This section is part of: Athanasopoulos, G. A. (2021) "Online Lecture Notes on Soil Mechanics", Geoengineer.org, DOI: https://doi.org/10.48246/GEOENG-EDU-001
Contents [show]
The Mohr’s circle has the characteristic property that the abscissa and ordinate (σθ,τθ) at a point A of the circle give us the stress state on a plane where the vertical of the plane forms an angle θ with respect to the direction of the principal stress σ₁. In soil mechanics, the stresses are simulated as follows:
It’s a point on the Mohr’s circle (which is symbolized with O🇵) for which: if we draw a line parallel with the plane of which we want to define the stress state (σ,τ), the line will cross the circle at a point with coordinates (σ,τ).
Problem 2.1 For the stress state of the following figure: Find the stresses (normal and shear)...
To solve the problem of the stress distribution in the soil, induced by a surcharge at the su...
Geostatic stresses When the soil has a horizontal surface and there is no horizontal variabilit...
Introduction Triaxial tests are widely used in geotechnical engineering both in soil and rock mec...
A new study presents the first quantitative stress magnitude map that also includes horizontal stre...
Shear strength is the ability of a material to resist shear forces - that is, forces that produce a...
Overburden Stress, also called Vertical Stress or Overburden Pressure, is the pressure imposed on a...