Lecture 8 - Rotational motion and moments of inertia#

In Lecture 7 we considered the forces acting on a circular system. What you will find, if you haven’t spotted it already, is that there is generally a rotational counterpart to all of the linear topics we have studied so far. Last time we looked at forces and in this chapter we are going to consider the kinematic equations for a rotating system, before moving on to consider how we need to rethink mass for rotating objects.

Rotational motion for constant angular acceleration systems#

We are going to only consider rotating systems that have a constant angular acceleration \(\alpha_0\). If our angular acceleration is constant then

\[\begin{align*} \alpha(t) &= \alpha_0 \end{align*}\]

but we can also make use of the definition that the angular acceleration is the rate of change of angular velocity \(\omega\), thus

\[\begin{align*} \frac{\mathrm{d}\omega}{\mathrm{d}t} &= \alpha_0\\ \int_0^t \frac{\mathrm{d}\omega}{\mathrm{d}t}\mathrm{d}t &= \int_0^t\alpha_0 \, \mathrm{d}t\\ \therefore \omega(t) &= \alpha t + c_1 \end{align*}\]

We can substitute in \(t=0\) to find this constant of integration because \(\omega(t=0)\) is simply the initial angular velocity \(\omega_0\), so \(c_1 = \omega_0\). Therefore

(50)#\[\omega(t) = \alpha_0 t + \omega_o\]

Take a moment to look at this expression. It looks remarkably similar to the constant acceleration kinematic equations for a linear system, in this case the \(v(t) = at + v_0\) equation. Swap linear velocities \(v\) for angular velocities \(\omega\), and do the same for accelerations \(a\) to \(\alpha\), and you can easily remember one set if you remember the other set.

For completeness though we will actually derive the kinematic equation for angular displacement. Starting from equation (50) and noting that the angular velocity is the rate of change of angle we can show

\[\begin{align*} \frac{\mathrm{d}\theta}{\mathrm{d}t} &= \alpha_0 t + \omega_0\\ \int_0^t \frac{\mathrm{d}\theta}{\mathrm{d}t}\mathrm{d}t &= \int_0^t \alpha_0 t + \omega_0\,\mathrm{d}t\\ \therefore \theta(t) &= \frac{\alpha_0 t^2}{2} + \omega_0 t + c_2 \end{align*}\]

Once again we make use of the initial conditions that for when \(t=0\) we have the initial displacement \(\theta(t=0)=\theta_0\) so putting these into the equation above means that \(c_2 = \theta_0\). So finally we find

\[\begin{align*} \theta(t) &= \frac{\alpha_0t^2}{2}+\omega_0t+\theta_0 \end{align*}\]

You should hopefully be able to see the similarites between this equation and the linear kinematic equation counterpart (\(x(t) = \frac{at^2}{2}+v_0t+x_0)\).

Using these kinematic equations is very similar to the linear version. You will get more practice of these in the tutorials and homeworks but you can find other practice questions in any undergraduate physics textbook.

Energy of a rotating body#

A logical next step will be to consider the total kinetic energy of a rotating body, firstly by examining an individual particle moving on a circular path but then developing this idea to an extended solid body rotating about some axis.

For the individual particle case we use our standard equation for the kinetic energy but note that the velocity is the tangential velocity. A justification for this is that if the centripetal force were to suddenly vanish the particle would move off in a straight line at the tengential velocity and therefore would have kinetic energy \(\frac{1}{1}mv_t^2\). However we now have an relationship between the tangential and angular velocities which allows us to define the kinetic energy of an individual particle moving in a circular path of radius \(r_i\) as

\[\begin{align*} KE_i = \frac{m_iv_i^2}{2} &= \frac{m_ir_i^2\omega^2}{2} \end{align*}\]

where the subscripts \(i\) indicate an individual particle, notation that will become very useful shortly.

Let us now move on to the extended solid body case. The way we treat this system is by breaking the single solid body down into the sum of individual particles all rotating about a common axis. It then follows that the total kinetic energy of the solid body is equal to the sum of the kinetic energies of these individual particles.

In Fig. 22 I have picked out two specific particles, labelled with subscripts 1 and 2, to highlight the differences. Particle 1 of mass \(m_1\) follows a circular path of radius \(r_1\) and has tangential velocity \(v_1\) whereas particle two has different mass \(m_2\), radius \(r_2\) and tangential velocity \(v_2\). What they do have in common is the angular velocity \(\omega\) - the angular velocity must be the same for all particles that make up the solid body if the body were to remain in the same shape and not skew or distort. You’ll also note that I have not made the assumption here that the masses of each particle are the same. This allows me to be more general in the subsequent treatments for bodies that have non-uniform densities, although in practice we will usually stick to the uniform case when solving problems in this course.

A randomly shaped blob rotating about some axis. This mass is split into small pieces, each of which have their own distance from the axis of rotation and tangential velocity. All mass pieces are moving with the same angular velocity.

