Animated Solution for Physics - Gravitation: The angular momentum of a planet of mass M moving around the Sun in an elliptical orbit is L. The magnitude of the areal velocity of the planet is
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Visualized Solution
The Elliptical Orbit
\text{Consider a planet of mass } M \text{ moving around the Sun.}
\text{Let the planet be at position } P \text{ at time } t.
Areal Velocity Setup
\text{In a small time interval } dt \text{, the planet moves to } P'.
\text{The magnitude of the areal velocity is } \frac{L}{2M}.
\text{This is a constant, verifying Kepler's Second Law.}
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The Sigma Insight: Kepler's Laws of Planetary Motion
Solution Diagram
The Geometry of the Orbit
Imagine standing far above the solar system, watching a planet glide silently along its elliptical path around the Sun. As it moves, the imaginary line connecting the Sun to the planet sweeps across the vastness of space.
If we look at a tiny snapshot of time, dt, the planet moves from a point P to a new point P′. The radius vector r sweeps out a small, almost triangular sliver of area, which we call dA. From the geometry of polar coordinates, the area of this infinitesimally small sector is given by:
dA=21r2dθ
To find how fast this area is being swept—the areal velocity—we simply divide by our tiny time interval dt:
dtdA=21r2dtdθ
Since the rate of change of the angle dtdθ is just the angular velocity ω, our areal velocity equation beautifully simplifies to:
dtdA=21r2ω
Angular Momentum
The Rotational Drive
Now, let's shift our perspective from pure geometry to the physical forces driving this motion. The planet has a mass M and is moving with some velocity v. Because it's orbiting a central body (the Sun), it possesses angular momentum, denoted by L.
The angular momentum of a particle about a central point is the product of its mass, its distance from the center, and its perpendicular velocity:
L=Mv⊥r
In circular or instantaneous rotational motion, the perpendicular velocity is intimately tied to the angular velocity by the relation v⊥=rω. Substituting this into our angular momentum equation gives:
L=M(rω)r=Mr2ω
The Beautiful Synthesis
We now hold two powerful equations in our hands. One describes the geometric sweeping of space, and the other describes the physical conservation of rotational motion. Let's bring them together.
From our angular momentum equation, we can isolate the angular velocity ω:
ω=Mr2L
Now, we take this expression for ω and substitute it back into our areal velocity equation:
dtdA=21r2(Mr2L)
Look at what happens next. The r2 in the numerator and the r2 in the denominator perfectly cancel each other out. The varying distance of the planet from the Sun completely vanishes from the equation! We are left with a stunningly simple and profound result:
dtdA=2ML
Because the angular momentum L is conserved (due to the absence of external torques) and the mass M is constant, the areal velocity 2ML must also be a constant. This elegant mathematical dance is the exact proof of Kepler's Second Law of Planetary Motion.