Linear Elasticity Equations
Summary of the Equations of Linear Elasticity
The stiffness matrix of linear elastic isotropic material contains two parameters:
E, Young's modulus (elastic modulus)
ν, Poisson’s ratio
Define the following quantities.
The equilibrium equation is
The linearized, small-displacement strain-displacement relationship is
The balance of angular momentum states that stress is symmetric:
The Voigt notation for the constitutive equation of the linear isotropic model is
The expanded form uses all the entries in σ and ε takes symmetry into account.
(1) |
In the preceding diagram, • means the entry is symmetric.
3D Linear Elasticity Problem
The toolbox form for the equation is
But the equations in the summary do not have ∇u alone, it appears together with its transpose:
It is a straightforward exercise to convert this equation for strain ε to ∇u. In column vector form,
Therefore, you can write the strain-displacement equation as
where A stands for the displayed matrix. So rewriting Equation 1, and recalling that • means an entry is symmetric, you can write the stiffness tensor as
Make the definitions
and the equation becomes
If you are solving a 3-D linear elasticity problem by using
PDEModel
instead of StructuralModel
, use the
elasticityC3D(E,nu)
function (included in your software) to
obtain the c
coefficient. This function uses the linearized,
small-displacement assumption for an isotropic material. For examples that use this
function, see StationaryResults
.
Plane Stress
Plane stress is a condition that prevails in a flat plate in the x-y plane, loaded only in its own plane and without z-direction restraint. For plane stress, σ13 = σ23 = σ31 = σ32 = σ33 = 0. Assuming isotropic conditions, the Hooke's law for plane stress gives the following strain-stress relation:
Inverting this equation, obtain the stress-strain relation:
Convert the equation for strain ε to ∇u.
Now you can rewrite the stiffness matrix as
Plane Strain
Plane strain is a deformation state where there are no displacements in the z-direction, and the displacements in the x- and y-directions are functions of x and y but not z. The stress-strain relation is only slightly different from the plane stress case, and the same set of material parameters is used.
For plane strain, ε13 = ε23 = ε31 = ε32 = ε33 = 0. Assuming isotropic conditions, the stress-strain relation can be written as follows:
Convert the equation for strain ε to ∇u.
Now you can rewrite the stiffness matrix as
Axisymmetric Analysis
Axisymmetric analysis speeds up simulations by simplifying 3-D solids using their symmetry around the axis of rotation and analyzing only the 2-D axisymmetric section. Use polar coordinates r,θ,z for radial, circumferential, and axial directions. If z is the axis of rotation, the symmetry around the z-axis means that the stress components are independent of the θ coordinate. The stress equilibrium equations for an axisymmetric structural mechanics are as follows:
τ is the shear stress, and γ is the shear strain. Assuming isotropic conditions, the stress-strain relation can be written as follows: