Study Notes on Gravitation

Chapter 13: Gravitation

The Goals of this Chapter

  • Understand the following definitions:
      - Geosynchronous Orbit: An orbit where the satellite has a period equal to the rotation of the Earth (24 hours).
      - Aphelion/Apogee: The furthest distance from the Sun/Earth in an orbit.
      - Perihelion/Perigee: The closest distance to the Sun/Earth in an orbit.

  • Recognize when to apply:
      - The new formulae concerning gravitational force and gravitational potential energy.

  • Apply Kepler’s Laws:
      - To analyze both elliptical and spherical orbits.

  • Understand Escape Velocity:
      - The minimum velocity required for an object to break free from a gravitational field without further propulsion.

Newton’s Law of Universal Gravitation

  • Conceptual Inquiry:
      - Explore the relationship between gravitational force acting upon an apple and the moon in orbit.
      - When throwing an apple horizontally from a mountain, it falls, illustrating Earth's curvature.
      - The challenge is to throw the apple fast enough to continuously fall without moving closer to the ground—a demonstration of orbital motion.

  • Illustration:
      - Newton provided sketches in his work "Principia" of 1687 showing these concepts visually.

The Inverse Square Law

  • Fundamentals:
      - The same gravitational force acts on both the apple and the moon, affirming its universal nature.

  • Characteristics of Gravitational Force:
      - The gravitational force is:
        - Always attractive.
        - Proportional to the product of the two masses involved.
        - Inversely proportional to the square of the distance between them, expressed mathematically as:
          F=Gm1m2r2F = G \frac{m_1 m_2}{r^2}

  • Value of Gravitational Constant (G):
      - G=6.67×1011 N m2/kg2G = 6.67 \times 10^{-11} \text{ N m}^2/\text{kg}^2

  • Force Vector Notation:
      - F=Gm1m2r2r^\mathbf{F} = -\frac{G m_1 m_2}{r^2} \hat{r}

  • Key Variables:
      - m1m_1, m2m_2: masses of the two bodies.
      - rr: distance between the centers of the two masses.

Gravitational Attraction Between Spherical Bodies

  • Complex Calculations:
      - For arbitrary objects, gravitational attraction requires integration over the object's mass distribution:
        F=iGmMir2r^=Gmρ(r)dV1r2dV\mathbf{F} = \sum_i G \frac{m M_i}{r^2} \hat{r} = \int G m \rho(\mathbf{r}) dV \frac{1}{r^2} dV

  • Simplified Approach for Spherical Bodies:
      - For spherical objects (or nearly spherical), treat all mass as concentrated at the center provided the other mass is located outside the sphere.
      - This simplification is proven through calculus in section 13.6 of the textbook.

Connecting G and g

  • Weight Calculation:
      - Relationship between gravitational force and weight can be expressed as:
        F=mg=GmMEr2F = mg = G \frac{m M_E}{r^2}
      - Rearranging gives:
        g=GMEr2g = G \frac{M_E}{r^2}

  • Sea Level Gravitational Acceleration:
      - gSeaLevel=GMERE2g_{Sea Level} = G \frac{M_E}{R_E^2}
      - Calculation yields:
        g=(6.67×1011)(5.97×1024)(6.37×106)2=9.81344m/s2g = (6.67 \times 10^{-11)(5.97 \times 10^{24})}{(6.37 \times 10^{6})^2} = 9.81344 \, m/s^2

  • Gravitational Acceleration at Different Elevations:
      - Example for Mt. St. Helens elevation (2550m):
        gMt.St.Helens=GME(RE+h)2=9.80559m/s2g_{Mt. St. Helens} = G \frac{M_E}{(R_E + h)^2} = 9.80559 \, m/s^2
        - Sea Level value: 1.0008imesg1.0008 imes g.

Earth’s Gravitational Field at the Surface

  • Graphical Representation:
      - Gravitational field representation at various distances from the mass at the origin.
      - The field shows how the mass influences surrounding space; actual force exists only when another mass is present in the field.

Example Problem #1: Weight on Another Planet

  • Problem Setup:
      - Weight of person on Earth = 200 lbs.
      - Given data:
        - Mass of Mars: MMars=6.39×1023kgM_{Mars} = 6.39 \times 10^{23} \, kg
        - Radius of Mars: RMars=3390kmR_{Mars} = 3390 \, km
        - Mass of Earth: MEarth=5.97×1024kgM_{Earth} = 5.97 \times 10^{24} \, kg
        - Radius of Earth: REarth=6370kmR_{Earth} = 6370 \, km

  • Calculation of Weight:
      - Using:
        wMars=wEarthMMarsMEarth(REarthRMars)2w_{Mars} = w_{Earth} \frac{M_{Mars}}{M_{Earth}} \left( \frac{R_{Earth}}{R_{Mars}} \right)^2
        - Substituting values yields:
          wMars=(200lbs)×6.39×1023kg5.97×1024kg×(6370km3390km)2=75.6lbsw_{Mars} = (200 \, lbs) \times \frac{6.39 \times 10^{23} \, kg}{5.97 \times 10^{24} \, kg} \times \left( \frac{6370 \, km}{3390 \, km} \right)^2 = 75.6 \, lbs

The Combo Platter: Inside a Solid Sphere

  • Gravitational Force at Center of Earth:
      - Condition assumed: human survivability under heat and pressure.
      - Derive mass: M=ρ43πr3M = \rho \frac{4}{3} \pi r^3
        - For a portion of Earth: mE(r3RE3)m_E \left( \frac{r^3}{R_E^3} \right).

