Introduction to Gravitational Fields
Imagine standing on the surface of a massive, uniform planet.
The gravitational pull you feel is a consequence of the entire mass of the planet acting upon you.
But what happens if you start tunneling deep towards the center of this planet?
Or what if you blast off in a rocket, soaring high above its atmosphere?
This classic problem from the 1994 JEE paper invites us to explore how the gravitational field intensity, F, behaves in these two fundamentally different environments: deep inside a solid sphere and far out in space.
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Analyzing the Setup
Let us define our system.
We have a uniform solid sphere of mass M and radius R.
We want to compare the gravitational field strengths F1 and F2 at two different radial distances, r1 and r2, from the center of the sphere.
To solve this, we must divide our analysis into two distinct physical domains:
1. The Interior Domain (r<R): Where we are deep inside the bulk of the sphere.
2. The Exterior Domain (r>R): Where we are completely outside the sphere.
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Domain 1
Deep Inside the Sphere (r<R)
When you are inside a uniform solid sphere at a distance r from the center, a fascinating physical phenomenon occurs.
According to Newton's Shell Theorem, the spherical shell of mass that lies at radii greater than r exerts zero net gravitational force on you!
All the gravitational pulls from the outer layers cancel each other out perfectly.
Therefore, the only mass that contributes to the gravitational field at your location is the mass enclosed within a smaller sphere of radius r.
Let's write this mathematically. The enclosed mass Menc is:
Menc=ρ⋅Venc=(34πR3M)⋅(34πr3)=MR3r3
Now, applying Newton's law of gravitation as if this enclosed mass were concentrated at the center:
F=r2GMenc=r2G(MR3r3)=R3GMr
This is a beautiful result!
It tells us that inside a uniform solid sphere, the gravitational field intensity is directly proportional to the distance from the center:
If we have two points r1 and r2 both lying inside the sphere (r1<R and r2<R), their fields are:
F1=R3GMr1andF2=R3GMr2
Taking the ratio of these two fields, the constants G, M, and R3 cancel out beautifully:
This perfectly matches Option (a)!
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Domain 2
Far Out in Space (r>R)
Now, let's blast off and look at the sphere from the outside.
According to the second part of the Shell Theorem, for any point outside a spherically symmetric mass distribution, the entire mass behaves as if it were concentrated at a single point at the geometric center.
Thus, the gravitational field intensity simply follows the classic inverse-square law:
Here, the field is inversely proportional to the square of the distance from the center:
If we have two points r1 and r2 both lying outside the sphere (r1>R and r2>R), their fields are:
F1=r12GMandF2=r22GM
Taking the ratio of these two fields:
F2F1=r22GMr12GM=r12r22
This perfectly matches Option (b)!
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Summary of Results
By carefully analyzing both domains, we have shown that:
Inside the sphere (r<R), the field is linear: F2F1=r2r1. This makes Option (a)* correct and rules out Options (c) and (d).
Outside the sphere (r>R), the field follows the inverse-square law: F2F1=r12r22. This makes Option (b)* correct.
Thus, the correct options are (a) and (b).