Introduction to Elasticity/Spinning disk
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[edit] Thin spinning disk
[edit] Problem 1:
A thin disk of radius a is spinning about its axis with a constant angular velocity
. Find the stress field in the disk using an Airy stress function and a body force potential.
[edit] Solution:
The acceleration of a point (r,θ) on the disk is
The body force field is
Since there is no rotational acceleration, the body force can be derived from a potential V. The relations between the stresses, the Airy stress function and the body force potential are
where
From equations (2) and (6) , we have,
Integrating equation (7), we have
Substituting equation (9) into equation (8), we get
This constant can be set to zero without loss of generality. Therefore,
The spinning disk problem is a plane stress problem. Hence the compatibility condition is
where
Now, from equations (11) and (13)
Therefore, equation (12) becomes
Since the problem is axisymmetric, there can be no shear stresses, i.e. σrθ = 0 and no dependence on θ. From Michell's solution, the appropriate terms of the Airy stress function are
Axisymmetry also requires that uθ, the displacement in the θ direction must be zero. However, if we look at Mitchell's solution, we see that uθ is non-zero if the term r2ln(r) is used in the Airy stress function. Hence, we reject this term and are left with
If we plug this stress function into equation (16) we see that
. Therefore, equation (18) represents a homogeneous solution of equation (16). The
that is a general solution of equation (16) is obtained by adding a particular solution of the equation.
One such particular solution is the stress function
since the biharmonic equation must evaluate to a constant. Plugging this into equation (16) we have
or,
Therefore, the general solution is
The corresponding stresses are (from equations (3, 4, 5)),
At r = 0, the stresses must be finite. Hence, C2 = 0. At r = a, σrr = σrθ = 0. Evaluating σrr at r = a we get
Substituting back into equations (22) and (23), we get









![\begin{align}
\text{(13)} \qquad \nabla^2{()} & = \frac{\partial^2 () }{\partial r^2} + \frac{1}{r}\frac{\partial () }{\partial r} +
\frac{1}{r^2}\frac{\partial^2 ()}{\partial \theta} \\
\text{(14)} \qquad \nabla^4{()} & = \nabla^2{[\nabla^2{()}]}
\end{align}](http://upload.wikimedia.org/math/f/e/3/fe3d6015ac362c3fc0c881eb10ebf85f.png)
![\text{(15)} \qquad
\nabla^2{V} = -\rho\dot{\theta}^2[1 + 1 + 0] = -2\rho\dot{\theta}^2](http://upload.wikimedia.org/math/3/d/1/3d144d74c78d2658c6ff5f3b7778373d.png)









![\text{(27)} \qquad
\sigma_{\theta\theta} = \frac{\rho\dot{\theta}^2}{8}\left[
(3+\nu)a^2 - (1+3\nu)r^2\right]](http://upload.wikimedia.org/math/0/7/c/07c0785bb5452107eca4139b52d02754.png)
