Gravitation, Satellite Motion, and Rotational Kinematics Guide

Universal Law of Gravitation and Weight Calculations

  • Inverse Square Law of Gravity: The gravitational force (FgF_g) between two objects is inversely proportional to the square of the distance between their centers (rr). Mathematically, F=Gm1m2r2F = \frac{G m_1 m_2}{r^2}. This implies that if the distance from the center of Earth doubles (r=2Rearthr = 2R_{earth}), the weight of an object decreases to one-quarter (1/41/4) of its weight at the surface.
  • Acceleration due to Gravity (gg) on Various Planets:     * The formula for acceleration due to gravity is g=GMR2g = \frac{G M}{R^2}, where G=6.67×1011Nm2/kg2G = 6.67 \times 10^{-11}\,N \cdot m^2/kg^2, MM is the planet's mass, and RR is its radius.     * Hypothetical Planet Scenarios:         * If a planet has half the mass of Earth and twice the radius (Mp=1/2MEM_p = 1/2 M_E, Rp=2RER_p = 2R_E), the acceleration due to gravity is g/8g/8.         * If a planet has one-third the mass and one-third the radius of Earth (Mp=1/3MEM_p = 1/3 M_E, Rp=1/3RER_p = 1/3 R_E), the gravity gg is 3g3g.         * If two planets have the same surface gravity but Planet B has twice the radius of Planet A, Planet B must have four times the mass (4m4m).         * If Planet A has twice the mass of Planet B but the radii are unknown, the acceleration due to gravity at the surface cannot be determined without the radius values.
  • Gravity at Specific Altitudes:     * At an altitude equal to the radius of the Earth (r=2Rearthr = 2R_{earth}), the acceleration due to gravity is g/4g/4.     * To find the height where gravity is a specific fraction of surface gravity (e.g., 0.54g0.54g), use the ratio galtgsurface=(RERE+h)2\frac{g_{alt}}{g_{surface}} = \left(\frac{R_E}{R_E + h}\right)^2. For Earth (RE=6.38×106mR_E = 6.38 \times 10^6\,m, ME=5.97×1024kgM_E = 5.97 \times 10^{24}\,kg), an acceleration of 0.54g0.54g occurs at an altitude of approximately 2300km2300\,km.     * An acceleration of 7.8m/s27.8\,m/s^2 on Earth occurs at an altitude of approximately 770km770\,km.
  • Gravitational Force Examples:     * The gravitational force between two 59kg59\,kg people standing 2.0m2.0\,m apart is approximately 5.8×108N5.8 \times 10^{-8}\,N.     * The force on a 70kg70\,kg person due to the Moon (M=7.35×1022kgM = 7.35 \times 10^{22}\,kg, distance r=3.82×108mr = 3.82 \times 10^8\,m) is 0.0024N0.0024\,N.     * Equilibrium Force Point: The point between Earth (ME=5.97×1024kgM_E = 5.97 \times 10^{24}\,kg) and the Moon (Mm=7.35×1022kgM_m = 7.35 \times 10^{22}\,kg) where gravitational forces cancel is located approximately 3.84×107m3.84 \times 10^7\,m from the center of the Moon.

Satellite Motion and Kepler's Laws

  • Orbital Speed and Mass Independence: The speed (vv) of a satellite in a circular orbit depends only on the mass of the central body (MM) and the orbital radius (rr), not the mass of the satellite itself. The formula is v=GMrv = \sqrt{\frac{GM}{r}}. Therefore, if Satellite A has twice the mass of Satellite B but orbits at the same distance, their speeds are equal.
  • Orbital Period (TT): Defined by Kepler's Third Law as T2=4π2r3GMT^2 = \frac{4 \pi^2 r^3}{GM}. This means T2r3T^2 \propto r^3. If the Sun's mass quadrupled, the Earth's orbital period would reduce to 1/21/2 of its current length (approx. 66 months).
  • Kepler's Three Laws:     1. First Law: Planets move in elliptical orbits with the Sun at one focus.     2. Second Law: A line joining a planet and the Sun sweeps out equal areas during equal intervals of time, meaning orbital speed increases as the planet nears the Sun (perihelion) and decreases as it moves away (aphelion).     3. Third Law: The ratio T2r3\frac{T^2}{r^3} is constant for all objects orbiting the same central mass.
  • Weightlessness in Space: Astronauts feel weightless not because gravity is absent, but because they and their satellite are in a state of continuous free-fall toward Earth.
  • Orbital Examples:     * International Space Station: At an altitude of 370km370\,km, the period is approximately 5.5×103s5.5 \times 10^3\,s and the speed is 7.7×103m/s7.7 \times 10^3\,m/s.     * A satellite revolving 55 times a day around Earth requires an orbital radius of 1.44×107m1.44 \times 10^7\,m.     * Jupiter-Earth Comparison: Using Kepler's Third Law TJ2RJ3=TE2RE3\frac{T_J^2}{R_J^3} = \frac{T_E^2}{R_E^3}, given Earth is 1.50×1011m1.50 \times 10^{11}\,m from the Sun and Jupiter is 7.78×1011m7.78 \times 10^{11}\,m, Jupiter's orbital period is approximately 1212 years.

