Laws of Kepler and Newton
Laws of Kepler and Newton
Introduction
Review of lectures by Pan Asen.
Focus on details needed for the International Olympiad on Astronomy (IOAA).
Third Law of Kepler and Newton's Law of Gravitation
Newton's Law of Gravitation (scalar form): F = G \frac{Mm}{R^2}
G is the gravitational constant.
M and m are the masses of the two bodies.
R is the distance between the centers of the two bodies.
Center of Mass
Formula for the radius vector of the center of mass:
R = \frac{\sum mi ri}{\sum m_i}$r_i$ is the radius vector of the i-th body.
$m_i$ is the mass of the i-th body.
If the origin is at the center of mass, then the radius vector of the center of mass is zero.
For two bodies with masses M1 and M2 and distances R1 and R2 from the center of mass:
\frac{M1}{M2} = \frac{R2}{R1}
M1 R1 = M2 R2
Derivation of Kepler's Third Law
Equating Newton's Law of Gravitation with centripetal force:
G \frac{Mm}{R^2} = m aCentripetal acceleration:
a = \frac{V^2}{r} = 4\pi^2 \frac{R}{T^2}
r is the distance from the body to the center of mass.
R is the distance between the two masses.
Relating distances to the center of mass:
\frac{M}{m} = \frac{R_1}{R}R + R_1 = r
R_1 = \frac{mR}{M}
r = R + \frac{mR}{M} = R(1 + \frac{m}{M})
Substituting R into the force equation:
G \frac{Mm}{R^2} = m \frac{4\pi^2 R}{T^2}G \frac{Mm}{R^2} = m 4\pi^2 \frac{1}{T^2} \frac{R}{(1+\frac{m}{M})^3}
T^2 = \frac{4\pi^2}{GM}(M+m)r^3
T^2 = \frac{4\pi^2}{G(M+m)}r^3
Cosmic Velocities
First Cosmic Velocity
The velocity required for a body to orbit a planet in a circular orbit.
Derived by equating gravitational force and centripetal force.
V_1 = \sqrt{\frac{GM}{R}}
Second Cosmic Velocity
The velocity required for a body to escape the gravitational influence of a planet.
Derived by setting the total energy of the body to zero.
V_2 = \sqrt{\frac{2GM}{R}}
V2 = \sqrt{2} \cdot V1
Conservation Laws
Applicable in a closed system without non-conservative forces.
Conservation of Energy
In a closed system, the total energy is conserved.
Total energy = Potential energy + Kinetic energy
Potential energy:
U = -\frac{GMm}{R}Kinetic energy:
K = \frac{1}{2} mv^2Total energy at infinity is zero (assuming zero initial velocity).
The formula U = mgh is only valid when the gravitational acceleration is constant.
Conservation of Angular Momentum
The product of the moment of inertia and angular velocity is constant.
L = r \times p = r \times mv = mrVsin(\alpha) = constant
$\alpha$ is the angle between the radius vector and the velocity vector.
If the force is in the radial direction, the angular momentum is conserved.
Kepler's Second Law
Equal areas are swept out in equal times.
dS = \frac{1}{2}r(V \Delta t) sin(\alpha)
\frac{dS}{dt} = \frac{L}{2m} = constant
Radiation and Albedo
Luminosity
The total energy radiated by an object per unit time.
Energy flux at a distance R:
F = \frac{L}{4\pi R^2}Solar constant: The power of solar radiation per unit area at the Earth's orbit.
Energy Absorption
Energy absorbed by a body:
E = \frac{L \pi r^2}{4 \pi R^2}For objects close to a star, integration over the surface may be needed.
Albedo
The fraction of incident radiation that is reflected by a surface.
Radiated energy:
E_r = \frac{A L \pi r^2}{4 \pi R^2}Emitted radiation at distance R':
F = \frac{A L r^2}{8 \pi^2 R^2 R'^2}
Vis-Viva Equation
Allows calculation of the velocity at any point in an orbit given the distance to that point.
V^2 = GM \left( \frac{2}{r} - \frac{1}{a} \right)
V is the speed of the body.
G is the gravitational constant.
M is the mass of the central body.
r is the distance between the bodies.
a is the semi-major axis of the orbit.
Derived from conservation of energy.
Virial Theorem
Relates the average kinetic energy of particles in a system to the forces acting within the system.
2 \langle T \rangle = n \langle U \rangle
$\langle T \rangle$ is the average kinetic energy.
$\langle U \rangle$ is the average potential energy.
n is related to the force (related to the inverse square law of gravity).
For gravitational forces (U = -\frac{GMm}{R}), n = -1. Then:
2 \langle T \rangle = -\langle U \rangleFor a gravitationally bound system:
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