Analyzing the Setup
Imagine a vast, spherical cloud of gas floating in the emptiness of space. This isn't just any cloud; it's a dynamic system where every single particle of mass m is orbiting the common center in perfect circles.
The problem gives us a fascinating constraint: every particle, regardless of its orbital radius r, possesses the exact same kinetic energy K. Our goal is to uncover the hidden structure of this cloud—specifically, how the number of particles per unit volume, n(r), changes as we move outward from the center.
To begin, let's focus on a single particle of mass m orbiting at a distance r. According to Newton's Shell Theorem, the gravitational force acting on this particle is determined solely by the mass enclosed within its orbit. Let's call this enclosed mass M.
The Master Equation
For our particle to maintain its circular orbit, it requires a centripetal force. In this isolated system, the only force available to play this role is the mutual gravitational attraction from the enclosed mass M.
We can set up our fundamental dynamic equation by equating the gravitational force to the required centripetal force:
This equation is the bridge between the geometry of the orbit and the mass distribution of the cloud.
The Kinetic Energy Connection
The problem states that the kinetic energy K is constant for all particles. We know the formula for kinetic energy is K=21mv2.
Let's manipulate our force equation to reveal this kinetic energy term. By multiplying both sides by r, we get:
Now, we can substitute mv2 with 2K:
This is a beautiful result! It directly links the enclosed mass M to the constant kinetic energy K. Let's isolate M to see how the enclosed mass grows with the radius:
Notice that since K, G, and m are all constants, the enclosed mass M increases linearly with the radius r.
Unveiling the Mass Distribution
We have the total enclosed mass M(r), but we need the local mass density ρ(r). To find this, we must look at how the mass changes as we increase the radius by a tiny amount dr.
Let's differentiate our mass equation with respect to r:
This dM represents the mass of a very thin spherical shell of thickness dr located at radius r.
Geometrically, the mass of this thin shell can also be expressed as its volume multiplied by the local density ρ(r). The volume of a thin spherical shell is its surface area (4πr2) times its thickness (dr):
Now, we have two distinct expressions for the same tiny mass dM. Let's equate them to solve for the density:
The dr terms cancel out perfectly, leaving us with:
Simplifying the fraction, we arrive at the mass density profile of the cloud:
Final Calculation
We are almost there! The question asks for the particle number density, n(r), which is the number of particles per unit volume.
Since we know the total mass per unit volume (ρ(r)) and the mass of a single particle (m), we can find the number density by simply dividing the mass density by the mass of one particle:
Substituting our expression for ρ(r):
This matches option (D). The inverse-square dependence on r tells us that the cloud is much denser at the center and thins out rapidly as we move towards the edges.