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Title: Gravity, Planetary Orbits, and


1
Chapter 11
  • Gravity, Planetary Orbits, and
  • the Hydrogen Atom

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11.1 Newtons Law of Universal Gravitation
  • Every particle in the Universe attracts every
    other particle with a force that is directly
    proportional to the product of their masses and
    inversely proportional to the square of the
    distance between them
  • G is the universal gravitational constant and
    equals 6.673 x 10-11 N?m2 / kg2

4
More About Forces
  • The forces form a Newtons Third Law
    action-reaction pair
  • Gravitation is a field force that always exists
    between two particles, regardless of the medium
    between them
  • The force decreases rapidly as distance increases
  • A consequence of the inverse square law

Fig 11.1
5
Notation
  • is the force exerted by particle 1 on
    particle 2
  • The negative sign in the vector form of the
    equation indicates that particle 2 is attracted
    toward particle 1
  • is the force exerted by particle 2 on
    particle 1

6
Law of Gravitation, cont
  • This is an example of an inverse square law
  • The magnitude of the force varies as the inverse
    square of the separation of the particles
  • The law can also be expressed in vector form

7
G vs. g
  • Always distinguish between G and g
  • G is the universal gravitational constant
  • It is the same everywhere
  • g is the acceleration due to gravity
  • g 9.80 m/s2 at the surface of the Earth
  • g will vary by location

8
Gravitational Force Due to a Distribution of Mass
  • The gravitational force exerted by a
    finite-sized, spherically symmetric mass
    distribution on a particle outside the
    distribution is the same as if the entire mass of
    the distribution were concentrated at the center
  • For the Earth, this means

9
Measuring G
  • G was first measured by Henry Cavendish in 1798
  • The apparatus shown here allowed the attractive
    force between two spheres to cause the rod to
    rotate
  • The mirror amplifies the motion
  • It was repeated for various masses

Fig 11.2
10
Gravitational Field
  • Use the mental representation of a field
  • A source mass creates a gravitational field
    throughout the space around it
  • A test mass located in the field experiences a
    gravitational force
  • The gravitational field is defined as

11
Gravitational Field of the Earth
  • Consider an object of mass m near the earths
    surface
  • The gravitational field at some point has the
    value of the free fall acceleration
  • At the surface of the earth, r RE and g 9.80
    m/s2

12
Representations of the Gravitational Field
Fig 11.3
  • The gravitational field vectors in the vicinity
    of a uniform spherical mass
  • fig. a the vectors vary in magnitude and
    direction
  • The gravitational field vectors in a small region
    near the earths surface
  • fig. b the vectors are uniform

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Fig 11.4
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11.2 Structural Models
  • In a structural model, we propose theoretical
    structures in an attempt to understand the
    behavior of a system with which we cannot
    interact directly
  • The system may be either much larger or much
    smaller than our macroscopic world
  • One early structural model was the Earths place
    in the Universe
  • The geocentric model and the heliocentric models
    are both structural models

18
Features of a Structural Model
  • A description of the physical components of the
    system
  • A description of where the components are located
    relative to one another and how they interact
  • A description of the time evolution of the system
  • A description of the agreement between
    predictions of the model and actual observations
  • Possibly predictions of new effects, as well

19
11.3 Keplers Laws, Introduction
  • Johannes Kepler was a German astronomer
  • He was Tycho Brahes assistant
  • Brahe was the last of the naked eye astronomers
  • Kepler analyzed Brahes data and formulated three
    laws of planetary motion

20
Keplers Laws
  • Keplers First Law
  • Each planet in the Solar System moves in an
    elliptical orbit with the Sun at one focus
  • Keplers Second Law
  • The radius vector drawn from the Sun to a planet
    sweeps out equal areas in equal time intervals
  • Keplers Third Law
  • The square of the orbital period of any planet is
    proportional to the cube of the semimajor axis of
    the elliptical orbit

21
Notes About Ellipses
  • F1 and F2 are each a focus of the ellipse
  • They are located a distance c from the center
  • The longest distance through the center is the
    major axis
  • a is the semimajor axis

Fig 11.5
22
Notes About Ellipses, cont
  • The shortest distance through the center is the
    minor axis
  • b is the semiminor axis
  • The eccentricity of the ellipse is defined as e
    c /a
  • For a circle, e 0
  • The range of values of the eccentricity for
    ellipses is 0 lt e lt 1

