2022
DOI: 10.1063/5.0073967
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Effect of relative humidity on the nonlinear elastic response of granular media

Abstract: We study the influence of relative humidity (RH) on the nonlinear elastic response of granular media. Previous work has shown that the nonlinear elastic response of consolidated granular media like rocks likely arises from two distinct mechanisms; however, we do not have a clear understanding of their physical origins at the microscopic scale. Here, we conduct dynamic acousto-elastic testing (DAET) on samples of glass beads under dry (∼10%), ambient (∼60%), and humid (∼100%) conditions at room temperature and … Show more

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Cited by 10 publications
(30 citation statements)
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“…We prepare samples of spherical soda-lime glass beads (diameter 100-140µm, Mo-Sci Corporation, Rolla, Missouri) and angular, fine quartz sand (diameter 50-150µm, 99.8% SiO 2 with minor amounts of Fe 2 O 3 , Al 2 O 3 , <0.1% each, U.S. Silica Company) using a setup identical to our previous study (Gao et al, 2022). We place a 4.5 mm thick pack of granular media (i.e., glass beads or sand) on top of a steel block of area 10*10 cm 2 .…”
Section: Methodsmentioning
confidence: 99%
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“…We prepare samples of spherical soda-lime glass beads (diameter 100-140µm, Mo-Sci Corporation, Rolla, Missouri) and angular, fine quartz sand (diameter 50-150µm, 99.8% SiO 2 with minor amounts of Fe 2 O 3 , Al 2 O 3 , <0.1% each, U.S. Silica Company) using a setup identical to our previous study (Gao et al, 2022). We place a 4.5 mm thick pack of granular media (i.e., glass beads or sand) on top of a steel block of area 10*10 cm 2 .…”
Section: Methodsmentioning
confidence: 99%
“…The sample is then quickly taken out of the sealed bag and a second steel block of identical size is placed on top of the granular layer. The sides are sealed using multiple layers of tape (Gao et al, 2022).…”
Section: Methodsmentioning
confidence: 99%
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“…The transient dynamics is generally interpreted as the result of 1) a phase of "damage" during deformation that arises from a variety of contacts (Ostrovsky et al 2019; which are broken at grain boundaries or at defect locations and 2) a phase of "healing" associated with thermally activated processes that bring the metastable contacts towards a new equilibrium state -a phase also called slow dynamics or relaxation (Guyer et al 1999;TenCate et al 2000). In rocks and near-surface geomaterials, this contact recovery is thought to happen due to micro-cracks and fracture closure (Meyer et al 2021) or re-arrangement of frictional shear zones (Lieou et al 2017) and with a large contribution of chemical processes modulated by moisture (Brantut 2015;Bittner & Popovics 2021;Gao et al 2022). Corresponding physical and phenomenological models can be developed from laboratory observations thanks to a fine control of the strain disturbance (Remillieux et al 2017), a well-resolved temporal acoustic monitoring system (that can observe relaxation timescales down to fractions of a second (Shokouhi et al 2017b)), simplified geometries (Yoritomo & Weaver 2020) or the knowledge of the physical properties of the chosen rock samples.…”
Section: Introductionmentioning
confidence: 99%