrast, since an obvious hysteretic effect was produced in the stress–strain curve during cyclic loading and unloading, the area encircled by the loading and unloading curves can reflect the energy dissipation characteristics in each cyclic loading and unloading cycle [ 30 ] and, thus, describe the damage characteristics of coal during cyclic loading and unloading from the perspective of energy dissipation.…”
Section: Discussionmentioning
confidence: 99%
“…Defects of different scales such as pores, joints, cracks and dislocations are naturally formed in rocks in the long geological history process and uneven initial damages exist in rocks [ 20 , 21 ], but the development of initial damage has a stress threshold. Under the continuous action of the stress level above this threshold, the uneven and localized damage evolution phenomenon occurs, thus resulting in aging deformation and failure [ 22 ].…”
Section: Comparative Analysis Of Full Stress-strain Curve and Creep Curve Of Uniaxial Compression Testsmentioning
confidence: 99%