Introduction to the Model
Description and Assumptions
This model applies to position of a single point particle, or to the angular position of a rigid body, which is constrained to one dimension and experiences a restoring force that is linearly proportional to its displacement from an equilibrium position. This form for the force or torque implies that the equation of motion for the point particle or rigid body will have the form:
\begin
[ a = \frac{d^
x}{dt^{2}} = - \omega_
^
x ]\end
or
\begin
[ \alpha = \frac{d^
\theta}{dt^{2}} = -\omega_
^
\theta] \end
.
As a consequence of this characteristic equation, the position, velocity, and acceleration (or the angular equivalents) will each be sinusoidal functions of time. Simple harmonic motion is sometimes abbreviated SHM, or referred to as "Simple Harmonic Oscillation" (SHO).
Learning Objectives
Students will be assumed to understand this model who can:
- Define the terms equilibrium position and restoring force.
- Define the amplitude, period, natural angular frequency and phase of oscillatory motion.
- Give a formula for the natural angular frequency of the oscillation of a pendulum or mass on a spring.
- Write mathematical expressions for the position, velocity and acceleration of Simple Harmonic Motion as functions of time for the special cases that the initial velocity is zero or the initial position is equilibrium.
- Graphically represent the position, velocity and acceleration of Simple Harmonic Motion.
- Use the laws of dynamics to determine the natural angular frequency of a system in the limit of very small displacements from equilibrium.
- Describe the consequences of conservation of mechanical energy for Simple Harmonic Motion (assuming no dissipation).
S.I.M. Structure of the Model
Compatible Systems
A single point particle (or, for the angular version of SHM, a single rigid body).
Relevant Interactions
The system must be subject to a one-dimensional restoring force (or torque) that varies linearly with the displacement (or angular displacement) from a stable equilibrium position.
Relevant Definitions
\begin
[ A = \sqrt{x_
^
+ \left(\frac{v_{i}}{\omega_{0}}\right)^{2}} ]\end
\begin
[ \phi = \cos^{-1}\left(\frac{x_{i}}
\right) = \sin^{-1}\left(\frac{v_{i}}{\omega_
A}\right)]\end
Laws of Change
Mathematical Representation
\begin
[ x(t) = x_
\cos(\omega_
(t-t_
)) + \frac{v_{i}}{\omega_{0}}\sin(\omega_
(t-t_
))]\end
\begin
[ v(t) = -\omega_
x_
\sin(\omega_
(t-t_
)) + v_
\cos(\omega_
(t-t_
))]\end
\begin
[ a(t) = -\omega_
^
x_
\cos(\omega_
(t-t_
)) - \omega_
v_
\sin(\omega_
(t-t_
)) = -\omega_
^
x(t) ]\end
\begin
[ x(t) = A\cos(\omega_
t + \phi)]\end
\begin
[ v(t) =-A\omega_
\sin(\omega_
t + \phi)]\end
\begin
[ a(t) =-\omega_
^
A\cos(\omega_
t+\phi) =-\omega_
^
x(t)]\end
Diagrammatic Representations
- position versus time graph
- [velocity versus time graph]
- [acceleration versus time graph]
Click here for a Mathematica Player application \\ illustrating these representations using phase. |
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