Animated Solution for Physics - Gravitation: A particle of mass m, and angular momentum ℓ is moving in a circular orbit of radius r0 under the influence of an attractive force F(r)=−r2kr^. Keeping its angular momentum unchanged, the particle is displaced radially by a small distance δr≪r0, due to which its radial distance varies periodically. The corresponding time period is:
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Visualized Solution
Initial Setup & Force F(r)
F(r)=−r2kr^
Angular momentum ℓ is constant.
Equilibrium Condition
Fattractive=Fcentrifugal
r02k=r0mv02
ℓ=mv0r0⟹v0=mr0ℓ
Calculating Radius r0
r02k=r0m(mr0ℓ)2
r02k=mr03ℓ2
r0=mkℓ2
Effective Force Feff
Let r=r0+x where x≪r0
Feff=Fcentrifugal−Fattractive
Feff=mr3ℓ2−r2k
Binomial Approximation
Feff=m(r0+x)3ℓ2−(r0+x)2k
Feff=mr03ℓ2(1+r0x)−3−r02k(1+r0x)−2
Feff≈mr03ℓ2(1−r03x)−r02k(1−r02x)
Restoring Force & SHM
Since mr03ℓ2=r02k
Feff≈r02k(1−r03x−1+r02x)
Feff≈−r03kx
This is SHM with Keff=r03k
Time Period T
T=2πKeffm=2πkmr03
T=2πkm(mkℓ2)3
T=mk22πℓ3
Conclusion
The particle oscillates radially while revolving, creating a rosette-like orbit.
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The Sigma Insight: Orbital Motion of a Satellite
Solution Diagram
Analyzing the Setup
Imagine a particle gracefully moving in a perfect circular orbit. The only reason it maintains this path is because a central attractive force is constantly pulling it inward, acting as an invisible tether.
The force given is F(r)=−r2kr^. This is an inverse-square law force, much like gravity or electrostatics.
The Master Equation for Equilibrium
For the particle to stay in this stable circular orbit of radius r0, the inward attractive force must perfectly balance the outward centrifugal tendency.
In a rotating frame of reference, we can express this balance as:
r02k=r0mv02
We are told that the angular momentum ℓ remains unchanged. We know that ℓ=mv0r0, which gives us v0=mr0ℓ.
Substituting this into our force balance equation:
r02k=r0m(mr0ℓ)2=mr03ℓ2
From this, we can isolate the equilibrium radius r0:
r0=mkℓ2
Introducing the Disturbance
Here is where the physics gets really interesting. We introduce a tiny radial disturbance, nudging the particle slightly away from its perfect circle to a new radius r=r0+x, where x≪r0.
Because it is a stable equilibrium, it will try to return, creating an oscillation. To analyze this wobble, we calculate the net effective force at this new radius.
The effective radial force is the difference between the centrifugal force and the attractive force:
Feff=mr3ℓ2−r2k
The Mathematics of the Wobble
Let's substitute r=r0+x into our effective force equation:
Feff=m(r0+x)3ℓ2−(r0+x)2k
Since the displacement x is very small, we can factor out r0 and use the binomial approximation (1+ϵ)n≈1+nϵ:
Feff=mr03ℓ2(1+r0x)−3−r02k(1+r0x)−2
Feff≈mr03ℓ2(1−r03x)−r02k(1−r02x)
Recall our equilibrium condition: mr03ℓ2=r02k. We can substitute this into the first term:
Feff≈r02k(1−r03x−1+r02x)
Feff≈−r03kx
Look at the structure of this resulting force! It is directly proportional to the displacement x, and it acts in the opposite direction. This is the undeniable signature of Simple Harmonic Motion.
Final Calculation
Our effective spring constant is Keff=r03k.
Now, we simply plug it into the classic time period formula for SHM:
T=2πKeffm=2πkmr03
Finally, we substitute our earlier expression for the stable radius r0=mkℓ2:
T=2πkm(mkℓ2)3=2πm2k4ℓ6
The algebra elegantly collapses into our final answer:
T=mk22πℓ3
This explains why planets do not just crash or escape when slightly nudged by the gravity of other celestial bodies!