Why metals don't break just by being squeezed from all sides
In short: If you squeeze a block of metal equally from every direction, it won't permanently deform. This counterintuitive reality is the foundation of the von Mises yield criterion, a mathematical rule that predicts exactly when a material will transition from elastic stretching to permanent plastic flow.
In materials science, a yield criterion defines the boundary where a material stops behaving elastically and begins to deform plastically. For ductile metals, this behavior is governed by the 'hydrostatic' and 'deviatoric' components of stress. Experimental evidence shows that hydrostatic stress—where pressure is applied equally in all directions (σ1 = σ2 = σ3)—does not induce plastic deformation. Because of this, the yield surface in 3D stress space is not a sphere, but a cylinder centered around the 'hydrostatic line.'
Yielding happens once the second invariant of deviatoric stress hits a critical threshold, according to the von Mises criterion (maximum distortion energy criterion). Mathematically, it is expressed as a constant relationship between principal stresses: (σ1 - σ2)² + (σ2 - σ3)² + (σ3 - σ1)² = constant. For a material with a uniaxial yield stress (Y), this constant is 2Y². This geometry creates a circular yield surface when viewed down the hydrostatic axis, representing the energy required to distort the material's shape rather than just change its volume.
While the von Mises criterion provides a more accurate fit for observed physical behavior than the simpler, hexagonal Tresca criterion, the latter is still frequently used due to its mathematical ease. The relationship between the two is precise: in pure shear, the shear yield stress (k) is exactly 1/√3 times the tensile yield stress (Y). This distinction is vital for engineers who must predict how complex, multi-axial loads will affect structural integrity based on simple, one-dimensional laboratory tests.
The history of this theory is a collaborative evolution of thought. While often associated with Richard Edler von Mises, who rigorously formulated it in 1913, the concept was anticipated by Tytus Maksymilian Huber in 1904 and independently formulated by Heinrich Hencky in 1924. It is also linked to James Clerk Maxwell's 1865 descriptions, leading many to refer to it as the Maxwell–Huber–Hencky–von Mises theory.
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Sources
- Summary by Intellect · source: Yield criteria for metals
- Also: Von Mises yield criterion
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