Escape Speed and Potential Energy

  • Escape Speed (vescv_{esc}): The minimum speed required for an object to escape the gravitational pull of a celestial body without further propulsion. It is calculated as vesc=2GMRv_{esc} = \sqrt{\frac{2GM}{R}}.     * Escape speed is independent of the mass of the escaping object; a 20N20\,N rocket and a 20,000N20,000\,N rocket have the same escape speed from the same planet.     * If a planet has the same mass/radius ratio as Earth (M/RM/R is the same, e.g., Planet X-39 with 1/31/3 mass and 1/31/3 radius), the escape speed is equal to Earth's escape speed.
  • Gravitational Potential Energy (UU): Defined as U=Gm1m2rU = -\frac{G m_1 m_2}{r}. For a system of multiple masses, the total potential energy is the sum of the potential energies of every pair of masses.     * Energy Requirements for Orbit Changes: To move an 825kg825\,kg vehicle from an orbit of radius 10,300km10,300\,km to 17,400km17,400\,km, the energy required is the difference in total mechanical energy (E=GMm2rE = -\frac{GMm}{2r}), resulting in approximately 1.30×1010J1.30 \times 10^{10}\,J.     * Impact Velocity: An asteroid falling from a very great distance hits Earth with a speed related to the conservation of energy. For an asteroid starting with 6500m/s6500\,m/s far away, it hits Earth at approximately 12,900m/s12,900\,m/s.

Uniform Circular Motion and Banked Curves

  • Centripetal Force and Acceleration: In uniform circular motion, acceleration (ac=v2ra_c = \frac{v^2}{r}) is always directed toward the center of the circular path. The force causing this acceleration is the centripetal force (Fc=mv2rF_c = \frac{mv^2}{r}).
  • Friction on Curves: On an unbanked (horizontal) curve, static friction between the tires and the road provides the centripetal force (fs=mv2rf_s = \frac{mv^2}{r}). The maximum safe speed is vmax=μsgrv_{max} = \sqrt{\mu_s g r}.     * If a car hits ice (where friction becomes zero), it moves in a straight-line path in its original direction (tangent to the circle) due to inertia.
  • Vertical Circular Motion:     * Loop-the-loop: The minimum speed at the top to prevent falling out (assuming no straps) is v=grv = \sqrt{gr}. For a 13.2m13.2\,m radius loop, this is 11.4m/s11.4\,m/s.     * Vertical Bumps and Depressions: At the top of a bump, the normal force is N=mgmv2rN = mg - \frac{mv^2}{r}. At the bottom of a depression, it is N=mg+mv2rN = mg + \frac{mv^2}{r}.
  • Banked Curves: Curves are banked at an angle θ\theta to allow vehicles to navigate them without relying on friction. The relationship is tan(θ)=v2rg\tan(\theta) = \frac{v^2}{rg}.     * For a radius of 110m110\,m and speed of 24.5m/s24.5\,m/s, the proper angle is 29.129.1^{\circ}.     * The safe speed on a banked curve is independent of the vehicle's mass and the quality of its tires (traction).
  • Artificial Gravity: Space stations can simulate gravity by rotating. A cylinder of diameter 380m380\,m needs a rotation period of 28s28\,s to provide normal gravity (9.8m/s29.8\,m/s^2).

Rotational Kinematics and Angular Quantities

  • Relationship between Angular and Linear Variables:     * Angular displacement: θ\theta     * Angular speed: ω=vr\omega = \frac{v}{r}     * Tangential acceleration: at=rαa_t = r \alpha     * Radial (Centripetal) acceleration: ar=rω2a_r = r \omega^2
  • Rigid Body Rotation: For a rigid object rotating about a fixed axis, all points on the object have the same angular speed (ω\omega) and angular acceleration (α\alpha). However, points farther from the axis have greater tangential speeds (vv) and radial accelerations (ara_r).
  • Rotational Kinematics Equations (Constant α\alpha):     1. ω=ω0+αt\omega = \omega_0 + \alpha t     2. Δθ=ω0t+12αt2\Delta \theta = \omega_0 t + \frac{1}{2} \alpha t^2     3. ω2=ω02+2αΔθ\omega^2 = \omega_0^2 + 2 \alpha \Delta \theta
  • Calculations and Unit Conversions:     * To convert RPM to rad/srad/s: ω=RPM×2π60\omega = \text{RPM} \times \frac{2 \pi}{60}. Example: 813.0rpm=85.14rad/s813.0\,rpm = 85.14\,rad/s.     * A centrifuge slowing from 3600rev/min3600\,rev/min to rest over 5050 turns has an angular acceleration magnitude of 230rad/s2230\,rad/s^2 and takes 1.7s1.7\,s to stop.     * A wheel accelerating from rest (ω0=0\omega_0 = 0) at 4.5rad/s24.5\,rad/s^2 for 2.0s2.0\,s turns through an angle of 11rad11\,rad and reaches a speed of 10rad/s10\,rad/s.