What is the Angular Frequency of Small Oscillations on a Nonuniform Disk?

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SUMMARY

The discussion focuses on calculating the angular frequency of small oscillations for a nonuniform disk with a center of mass offset from its geometric center. The relevant equations include the Parallel Axis Theorem, the kinetic energy of a rotating object, and the Lagrangian formulation. The derived angular frequency formula is ω = √((g*a)/(2A² + (1/2)*R²)), where 'g' is the acceleration due to gravity, 'a' is the distance from the pivot to the center of mass, 'A' is the distance from the geometric center to the center of mass, and 'R' is the radius of the disk. The discussion also references alternative forms of the Lagrangian and angular frequency derived from the problem statement.

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GleefulNihilism
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Well, I had a couple problems on my final I was hoping to go over- hope nobody minds. Here's the second.

Homework Statement


A nonuniform disk of radius R and mass m has the center of mass at a distance A from the geometrical center. Its moment of inertia about the axis passing through the center of mass and perpendicular to it's plane is I. Assuming that the cylinder rolls without sliding, find the angular frequency of small oscillations about a position of stable equilibruim on a horizontal plane.


Homework Equations


Parallel Axis Theorem
I = i + mr^2, where i is the moment of inertia through the geometrical center.

Kinetic Energy of A Rotating Object
T = T(translational) + T(rotational)
= (m/2)*(x'^2 + y'^2) + (1/2)*I*omega^2

Lagrangian
L = T - U
And
d( dL/dq' ) / dt - dL/dq = 0, where ' is short hand for the time derivative.

Small Angle Approximation
cos(phi) is about equal to 1 - (1/2)*(phi)^2

The Attempt at a Solution



First, we put the pieces of the Lagrangian together.

U = Potential Energy, in this case we only worry about Gravitational. Basing it off of the center of mass of the cylinder I got this.

U = m*g*(R - A*cos(phi)) where phi is the angle of the center of mass of the disk to the center of the disk to the vertical axis.

T(rotational) = (1/2)*I*phi'^2.

By parallel-axis theorem I = (mR^2)/2 + mA^2

so T(rotational) = (m/2)*((R^2)/2 + A^2)*phi'^2.

And T(translational) = (m/2)*(x'^2 + y'^2)

x = D + A*sin(phi) where D is displacement from the origin in x.
y = R - A*cos(phi)

So x' = A*phi'*cos(phi) and y' = A*phi'*sin(phi)

Which gives T(translational) = (m/2)*((A*phi'*cos(phi))^2 + (A*phi'*sin(phi))^2)
Which simplifies to T(translational) = (m/2)*A^2*phi'^2


Thus L = (m/2)*A^2*phi'^2 + (m/2)*((R^2)/2 + A^2)*phi'^2 - m*g*(R - A*cos(phi))

We limit ourselves to small oscillations so. . .

L = (m/2)*((R^2)/2 + 2A^2)*phi'^2 - m*g*(R - A*(1 - (1/2)*phi^2))

Thus dL/d(phi') = m*(2A^2 + (R^2)/2)*phi' so d( dL/dq' ) / dt = m*(2A^2 + (R^2)/2)*phi''

And dL/d(phi) = -m*g*A*phi

So, phi'' + (g*a)/(2A^2 + (1/2)*R^2) * phi = 0

and omega = sqrt((g*a)/(2A^2 + (1/2)*R^2)) from the characteristic equation of such a lagrangian.
 
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Still no bites?

Well, if it helps I just want to see how the professor got this.

A.) L = (1/2)*[m*(R^2 + A^2 - 2AR*cos(phi)) + I]*phi'^2 + m*g*A*cos(phi)

B.) omega = sqrt( (m*g*A) / ( m*(R-A)^2 + I) )
 

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