Theory: Mohr's Circle
How the stresses at a point of soil change with the plane, how Mohr's circle shows them, and how the Mohr-Coulomb envelope tells whether the soil fails and on which plane.
Stresses at a point
In plane strain, three values set the stresses at a point: the normal stresses σx and σy on the vertical and horizontal faces of an element and the shear τxy between them. From them follow the stresses on any plane through the point, turned θ from the x-plane:
Since soils are nearly always compressed, soil mechanics takes compression as positive, the opposite of structural mechanics.
Mohr's circle
Mohr showed in 1882 that the pairs (σθ, τθ) of all planes fall on a circle of center s and radius t:
The vertical and horizontal faces are the points X (σx, τxy) and Y (σy, −τxy), at the ends of a diameter. Turning the plane θ turns its point 2θ around the circle, the same way with this page's signs.
Principal stresses
The principal planes carry no shear and are square to each other. The largest shear, equal to t, acts at 45° to them.
Mohr-Coulomb criterion
Coulomb proposed in 1776 that a soil's shear strength rises with the normal stress on the failure plane. In effective stresses:
Mohr joined his circle to that line: the soil fails when the circle touches the envelope, and no stress state can cross it. At failure:
This page compares the circle's radius with that of the circle of the same center tangent to the envelope, Rf = (s + c′ cot φ′) sin φ′. The ratio t / Rf is the stress level: 100% is failure.
Failure plane
The point of tangency is 90° + φ′ around the circle from σ1's point, so the failure plane makes 45° + φ′/2 with the plane σ1 acts on — on either side, in a pair of conjugate planes. Before failure, these are the critical planes, whose points come closest to the envelope.
The failure plane isn't the plane of largest shear: there, the normal stress is higher, and so is the strength.
Limitations
- The criterion holds in effective stresses; with total stresses, use the undrained parameters.
- Plane strain leaves out the intermediate principal stress σ2, which the Mohr-Coulomb criterion ignores too.
- The real envelope is usually curved; the line holds over the range of stresses c′ and φ′ were fitted to.
- At low or tensile stresses the apparent cohesion may not exist, and the soil may crack before touching the envelope.
References
- Coulomb, C. A. Essai sur une application des règles de maximis et minimis à quelques problèmes de statique, relatifs à l'architecture. Mémoires de l'Académie Royale des Sciences, v. 7, 1776.
- Mohr, O. Über die Darstellung des Spannungszustandes und des Deformationszustandes eines Körperelementes. Civilingenieur, v. 28, 1882.
- Lambe, T. W.; Whitman, R. V. Soil Mechanics. New York: Wiley, 1969.
- Das, B. M.; Sobhan, K. Principles of Geotechnical Engineering. 9th ed. Boston: Cengage, 2018.