Principal Stresses — Mohr's Circle
Fundamental :
The state of stress at a point is typically represented by a cube with axes in the x, y, and z directions. The stress vector on each face is decomposed into a normal stress (e.g., in the x-direction) and two shear stresses (e.g., in the y and z directions).
For equilibrium, shear stresses on perpendicular planes must be equal ().
Definition :
: Normal stress on the plane perpendicular to the x-direction.
: Shear stress on the plane perpendicular to the x-direction and acting in the y-direction.
: Shear stress on the plane perpendicular to the x-direction and acting in the z-direction.

Note : Sign Convention
Compressive stresses are considered positive, as they are most common in soil mechanics. The sign convention for shear stresses is shown in the figure below .

For two perpendicular planes, the normal and shear stresses on any other plane can be related to the stresses on the perpendicular planes as follows:

From equilibrium conditions, the following equations are derived:
Where A in the surface of the inclined face.
If the planes perpendicular to the x and y directions are principal planes (zero shear stress), the equations simplify to:
Where and are the major and minor principal stresses, respectively.
These equations yield the relationship:
This is the equation of a circle (Mohr's Circle[1]) with center at (,0) and radius
An example of Mohr's Circle for a triaxial test at failure is shown in the figure below
