Question
Question: Kepler's second law is a consequence of (A) Conservation of energy (B) Conservation of linear mo...
Kepler's second law is a consequence of
(A) Conservation of energy
(B) Conservation of linear momentum
(C) Conservation of angular momentum
(D) Conservation of mass
Solution
Kepler's second law states that the planet moves in an elliptical orbit such that the line between it and the Sun placed at a focus sweeps out equal areas in equal times. Conservation of angular momentum states that the angular momentum of a body remains constant unless an external torque is applied.
Formula used:
The area of the triangle/wedge is A=21×base×height
rdtdθ=v (Where v is linear velocity, dθ is an elemental angle which we have considered, r is the radius of the orbit of which the wedge is a part anddtis the elemental time in which our observation is made.)
L=m(r×v)(Where L is angular momentum)
Complete step-by-step answer:
Consider a small wedge of the orbit traced out in time dt, dθ is an elemental angle which we have considered, r is the radius of the orbit of which the wedge is a part
So,
Area of the wedge is, A=21×base×height
The base is r and height is rdθ, dA is the area of the wedge,
⇒dA=21r×rdθ
The rate at which area is swept out is,
⇒dtdA=21r×rdtdθ
since rdtdθ=v , where v is linear velocity, θ is the angle between r and v
⇒dtdA=21rvθ
We know that,
L Is angular momentum and m is the mass of the object
⇒L=m(r×v)
⇒L=mrvsinθ
As θ is very small, sinθ≃θ
⇒L=mrvθ
From the above equation, we can draw that,
⇒dtdA=21mL
Hence dtdA is constant with time as L is constant (from conservation of angular momentum) and mass is also constant. This is what Kepler stated in his second law.
Hence option (C) Conservation of angular momentum is the correct answer.
Note
Kepler gave three such laws on the planetary motion we just saw and proved the second law given by Kepler. The first law explained that the earth moves in an elliptical orbit and the sun is present at one of the foci of that ellipse. The third law gave the relation between the length of the semi-major axis of an ellipse about which earth is moving and the time period of this motion.