Fig 11.5
23
Notes About Ellipses, Planet Orbits
  • The Sun is at one focus
  • Nothing is located at the other focus
  • Aphelion is the point farthest away from the Sun
  • The distance for aphelion is a c
  • For an orbit around the Earth, this point is
    called the apogee
  • Perihelion is the point nearest the Sun
  • The distance for perihelion is a c
  • For an orbit around the Earth, this point is
    called the perigee

24
Keplers First Law
  • A circular orbit is a special case of the general
    elliptical orbits
  • Is a direct result of the inverse square nature
    of the gravitational force
  • Elliptical (and circular) orbits are allowed for
    bound objects
  • A bound object repeatedly orbits the center
  • An unbound object would pass by and not return
  • These objects could have paths that are parabolas
  • and hyperbolas

25
Orbit Examples
  • Pluto has the highest eccentricity of any planet
    (a)
  • ePluto 0.25
  • Halleys comet has an orbit with high
    eccentricity (b)
  • eHalleys comet 0.97

Fig 11.6
26
Keplers Second Law
  • Is a consequence of conservation of angular
    momentum
  • The force produces no torque, so angular momentum
    is conserved

Fig 11.7(a)
27
Keplers Second Law, cont.
  • Geometrically, in a time dt, the radius vector r
    sweeps out the area dA, which is half the area of
    the parallelogram
  • Its displacement is given by

Fig 11.7(b)
28
Keplers Second Law, final
  • Mathematically, we can say
  • The radius vector from the Sun to any planet
    sweeps out equal areas in equal times
  • The law applies to any central force, whether
    inverse-square or not

29
Keplers Third Law
  • Can be predicted from the inverse square law
  • Start by assuming a circular orbit
  • The gravitational force supplies a centripetal
    force
  • Ks is a constant

30
Keplers Third Law, cont
  • This can be extended to an elliptical orbit
  • Replace r with a
  • Remember a is the semimajor axis
  • Ks is independent of the mass of the planet, and
    so is valid for any planet

31
Keplers Third Law, final
  • If an object is orbiting another object, the
    value of K will depend on the object being
    orbited
  • For example, for the Moon around the Earth, KSun
    is replaced with KEarth

32
Fig 11.8
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11.4 Energy in Satellite Motion
  • Consider an object of mass m moving with a speed
    v in the vicinity of a massive object M
  • M gtgt m
  • We can assume M is at rest
  • The total energy of the two object system is E
    K Ug

35
Energy, cont.
  • Since Ug goes to zero as r goes to infinity, the
    total energy becomes

36
Energy, Circular Orbits
  • For a bound system, E lt 0
  • Total energy becomes
  • This shows the total energy must be negative for
    circular orbits
  • This also shows the kinetic energy of an object
    in a circular orbit is one-half the magnitude of
    the potential energy of the system

37
Energy, Elliptical Orbits
  • The total mechanical energy is also negative in
    the case of elliptical orbits
  • The total energy is
  • r is replaced with a, the semimajor axis

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Fig 11.10
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Escape Speed from Earth
  • An object of mass m is projected upward from the
    Earths surface with an initial speed, vi
  • Use energy considerations to find the minimum
    value of the initial speed needed to allow the
    object to move infinitely far away from the Earth

Fig 11.11
46
Escape Speed From Earth, cont
  • This minimum speed is called the escape speed
  • Note, vesc is independent of the mass of the
    object
  • The result is independent of the direction of the
    velocity and ignores air resistance

47
Escape Speed, General
  • The Earths result can be extended to any planet
  • The table at right gives some escape speeds from
    various objects

48
Escape Speed, Implications
  • This explains why some planets have atmospheres
    and others do not
  • Lighter molecules have higher average speeds and
    are more likely to reach escape speeds
  • This also explains the composition of the
    atmosphere

49
Black Holes
  • A black hole is the remains of a star that has
    collapsed under its own gravitational force
  • The escape speed for a black hole is very large
    due to the concentration of a large mass into a
    sphere of very small radius
  • If the escape speed exceeds the speed of light,
    radiation cannot escape and it appears black

50
Exercises of Chapter 11
  • 6, 9, 10, 14, 17, 18, 28, 31, 48, 59
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