Construct · 1 fields · 1 citations

Biot poroelasticity: a standalone construct

One name. One construct. A landmark on the map.

● anchor · a standalone construct Nearest construct by meaning·not indexed
Biotporoelasticity1 CONSTRUCTBiot poroelasticity BIOT · GEOPHYSICS

A single standalone construct; nearby constructs are located against it in the Collider. Tap a field for its definition, unit, and measures.

Geophysics

the theory of coupled deformation of a porous solid and flow of the fluid filling its pores.

In geophysics, Biot poroelasticity refers to the theory of coupled deformation of a porous solid and flow of the fluid filling its pores. This meaning comes from Biot (1941) in Journal of Applied Physics.[1]

Unit
Recovery means
Measured by

Next

Run it through the Collider, or take the citations with you.

See how Biot poroelasticity sits against neighbouring constructs in the Collider, or export every reference on this page in one click.

Open in ColliderExport BibTeXReport this entry

Nearby constructs

Biot slow wave1 fields · 1 citationsanchor · a standalone constructflow6 names · 12 citationsjangle · five names, one experience, partlyMandel-Cryer effect1 fields · 1 citationsanchor · a standalone construct

References

  1. Biot, M. A. (1941). General Theory of Three-Dimensional Consolidation. Journal of Applied Physics, 12(2), 155-164. https://doi.org/10.1063/1.1712886

Cited on this page?

Confirm your construct, or correct us.

If your work is cited behind one of these entries, you know better than we do whether we captured the meaning right. Confirm it, suggest an edit, or dispute it, and your name goes on the entry as an author who has checked it, linked to your ORCID.

Claim your construct