2022
DOI: 10.1038/s41598-022-19287-1
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Development of the shear displacement of sandy soil due to absorption under constant shear stress for creep failure

Abstract: Measurement of the displacement and pore pressure in physical model slopes and natural slopes revealed that not only an accelerative increase up to failure but also a decelerative increase occurred in surface displacement under a constant groundwater level, which could be recognized as creep deformation under constant stress. The displacement increased significantly at first in both types, which made it difficult to evaluate whether the displacement developed to the point of failure at the start of the increas… Show more

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