Chapter 4 - Motion in gravitational fields

Newton’s Law of Universal Gravitation

  • The law states that the force between two objects with mass is given by:F = \frac{GMm}{r^2}

  • Where:

    • F is the gravitational force

    • G is the gravitational constant (6.674 × 10^-11 N(m/kg)^2)

    • M and m are the masses of the two objects

    • r is the separation between the centers of the two masses

Outcomes Related to Gravitational Motion

  • Apply Newton's Law both qualitatively and quantitatively to determine gravitational forces and predict gravitational field strength (g) at different points, including Earth's surface.

  • Investigate the orbital motion of planets and satellites, focusing on relationships among gravitational force, centripetal force, acceleration, mass, radius, velocity, and orbital period.

  • Utilize mathematical equations like:g = \frac{GM}{r^2}to predict gravitational properties in varying scenarios, including geostationary orbits.

Kepler’s Laws of Planetary Motion

  • Provides a foundation for understanding how the gravitational forces affect planetary motions.

  • Kepler's First Law: Planets move in elliptical orbits with the Sun at one focus.

  • Kepler's Second Law: A line segment joining a planet and the Sun sweeps out equal areas during equal intervals of time, meaning planets move faster when closer to the Sun.

  • Kepler's Third Law: The square of the orbital period (T^2) is proportional to the cube of the semi-major axis of its orbit (r^3): T^2 \propto r^3.

Gravitational Field Strength

  • Defined as the gravitational force per unit mass: g = \frac{F}{m}.

  • Close to Earth, this is approximately 9.8 N/kg.

  • The concept of a gravitational field explains how objects such as satellites orbit due to gravity acting as a centripetal force.

Orbital Properties of Satellites

  • For a satellite to remain in orbit:

    • The gravitational force acts as the net centripetal force:\frac{GMm}{r^2} = \frac{mv^2}{r}.

  • The orbital velocity (v) can be derived as:v = \sqrt{\frac{GM}{r}}.

  • Orbital period (T) is related to orbital radius by:T = 2\pi \sqrt{\frac{r^3}{GM}}.

  • For geostationary satellites, the orbital radius is around 36,000 km above Earth's surface, matching Earth's rotation period.

Gravitational Potential Energy

  • Gravitational potential energy (U) is expressed as:U = - \frac{GMm}{r}.

  • The total energy (E) of a satellite in orbit is:E = K + U = \frac{mv^2}{2} - \frac{GMm}{r}.

  • The escape velocity (V_escape) from a gravitational field is determined by:V_escape = \sqrt{\frac{2GM}{R}}.

Application and Prediction

  • Use these relationships to solve physical problems, including predicting the gravitational force between celestial bodies, understanding escape velocities, and analyzing satellite motion and stability.

  • Investigate orbital properties quantitatively, which is applicable for near Earth and other celestial bodies.