The beauty of Simple Harmonic Motion (SHM) lies in its predictability. If you know where a particle starts and how it moves in the first few moments, you can mathematically decode its entire future and past. This problem is a classic example of using initial conditions and kinematic data to reverse-engineer the core parameters of the motion: the amplitude and the time period.
Analyzing the Setup
The problem states that the particle starts from rest. In the realm of SHM, a particle only comes to rest at its extreme positions. Therefore, at time t=0, the particle is at an extreme position, which we can denote as x=A (where A is the amplitude).
Because the motion starts from the extreme position, the most natural equation to describe its position
x at any time
t is the cosine function:
x=Acosωt
Here, x is the displacement from the mean position, and ω is the angular frequency.
Translating Physics into Math
The problem gives us two critical pieces of information about the distances traveled:
1.
In the first τ seconds: The particle travels a distance
a. Since it started at
x=A and is moving towards the mean position, its new coordinate is
x=A−a. Substituting this into our SHM equation yields:
A−a=Acosωτ…(1)
2.
In the next τ seconds: The particle travels an additional distance of
2a in the same direction. This means the total time elapsed is
2τ, and the total distance traveled from the start is
a+2a=3a. Its new coordinate is
x=A−3a. Substituting this gives:
A−3a=Acos2ωτ…(2)
The Mathematical Interlude
We now have a system of two equations with two unknowns (
A and
ω). The challenge is that the angular terms are
ωτ and
2ωτ. To bridge this gap, we must call upon a fundamental trigonometric identity—the double angle formula for cosine:
cos2θ=2cos2θ−1
Applying this to our equations, we can express
cos2ωτ in terms of
cosωτ:
AA−3a=2(AA−a)2−1
Algebraic Execution
Now, we roll up our sleeves and execute the algebra. Let's expand the squared term on the right side:
AA−3a=A22(A2+a2−2Aa)−1
Taking the common denominator on the right side:
AA−3a=A22A2+2a2−4Aa−A2
AA−3a=A2A2+2a2−4Aa
We can cancel one
A from the denominators (since
$A
eq 0$) and cross-multiply the remaining
A to the left side:
A(A−3a)=A2+2a2−4Aa
A2−3aA=A2+2a2−4Aa
The
A2 terms beautifully cancel out, leaving us with a simple linear relationship between
A and
a:
4Aa−3aA=2a2
aA=2a2
Since the distance
a is non-zero, we can divide by
a to find the amplitude:
A=2a
The Final Stretch
With the amplitude
A known, finding the time period
T is straightforward. We substitute
A=2a back into our first equation:
2a−a=2acosωτ
a=2acosωτ
cosωτ=21
The principal angle whose cosine is
1/2 is
π/3 radians. Therefore:
ωτ=3π
We know that the angular frequency
ω is related to the time period
T by the equation
ω=T2π. Substituting this in:
T2πτ=3π
Solving for
T, the
π terms cancel out, and we get:
T=6τ
This elegant result tells us that the total time period of the oscillation is exactly six times the duration of that first interval. The physics perfectly aligns with the math!