  • Expression for Gravitational Force:
      - At the center:
        F=GmmERE3rF = G \frac{m m_E}{R_E^3} r

Gravitational Potential Energy

  • Connection to Conservative Forces:
      - Result from previous chapters stating that conservative forces and potential energy are related:
        F=U\mathbf{F} = -\nabla U
      - For gravitational potential energy:
        - U=Gm1m2rU = -G \frac{m_1 m_2}{r}

Connecting Potential Energy Forms

  • Relationship:
      - From different expressions of potential energy:
        U(RE+h)U(RE)=GmEmRE+h+GmEmREU(R_E + h) - U(R_E) = - G \frac{m_E m}{R_E + h} + G \frac{m_E m}{R_E}
      - Rearranging leads to the approximation:
        U(RE+h)U(RE)mghU(R_E + h) - U(R_E) \approx mg h where g=GmERE2g = G \frac{m_E}{R_E^2}.

Concepts of Gravitational Energy

  • Visualizing Energy Differences:
      - Potential energy expressions in different forms:
        - F:2RE,U:3REF: \frac{2}{R_E}, U: \frac{3}{R_E} for different altitudes using gravitational relations.

Escape Velocity

  • Understanding Escape Velocity:
      - Defined as the speed needed to overcome gravitational influence:
        0=U+K<br>ightarrow0=GmMr+12mve20 = U + K <br>ightarrow 0 = -G \frac{m M}{r} + \frac{1}{2} mv_e^2
      - Rearranging gives:
        ve=2GMrv_e = \sqrt{\frac{2GM}{r}}
      - Example escape velocity from Earth:
        ve,Earth=11,180m/sv_{e, Earth} = 11,180 \, m/s (approximately 25,000 mph).

Example Problem #2: Astronaut in Space

  • Scenario:
      - Astronaut of mass 95 kg at rest, stranded 12 m away from a spaceship of mass 880,000 kg.
      - Spaceship radius: 15.4 m.

  • Using Conservation of Energy:
      - Initial energy conservation: U0+K0=Uf+KfGmamsr0U_0 + K_0 = U_f + K_f - G \frac{ma m_s}{r_0}
      - Calculation involving gravitational attraction between the astronaut and spaceship yields:
        v=2Gms(rfr0)v = \sqrt{2G \frac{m_s}{(r_f - r_0)}}

  • Time to Return:
      - Estimating time required to return to the ship:
        test=2Δxaest=11900s3.305hrt_{est} = 2 \frac{\Delta x}{a_{est}} = 11900 \, s \approx 3.305 \, hr
      - Comparative analysis of throwing away flashlight with a velocity of 5.20 m/s.

  • Final Calculations for Velocity and Acceleration:
      - Using gravitational force formula yield spacecraft moving at a deceleration due to gravitational pull.

Kepler’s Laws of Motion

  • 1st Law:
      - Planets move along elliptical paths with the Sun at one focus.
      - Circular orbits are a specific case of this. (e.g., the moon's orbit around Earth).

  • Definitions:
      - Semi-major Axis ($a$): Half the ellipse's longest axis.
      - Semi-minor Axis ($b$): Half the ellipse's shortest axis.
      - Eccentricity ($e$): Measure of how much the orbit deviates from circularity. Defined as:
        e=1(ba)2e = \sqrt{1 - \left(\frac{b}{a}\right)^2}
      - Perihelion/Perigee: Closest distance to the Sun/Earth.
      - Aphelion/Apogee: Farthest distance from the Sun/Earth.

Kepler’s Laws of Motion – 2nd Law

  • Description:
      - Equal area is swept over equal time, implying that planets move faster when closer to the Sun and slower when further away.
      - Associated changes in kinetic energy.

Kepler’s Laws of Motion – 3rd Law

  • Period and Semi-major Axis Relationship:
      - Ta3/2T \propto a^{3/2}, where TT is the orbital period and aa is the semi-major axis.
      - Calculation for the period:
        T=2πa3/21GMT = 2 \pi a^{3/2} \frac{1}{\sqrt{GM}}

  • Astronomical Units:
      - 1 AU is the average distance from the Sun to Earth.
      - Equivalent notation for circular orbits utilizes rr.

Kepler’s Laws of Motion – 3rd Law Extended

  • Graphs of Planetary Periods:

  • Various planets, dwarf planets, and asteroids graphed against their semi-major axes, indicating clear relationships reinforcing Kepler's 3rd Law.

Example Problem #4: Work Required for Satellite Change

  • Context:
      - Satellite being raised from Low Earth Orbit (~800 km) to geosynchronous orbit.

  • Gravitational Calculations:
      - Key values:
        - Mass of Earth: ME=5.97×1024kgM_E = 5.97 \times 10^{24} \, kg.
        - Final calculation indicating the work required in Joules and comparing household energy consumption equivalents.

Halley’s Comet Perihelion and Aphelion Analysis

  • Calculating Distances:
      - Based on gravitational potential energy and angular momentum preservation:
        U0+K0=Uf+KfU_0 + K_0 = U_f + K_f for aphelion distance calculations, reinforcing conservation principles relating to eccentric orbits.