Orbital Dynamics and Kepler's Laws
This page delves deeper into orbital dynamics and introduces Kepler's Laws, which are fundamental to understanding planetary motion in our solar system.
The page starts by examining the conditions for circular orbits, where tangential acceleration is zero and normal acceleration is constant. It derives the expression for orbital velocity and period for circular orbits.
Example: For a circular orbit, the orbital period T is given by T = 2πr / √(GM/r), where r is the orbital radius and M is the mass of the central body.
The page then introduces Kepler's Three Laws of planetary motion:
- The orbit of each planet is an ellipse with the Sun at one of the two foci.
- A line segment joining a planet and the Sun sweeps out equal areas during equal intervals of time.
- The square of the orbital period of a planet is directly proportional to the cube of the semi-major axis of its orbit.
Highlight: Kepler's Third Law is expressed mathematically as T² / r³ = constant, a relationship crucial for comparing different orbits.
These laws provide a powerful framework for understanding and predicting planetary motion, forming the basis for modern celestial mechanics.