Throughout this file, amplitude is A and initial phase is ϕ0Corresponding to the data Booklet notation x0 and Φ.
Fundamental Principles
Simple Harmonic Motion (SHM) is a periodic oscillation about a stable equilibrium position, Characterized by a restoring force F directly proportional to the displacement x from Equilibrium and directed oppositely to the displacement. This yields Newton’s second law:
\begin`\{aligned}` F \propto -x \\ F_{\mathrm{net}} = -kx = m \frac{d^2x}{dt^2}, \end`\{aligned}`
Where k>0 is the stiffness constant (e.g., spring constant). Rearranged as the equation of Motion:
dt2d2x+ω2x=0,ω=mk.(1)
Here, ω is the angular frequency (rad s−1), governing the system’s temporal evolution.
Key Characteristics:
Equilibrium Position: Point where net force vanishes (Fnet=0).
Amplitude (A): Maximum displacement from equilibrium (∣x∣max=A).
Isochrony: Period T is amplitude-independent for ideal SHM.
Conditions for Ideal SHM:
Restoring force obeys Hooke’s law: F=−kx.
Zero dissipative forces (undamped motion).
Constant total mechanical energy.
Kinematic Relations
The general solution to Equation (1) is:
X(t)=Acos(ωt+ϕ0),(2)
Where ϕ0 is the initial phase angle. Velocity v and acceleration a follow by Differentiation:
V(t) = \frac`\{dx}``\{dt}` = -\omega A \sin(\omega t + \phi_0), \tag{3}A(t)=dt2d2x=−ω2Acos(ωt+ϕ0)=−ω2x.(4)
Phase Relationships:
Displacement-Velocity: v=±ωA2−x2 (from energy conservation).
Displacement-Acceleration: a=−ω2x (definitive property of SHM).
Extrema:
∣v∣max=ωA at x=0 (equilibrium).
∣a∣max=ω2A at x=±A (max displacement).
Graphical Interpretation:
x(t), v(t)And a(t) are phase-shifted sinusoids.
a(t) is inverted relative to x(t) due to a∝−x.
Energy Conservation
Total mechanical energy Etotal is conserved:
Etotal=K+U=21mv2+21kx2.(5)
Substituting Equations (2)—(4) yields: Kinetic Energy (K):
K=21mω2A2sin2(ωt+ϕ0)=21mω2(A2−x2).(6)
Potential Energy (U):
U=21kx2=21mω2x2.(7)
Total Energy:
Etotal=21kA2=21mω2A2.(8)
Energy Oscillations:
Kmax=Etotal at x=0.
Umax=Etotal at x=±A.
Example Systems
Simple Pendulum
Description: Point mass m suspended on a massless string of length L in gravitational field g. Equation of Motion: For small θ (sinθ≈θ):
dt2d2θ+Lgθ=0.(9)
This matches Equation (1) with ω=g/L. Period:
T=ω2π=2πgL.(10)
Properties:
T∝L; T∝1/g; independent of m and A (for θ≪1 rad).
Mass-Spring System
Masses and Springs
Explore how mass, spring stiffness, and damping affect oscillations. Hang different masses from Springs and observe how the period and amplitude change in real time.
Description: Mass m attached to a spring of stiffness k. Equation of Motion: From Hooke’s law:
Mdt2d2x=−kx⟹dt2d2x+mkx=0.(11)
Period:
T=2πkm.(12)
Properties:
T∝m; T∝1/k; independent of A.
Angular Frequency and Phase
Angular Frequency (ω):
ω=2πf=T2π,(13)
Where f is linear frequency (Hz). Converts temporal periodicity to angular speed.
Phase Angle (ϕ): Generalizes Equation (2):
X(t)=Acos(ωt+ϕ0).
Phase Difference (Δϕ): Temporal shift between two SHMs: Δϕ=ωΔt=T2πΔt.(14)
Measured in radians (1 rad ≈ 57.3°).
Summary of Key Equations
Quantity
Expression
Displacement
x=Acos(ωt+ϕ0)
Velocity
v=−ωAsin(ωt+ϕ0)
Acceleration
a=−ω2x
Angular Frequency
ω=k/m (spring), ω=g/L (pendulum)
Period
T=2π/ω
Kinetic Energy
K=21mω2(A2−x2)
Potential Energy
U=21mω2x2
Total Energy
Etotal=21mω2A2
Derivation of the SHM Solution
Verification by Direct Substitution
Claim:x(t)=Acos(ωt+ϕ0) satisfies dt2d2x+ω2x=0 for any Constants A, ωAnd ϕ0.
Proof. First derivative:
\frac`\{dx}``\{dt}` = -\omega A \sin(\omega t + \phi_0)
Second derivative:
dt2d2x=−ω2Acos(ωt+ϕ0)=−ω2x
Substituting into the equation of motion:
dt2d2x+ω2x=−ω2x+ω2x=0■
Sine Form Equivalence
Claim:x(t)=Asin(ωt+ϕ0) is equally valid as a general solution.
Using the identity sinθ=cos(θ−2π):
Asin(ωt+ϕ0)=Acos(ωt+ϕ0−2π)
This is the cosine form with a shifted phase. Since ϕ0 is already an arbitrary constant, Absorbing a constant offset of −π/2 does not reduce generality. Both forms span the full Two-parameter solution space (A,ϕ0).
Direct substitution confirms:
dt2d2[Asin(ωt+ϕ0)]=−ω2Asin(ωt+ϕ0)=−ω2x■
Choosing Sine vs Cosine
The two forms are physically equivalent; the choice is a matter of convenience based on initial Conditions.
Initial condition
Preferred form
Rationale
Released from x=A with v=0
x=Acos(ωt)
cos(0)=1, sin(0)=0
Released from x=0 with v=vmax
x=Asin(ωt)
sin(0)=0, cos(0)=1
General initial state
Either with appropriate ϕ0
Phase angle absorbs the offset
The IB data booklet uses the sine convention (x=x0sin(ωt+Φ)). Both conventions are Correct. Pick one and remain consistent within a single problem. Switching conventions mid-problem Introduces a systematic phase error of ±π/2.
Worked Examples — SL Level
Example 1: Period and Frequency of a Mass-Spring System
A spring of stiffness k=200N/m has a 0.50kg mass attached. Find the period T and frequency f.
A simple pendulum on Earth has a period of 2.00s. Determine its length. Use g=9.81m/s2.
L=4π2gT2=4π2(9.81)(2.00)2=39.539.2=0.993m
This is close to 1.00mWhich is why a “seconds pendulum” (T=2s) is Approximately 1m long on Earth.
Example 5: Phase Difference Between Two Oscillators
Two identical mass-spring systems oscillate with the same amplitude and frequency. System A is Released from maximum displacement at t=0. System B is released from equilibrium, moving in the Positive direction, at t=0. Find the phase difference Δϕ.
System A (cosine form): xA=Acos(ωt)
System B (starts at x=0 with positive velocity, sine form): xB=Asin(ωt)=Acos(ωt−2π)