Animated Solution for Physics - Gravitation: A thin uniform annular disc (see figure) of mass M has outer radius 4R and inner radius 3R. The work required to take a unit mass from point P on its axis to infinity is
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Visualized Solution
Visualizing the Annular Disc and Point P
We are given a thin uniform annular disc of mass M, inner radius 3R, and outer radius 4R.
Point P lies on the axis of the disc at a distance of 4R from its center O.
Our goal is to find the work required to move a unit mass from point P to infinity.
Connecting Work and Gravitational Potential
The work done by an external agent in slowly moving a mass m from point P to infinity is:
W=U∞−UP
Since potential energy at infinity is zero (U∞=0):
W=−UP=−mVP
For a unit mass (m=1):
W=−VP
Calculating the Surface Mass Density
The total mass of the annular disc is M.
The area of the annular region is:
A=π(4R)2−π(3R)2=16πR2−9πR2=7πR2
Therefore, the surface mass density σ is:
σ=7πR2M
Selecting an Elemental Ring
Consider a thin concentric ring of radius r and radial width dr.
The area of this elemental ring is:
dA=2πrdr
The mass of this elemental ring is:
dM=σdA=(7πR2M)(2πrdr)=7R22Mrdr
Potential of the Elemental Ring at Point P
Every point on the elemental ring is at the same distance from point P:
s=(4R)2+r2=16R2+r2
The gravitational potential dVP at point P due to this ring is:
dVP=−sGdM=−16R2+r2GdM
Setting up the Integral for Total Potential
Substitute dM=7R22Mrdr into the expression for dVP:
dVP=−16R2+r2G(7R22Mrdr)=−7R22GM16R2+r2rdr
To find the total potential VP, we integrate from the inner radius r=3R to the outer radius r=4R:
VP=−7R22GM∫3R4R16R2+r2rdr
Solving the Integral: Substitution
Let t2=16R2+r2
Differentiating both sides:
2tdt=2rdr⟹rdr=tdt
Changing the limits of integration:
At r=3R⟹t=16R2+9R2=5R
At r=4R⟹t=16R2+16R2=42R
Evaluating the Integral
Substitute rdr=tdt and 16R2+r2=t into the integral:
VP=−7R22GM∫5R42Rttdt
VP=−7R22GM∫5R42Rdt
VP=−7R22GM[t]5R42R
VP=−7R22GM(42R−5R)
Simplifying the Potential Expression
VP=−7R22GM⋅R(42−5)
VP=−7R2GM(42−5)
Calculating the Work Done
Using the relation W=−VP:
W=−[−7R2GM(42−5)]
W=7R2GM(42−5)
This matches option (a).
Exploring Further Variations
What if the mass was not a unit mass but m?
Then, W=7R2GMm(42−5).
What if point P was at a different height z?
Then, VP=−7R22GM(z2+16R2−z2+9R2).
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The Sigma Insight: Gravitational Potential and Potential Energy
Solution Diagram
Analyzing the Setup
Imagine a flat, ring-like disc—an annular disc—lying in the horizontal plane.
It has an inner boundary of radius 3R and an outer boundary of radius 4R.
Directly above its center, at a height of 4R along the vertical axis, sits our point of interest, point P.
We want to find out how much work is needed to take a tiny unit mass from this point P all the way to infinity, completely escaping the disc's gravitational pull.
The Work-Energy Connection
To find the work done, we use the work-energy theorem.
When we move a mass slowly, the work done by an external agent is simply the change in potential energy:
W=U∞−UP
Since gravity fades to zero at infinite distance, the potential energy at infinity is zero (U∞=0).
This means the work done is simply the negative of the potential energy at point P:
W=−UP
And since we are moving a unit mass (m=1), the work is exactly equal to the negative of the gravitational potential at point P:
W=−VP
So, our main task is to find this potential, VP.
Setting up the Calculus
Before we can integrate to find the potential, we need to know how the mass is distributed across the disc.
The disc is uniform, so we can define a constant surface mass density, σ.
The area of this annular shape is the area of the outer circle minus the area of the inner circle:
A=π(4R)2−π(3R)2=16πR2−9πR2=7πR2
Dividing the total mass M by this area, we get our surface mass density:
σ=7πR2M
Now, let's use the power of calculus! We divide the entire annular disc into infinitely many thin concentric rings.
Let's focus on one such representative ring of radius r and extremely small width dr.
The area of this thin strip is its circumference, 2πr, multiplied by its width, dr:
dA=2πrdr
To find its tiny mass, dM, we multiply this area by our surface mass density, σ:
dM=σdA=(7πR2M)(2πrdr)=7R22Mrdr
Next, let's find the gravitational potential at point P due to just this single elemental ring.
Because of the symmetry, every single point on this ring is at the exact same distance from point P.
Using the Pythagorean theorem on our right-angled triangle, this distance is:
s=(4R)2+r2=16R2+r2
Since potential is a scalar quantity, we can write the elemental potential, dVP, simply as:
dVP=−sGdM=−16R2+r2GdM
Substituting our expression for dM:
dVP=−7R22GM16R2+r2rdr
To find the total potential, VP, produced by the entire disc, we must sum up the contributions of all such rings by integrating from the inner radius 3R to the outer radius 4R:
VP=−7R22GM∫3R4R16R2+r2rdr
The Integration Journey
To solve this integral, we can use a simple substitution.
Let's define a new variable, t2, equal to 16R2+r2.
Differentiating both sides gives:
2tdt=2rdr⟹rdr=tdt
We also need to update our integration limits for this new variable:
- When r=3R, t=16R2+9R2=5R
- When r=4R, t=16R2+16R2=42R
Let's substitute these new terms and limits back into our integral:
VP=−7R22GM∫5R42Rttdt
The t in the numerator and denominator cancel out beautifully, leaving us with the simplest possible integral:
VP=−7R22GM∫5R42Rdt
Integrating dt gives us simply t:
VP=−7R22GM[t]5R42R
Evaluating this at the upper and lower limits, we get:
VP=−7R22GM(42R−5R)
Factoring out R from the bracket and dividing it by R2 in the denominator leaves us with a single R in the denominator: