Specific relative angular momentum
- See also: Classical central-force problem
In celestial mechanics the specific relative angular momentum plays a pivotal role in the analysis of the two-body problem. One can show that it is a constant vector for a given orbit under ideal conditions. This essentially proves Kepler's second law.
It's called specific angular momentum because it's not the actual angular momentum , but the angular momentum per mass
The vector is always perpendicular to the instantaneous osculating orbital plane, which coincides with the instantaneous perturbed orbit. It would not necessarily be perpendicular to an average plane which accounted for many years of perturbations.
As usual in physics, the magnitude of the vector quantity is denoted by :
Proof that the specific relative angular momentum is constant under ideal conditions
What follows is only valid under the simplifications that also count for Newton's law of universal gravitation.
One looks at to point masses and , at the distance from one another and with the gravitational force acting between them. This force acts instantly, over any distance and is the only force present. The coordinate system is inertial.
The further simplification is assumed in the following. Thus is the central body in the origin of the coordinate system and is the satellite orbiting around it. Now the reduced mass is also equal to and the equation of the two-body problem is
It is important not to confound the gravitational parameter with the reduced mass, which is sometimes also denoted by the same letter .
One obtains the specific relative angular momentum by multiplying (cross product) the equation of the two-body problem with the distance vector
The cross product of a vector with itself (right hand side) is 0. The left hand side simplifies to
according to the product rule of differentiation.
This vector is perpendicular to the orbit plane, the orbit remains in this plane because the angular momentum is constant.
One can obtain further insight into the two-body problem with the definitions of the flight path angle and the transversal and radial component of the velocity vector (see illustration on the right). The next three formulas are all equivalent possibilities to calculate the absolute value of the specific relative angular momentum vector
Kepler's laws of planetary motion
Kepler's laws of planetary motion can be proved almost directly with the above relationships.
The proof starts again with the equation of the two-body problem. This time one multiplies it (cross product) with the specific relative angular momentum
The left hand side of the is equal to the derivative because the angular momentum is constant.
After some steps the right hand side becomes
Setting these two expression equal and integrating over time leads to (with the constant of integration )
Now this equation is multiplied (dot product) with and rearranged
which is the equation of a conic section in polar coordinates with semi-latus rectum and eccentricity . This proves Kepler's first law, in words:
The orbit of a planet is an ellipse with the Sun at one focus.
The second law follows instantly from the second of the three equations to calculate the absolute value of the specific relative angular momentum.
If one connects this form of the equation with the relationship for the area of a sector with an infinitesimal small angle (triangle with one very small side), the equation [References 4]
comes out, that is the mathematical formulation of the words:
The line joining the planet to the Sun sweeps out equal areas in equal times.
Kepler's third is a direct consequence of the second law. Integrating over one revolution gives the orbital period
for the area of an ellipse. Replacing the semi-minor axis with and the specific relative angular momentum with one gets [References 4]
There is thus a relationship between the semi-major axis and the orbital period of a satellite that can be reduced to a constant of the central body. This is the same as the famous formulation of the law:
The square of the period of a planet is proportional to the cube of its mean distance to the Sun.
- Specific orbital energy, another conserved quantity in the two-body problem.
- The derivation of the specific angular momentum works also if one does not make this assumption. Then the origin of the coordinate system is in the barycenter, the gravitational parameter is and remains the reduced mass (not ). But this approximation is often very good and the proofs of Kepler's laws become easier.
- Vallado, David Anthony (2001). Fundamentals of Astrodynamics and Applications. Springer. p. 24. ISBN 0-7923-6903-3.
- Vallado, David Anthony (2001). Fundamentals of Astrodynamics and Applications. Springer. p. 28. ISBN 0-7923-6903-3.
- Vallado, David Anthony (2001). Fundamentals of Astrodynamics and Applications. Springer. p. 10. ISBN 0-7923-6903-3.
- Vallado, David Anthony (2001). Fundamentals of Astrodynamics and Applications. Springer. p. 30. ISBN 0-7923-6903-3.