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General Theory of Three-Dimensional Consolidation

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Biot, Maurice A.·1941·Journal of Applied Physics

Abstract

The settlement of soils under load is caused by a phenomenon called consolidation, whose mechanism is known to be in many cases identical with the process of squeezing water out of an elastic porous medium. The mathematical physical consequences of this viewpoint are established in the present paper. The number of physical constants necessary to determine the properties of the soil is derived along with the general equations for the prediction of settlements and stresses in three-dimensional problems. Simple applications are treated as examples. The operational calculus is shown to be a powerful method of solution of consolidation problems.

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Metadata

Authors
Biot, M. A.
Venue
Journal of Applied Physics
Published
1941-02-01
Volume
12
Issue
2
Pages
155-164
ISSN
  • 0021-8979 (ISSN-L)
  • 1089-7550
OpenAlex
W2055072688
Cited by
9,723
References
0
FWCI
18.82
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: General Theory of Three-Dimensional Consolidation. https://app.cochat.ai/papers/10.1063/1.1712886
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Biot, M. A. (1941). General Theory of Three-Dimensional Consolidation. Journal of Applied Physics. https://doi.org/10.1063/1.1712886

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.