We can express all the equations in terms of the displacement field. Its primary advantage is that it combines the three sets of governing equations (equilibrium, kinematics, and constitutive) into a single vector equation, reducing the problem from 15 unknowns (stress, strain, displacement) to just 3 (the components of the displacement vector
The derivation involves a systematic substitution, starting with the equilibrium equation and progressively replacing stress with strain, and then strain with displacement.
We begin with the three fundamental sets of equations in index notation.
1. Equilibrium Equation (Equation of Motion): This equation relates the divergence of the stress tensor to body forces and inertia.
Alternative form:
2. Constitutive Law (Generalized Hooke’s Law for Isotropic Materials): This law relates stress to strain using the two Lamé parameters,
Altenative form:
3. Kinematic (Strain-Displacement) Relation: This equation defines strain in terms of displacement gradients for small deformations.
Step A: Express Stress in terms of Displacement First, substitute the kinematic relation (3) into the constitutive law (2).
Alternative form: First, note that the trace of the strain tensor is the divergence of the displacement vector:
Step B: Substitute Stress into the Equilibrium Equation Now, substitute this expression for stress (4) into the equilibrium equation (1). Since the stress tensor is symmetric (
Combining these terms gives:
This is the Lamé-Navier equation in index notation.
Alternative form:
Now, take the divergence of the stress expression (4’) and substitute it into the equilibrium equation (1’):
Applying these identities to our equation (assuming constant
Boundary Conditions in Terms of Displacement
The boundary conditions that we discussed in the previous section