Geomechanics and Geotechnics of Particulate Media 2017
DOI: 10.1201/9781315106656-68
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Micro and macroscopic processes on the collapse and growth of cavity regions in a granular material due to viscous flow

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Cited by 3 publications
(5 citation statements)
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“…Duran 1997). We have chosen the front-end boundary of respective cavities to be such positions, which is supported in our 2D experiment (Kaneko and Sano 2005, Sano and Nagata 2006, 2006b, Sano 2020. Generally speaking, however, granular material is more often inhomogeneous in practice, so that a catastrophic configuration change can be triggered at any positions.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…Duran 1997). We have chosen the front-end boundary of respective cavities to be such positions, which is supported in our 2D experiment (Kaneko and Sano 2005, Sano and Nagata 2006, 2006b, Sano 2020. Generally speaking, however, granular material is more often inhomogeneous in practice, so that a catastrophic configuration change can be triggered at any positions.…”
Section: Discussionmentioning
confidence: 99%
“…Enhancement of the flow at the center of a cavity as much as three times of the undisturbed flow is noteworthy for the accurate prediction of the groundwater flow by a single boring method in the field work measurement. They also pointed out the possibility of the collapse of the cavities and global fluidization, which are caused by the local enhancement of the stress on the cavity boundaries due to the concentration of incident flow (Kaneko and Sano 2005, Sano and Nagata 2006, 2006b, Koizumi et al 2009, Sano 2011, Sano et al 2013.…”
Section: Introductionmentioning
confidence: 99%
“…If, however, a number of cavities are distributed within a well-interacting distance, the fluidized region will merge to form a long waterway. The details on the flow through a noncircular cavity are given in [7,8], while evolution of the cavity shape, migration and merging of cavities are given in [10][11][12][13][14]. Furthermore, if many such waterways spread sheet-like and slanted, as is often observed on the boundary of impermeable layer of stratum, one side of the granular layer is disconnected to the other side, which can be a cause of landslide at a heavy rainfall.…”
Section: Discussionmentioning
confidence: 99%
“…Flow concentration enhances the local stress on the upstream-side boundary of the cavity, so that the grains of that part will be eroded and carried to the downstream-side boundary if it exceeds certain criteria. This process effectively causes the migration of the cavity towards the upstream direction, or a narrow waterway formation in the medium as was previously shown [10][11][12][13][14][15]. In this paper, we reformulate the analysis on the fundamental flow through a single cavity, and apply it to the interaction of two cavities.…”
Section: Introductionmentioning
confidence: 87%
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