Stress and strain#
Strain measures#
Deformation gradient tensor#
The deformation gradient tensor, \(\mathbf{F}\), is a crucial concept in finite deformation (large deformation) continuum mechanics, as it forms the basis for deriving all measures of deformation. It provides a linear mapping between an initial configuration, \(d\mathbf{X}\), to an deformed configuration, \(d\mathbf{x}\), without assuming that displacements or rotations are small. It is expressed as:
Velocity gradient tensor#
The velocity gradient tensor, \(\mathbf{L}\), quantifies the spatial rate of change of the velocity field, \(\mathbf{v}\), within the material. It captures the local rate of stretching, shearing, and rotation. \(\mathbf{L}\) is defined as the gradient of the velocity vector, and its components are given by:
Numerical integration of deformation gradient#
To numerically compute \( \mathbf{F} \) over a discrete time step \( \Delta t \), we use the forward Euler approximation for \( \dot{\mathbf{F}} \):
Substituting \( \dot{\mathbf{F}} = \mathbf{L}_p \cdot \mathbf{F}_p^t \):
Factoring \( \mathbf{F}_p^t \):
Rate of deformation tensor (strain rate tensor)#
The rate of deformation tensor, \(\mathbf{D}\), also known as the strain rate tensor, represents the symmetric part of the velocity gradient tensor, \(\mathbf{L}\). It describes the rate of change of strain in the material (rate of stretching and shearing). Mathematically, \(\mathbf{D}\) is given by:
As a 6x1 the rate of deformation tensor \(\mathbf{D} = \left[\frac{dv_x}{dx}, \frac{dv_y}{dy}, \frac{dv_z}{dz}, \frac{1}{2}(\frac{dv_x}{dy} + \frac{dv_y}{dx}), \frac{1}{2}(\frac{dv_y}{dz} + \frac{dv_z}{dy}), \frac{1}{2}(\frac{dv_x}{dz} + \frac{dv_z}{dx})\right]^T\)
Stress and Strain#
Strain increment#
Strain increments \( \Delta \boldsymbol{\varepsilon}_p \) are obtained from gradients of the nodal velocities evaluated at the material point \(\boldsymbol{p}\).
where \( \mathbf{L}_p \) is the velocity gradient.
Stress increment#
Stress increments are obtained from the strain increments. It is computed using the material’s constitutive model: