Finite Element: Q8 Quadrilaterals
Last updated August 30, 2023
By Ian Story
The following are notes that may be helpful when implementing the stiffness matrix for a Q8 quadrilateral. These notes supplement the following YouTube lectures by Dr. Clayton Pettit:
Finite Element Method: Quadrilateral Elements
Finite Element Method: Isoparametric Elements
Shape Functions
Throughout this derivation, we will use the following shape functions:
To simplify display in matrices, the function arguments are omitted in the following derivation. Just remember that everywhere appears, it actually means , a function that must be evaluated at every point in the natural coordinate system.
Coordinate Mapping
Jacobian Matrix
Where:
The partial derivative for y and partial derivatives with respect to are identical to the above: just swap out the relevant symbols.
Making use of the matrix, presented below, the Jacobian matrix can be expressed as follows:
N Matrix
To simplify further calculations, we can define a N matrix as follows:
Where:
B Matrix Derivation
Where (by multivariable chain rule):
Or, in matrix form:
Conveniently, the first matrix can be simplified based on existing information, because:
Because and are just the nodal displacements at and , the same coordinate mapping applies here:
Therefore:
Replacing the nodal displacements with a vector, ,
This 4×16 matrix is just the matrix with zero columns inserted between each column, repeated and offset by one column. Therefore, let us define:
Putting all the pieces together gives
By the definition of the kinematic matrix ()
Which implies
C Matrix
Under plane stress,
By the definition of the constitutive matrix ():
Therefore,
Element Stiffness Matrix
This integral can be simplified by using Gauss Integration (recommended n=3 for balance between performance and accuracy – this requires sampling the element at 9 points)
Tutorial: Dr. Clayton Pettit on Gaussian Integration
Post Processing
Once nodal deflections are known, the strains and stresses can be determined at any point on the element:
Note that it is not easy to convert from the local/global coordinate systems to the natural coordinate system. Because all of the shape functions depend on inputs of and , working backwards requires a trial and error process until the guesses match the desired x, y outputs.
Therefore, it is more typical to calculate stresses in the natural coordinate system at regular intervals and place these at their corresponding places in the local coordinate system.
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