Fig. 22 A randomly shaped blob rotating about some axis. This mass is split into small pieces, each of which have their own distance from the axis of rotation and tangential velocity. All mass pieces are moving with the same angular velocity.#

The total kinetic energy \(KE_T\) of the solid body is the sum of the individual kinetic energies of the particles, and so

\[\begin{align*} KE_T &= \sum_i\frac{m_ir_i^2\omega^2}{2}\\ &= \frac{\omega^2}{2}\sum_im_ir_i^2\\ &=\frac{I\omega^2}{2} \end{align*}\]

where \(I\) is the moment of inertia defined by \(\sum_im_ir_i^2\). Note that this equation for the total kinetic energy is similar to the equation for our linear systems \(\left(\frac{mv^2}{2}\right)\) where \(\omega\) is the rotational counterpart to \(v\) and \(I\) is therefore the counterpart to \(m\). But what exactly is the moment of inertia? Why does the “mass like” term in the kinetic energy of a rotating body have units of mass \(\times\) length\(^2\)?

Moment of inertia#

Note

This topic is historically the one that students find the most difficult of the entire Mechanics course. So if you do not understand it immediately, don’t worry. It is something that makes more sense when you re-read it a few times in conjunction with working through some derivations and practice questions.

To get an understanding of what moment of inertia is I want to return to our old friend Newton’s Second Law but to reframe what it means. Taking the simple case where the mass remains constant, i.e. we use \(F=ma\) then it is possible to redefine the mass as a measure of resistance to changes in linear motion. In the Second Law equation \(m\) is a constant of proportionality and if this constant is larger then a larger force is required to cause the same acceleration (hence being a measure of resistance).

The moment of inertia is the rotational analogue; it is the resistance to changes in rotational motion.

There is a key difference between mass and moment of inertia. The mass of an object is intrinsic to it, and when we want to accelerate a body of mass \(m\) along a straight line it does not matter how this mass is distributed. The same is not true for a rotating body. The resistance to changing the rotational motion of a body depends not only on how much mass the body has but how this mass is distributed with respect to the axis of rotation. We will explore this further in a couple of worked examples below and some in your tutorials, but table 9.2 in the core textbook shows the range of geometries we will consider in this course.

Before we embark on some worked examples we need to make one final adjustment to our definition of the moment of inertia. In the definition above we are taking a simple summation of discrete particles of equal mass \(\Delta m\) but it is more useful to take the limit of this as the masses tend to \(0\)

(51)#\[\begin{split}I &= \lim\limits_{\Delta m \to 0}\sum_i r_i^2\Delta m\nonumber\\ &= \int r^2\, \mathrm{d}m\end{split}\]

The general procedure for solving this integral is:

  1. Split the body up into small mass elements \(\mathrm{d}m\)

  2. Change \(\mathrm{d}m\) into a distance element, assuming the body has a uniform density.

  3. Integrate equation (51) over this substituted distance element, noting that the limits should cover the whole length of the body with respect to the axis of rotation.

In some cases we can deviate from this general procedure but this is very much dependent on the geometry of the system.

Important

All moment of inertias will be of the form \(cMR^2\) or \(cML^2\), i.e mass times distance squared, with some numerical prefactor \(c\) that depends on the geometry of the system and the location of the axis of rotation.

Using symmetry#

All of the examples we have considered so far have been solved by adding up the moment of inertia contributions from small point masses across the whole extended shape we are interested in. In other words

(53)#\[I = \int\mathrm{d}I\]

This may seem a silly statement to make but it does allow us to leverage symmetry to make the process easier for certain shapes. If it is possible to construct one shape out of an infinite number of another shape for which we know the moment of inertia expression, then we can use (53) with the moment of inertia for these “infinite shapes” on the right hand side.

This is a lot clearer by going through two more examples, the solid disc and the solid sphere.

Axis theorems for moments of inertia#

In the real world we often want to calculate the moment of inertia for a body about an axis that does not lend itself to a nice symmetry of mass distribution. You will see this in one of the tutorial questions where we examine in great depth the opening of a swing bin lid.

There are two theorems that come to our aid, the parallel axis theorem and the perpendicular axis theorem. These are extremely useful as they allow us to translate from rotation about one axis to another axis so long as the new one is either parallel or perpendicular to the first axis. In practice this means we often start with one of the nice symmetric systems and shift our axes to suit.

For example if we wanted to calculate the moment of inertia of a hula hoop being spun around on your wrist then we can start with the moment of inertia for the hoop through the centre of mass (i.e. the centre of the hoop) and shift the axis by a distance equal to the radius of the hoop.

You are able to prove these theorems fairly easily but for the purpose of this course you will not be expected to remember the proofs. The results are worth remembering but knowing how to derive them can be helpful in a pinch if you cannot remember the final equations.

Paralled axis theorem#

The moment of inertia about a parallel axis some distance \(D\) away from the centre of mass axis is

(54)#\[\begin{align} I &= I_{\text{CM}} + MD^2 \end{align}\]

Perpendicular axis theorem#

If the moments of inertia about the \(x\) and \(y\) axis are known then the moment of inertia about \(z\) is

\[\begin{align*} I_z &= I_x + I_y \end{align*}\]

Note that my choice of \(x\), \(y\) and \(z\) is arbitrary. \(I_x = I_y + I_z\) is equally valid. The important point is that the three axes involved are perpendicular to each other.

Lecture Questions#