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1 Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley PowerPoint ® Lectures for University Physics, Twelfth Edition – Hugh D. Young and Roger A. Freedman Lectures by James Pazun Chapter 12 Gravitation Modified by P. Lam 6_13_2011 Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley Goals for Chapter 12 To study Newtons Law of Gravitation Use Newtons Law of Gravitation and Newtons Second Law of Motion (F=ma) to calculate orbital speed of satellites and planets Use energy method to determine escape velocityUse Newtons Law of Gravitation and Newtons Second Law of Motion to explain Keplers Laws of planetary motion Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley Newtons Law of Gravitation The gravitational force is always attractive and its magnitude depends on both the masses of the bodies involved and their separations. ! F g = Gm 1 m 2 r 2 G = 6.6742 x10 "11 N m 2 / kg 2 Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley Superposition principle The total force on m1= force on m1 by m2 + force on m1 by m3 m1 m2 m3 Find ! F 1 , ! F 2 and the net force ! F Express the forces in ˆ i , ˆ j .

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  • 1

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    PowerPoint® Lectures for University Physics, Twelfth Edition – Hugh D. Young and Roger A. Freedman

    Lectures by James Pazun

    Chapter 12

    Gravitation

    Modified by P. Lam 6_13_2011 Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Goals for Chapter 12

    •  To study Newton’s Law of Gravitation

    •  Use Newton’s Law of Gravitation and Newton’s Second Law of Motion (F=ma) to calculate orbital speed of satellites and planets

    •  Use energy method to determine “escape velocity”

    •  Use Newton’s Law of Gravitation and Newton’s Second Law of Motion to explain Kepler’s Laws of planetary motion

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Newton’s Law of Gravitation

    •  The gravitational force is always attractive and its magnitude depends on both the masses of the bodies involved and their separations.

    !

    ! F g =

    Gm1m2

    r2

    G = 6.6742x10"11

    N • m2/kg

    2

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Superposition principle

    •  The total force on m1= force on m1 by m2 + force on m1 by m3

    m1 m2

    m3

    !

    Find ! F 1,! F 2and the net force

    ! F

    Express the forces in ˆ i , ̂ j .

  • 2

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Compare little “g” with big “G”

    Consider the gravitational force on a mass (m) by the Earth:

    F =GmME

    r2=ma

    ! a =GME

    r2

    Near Earth's surface ! r~RE

    ! a =GME

    RE2" 9.8

    m

    s2

    #

    $%&

    '(= g (free) fall acelleration)

    The magnitude of "g" decreases as the object gets

    further away from the Earth.

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Satellite motion

    Orbital motion = projectile motion with very large initial velocity How large an initial velocity is required? Answer on next slide

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Calculate satellite orbits - assume circular orbit

    !

    This example consider satellite around the Earth

    (but the same method applies to motion of satellite around

    any large mass even for a planet around the Sun)

    (1) Draw free diagram on the satellite

    (2) Set up Newton's 2nd Law F = ma equation (a = v2 /r)

    " F = mv

    2

    r

    (3) Apply Newton's Law of Gravitaion : F =GmM

    E

    r2

    (4) Combine "GmM

    E

    r2

    = mv

    2

    r

    (5) Solve for v in terms of r

    " v =GME

    r

    For an orbit near the surface of the Earth

    (r # RE = 6.4x106m),

    v # 8x103m /s ~ 18,000mi /h

    m

    ME

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Calculate planetary orbits - assume circular orbit

    mp

    MS

    !

    GmpMS

    r2

    = mpv

    2

    r

    v2 =GMS

    r

    v =2"r

    T; T = orbital period

    #2"r

    T

    $

    % &

    '

    ( )

    2

    =GMS

    r

    #r

    3

    T2

    =GMS

    4" 2= same number for all

    planets in the solar system.

    (This called Kepler's 3rd Law)

  • 3

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Gravitational potential energy

    !

    The expression for the gravitaitonal

    potential energy for a mass at height

    h from the surface of the Earth :

    U = mgh is only valid for an object

    near the surface of the Earth.

    The more general expression is :

    U = " GmME

    r= potential energy for the

    mass - Earth system separated by a distance of r.

    Near the surface of the Earth r = RE + h

    U(RE + h) "U(RE ) = "GmME

    RE + h

    #

    $ %

    &

    ' ( " "

    GmME

    RE

    #

    $ %

    &

    ' ( ) m

    GME

    RE2h = mgh

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Calculate escape velocity

    •  What is the minimum initial velocity of a rocket for it to escape from the gravitational effect of the Earth?

    !

    Ki +Ui = K f +Uf

    1

    2mvi

    2+1

    2MEVi

    2"GmME

    RE= 0 +

    1

    2MEVf

    2"GmME

    #

    Vf $Vi

    %1

    2mvi

    2"GmME

    RE= 0

    % vi =2GME

    RE& 25,300mi /h

    !

    Note : If a star is very dense such that it has a large mass

    but a small radius, then vescape > speed of light!!

    Such a star is a "black hole".

    However, correct treatment of black hole requires

    Einstein's theory of Gravitation (General Relativity).

    Newton's theory of graviation is only approximate.

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Newton’s Law of gravitation

    How did Newton come up with the Law of Gravitation?

    !

    ! F =

    Gm1m2

    r2

    Newton relied on the astronomical data of Kepler.

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Kepler’s laws for planetary motion

    •  1st Law: Each planet moves in an elliptical orbit with the sun at one of the foci

    •  2nd Law: A line connecting the sun to a given planet sweeps out equal areas in equal times.

    •  3rd Law: The periods of the planets are proportional to the 3/2 powers of the major axis lengths in their orbits. (Planets further away from the Sun takes longer to go around the Sun)

  • 4

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Kepler’s 1st Law - elliptical orbits

    Elliptical orbits are consequence of the 1/r2 dependence of the gravitational force.

    The proof requires advanced calculus.

    Circular orbit is a special case of elliptical orbit.

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Kepler’s 2rd Law - Conservation of angular momentum • 2nd Law: A line connecting the sun to a given planet sweeps out equal areas in equal times => a planet moves faster when it is closer to the sun.

    !

    Kepler's 2nd Law : dA

    dt= constant

    Relate dA

    dt to angular momentum (

    ! L ) of the planet about the Sun

    dA

    dt=

    1

    2

    ! r "! v =

    1

    2m

    ! r "m

    ! v =

    ! L

    2m

    dA

    dt= constant #

    ! L = constant # small r means larger v.

    ! L = constant when torque = 0.

    Newtons concluded that the gravitaional force must be directed

    along the "radius" from the Sun to the planet.

    Since ! F and

    ! r are along the same direction,

    ! r "! F = 0.

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Kepler’s 3rd Law and Newton’s Law of Gravitation

    !

    Derived in an earlier slide, repeat here :

    Newton's 2nd Law : F = ma = mpv2

    r

    Newton's Law of gravitation : F =GmpMS

    r2

    = mpv2

    r

    " v2 =GM

    S

    r

    Assume circular orbit " v =2#r

    T, T = orbital period

    "2#r

    T

    $

    % &

    '

    ( )

    2

    =GM

    S

    r

    " T =(2# )r3 / 2

    GMS

    * r3 / 2 (Kepler's 3rd Law)

    Newton did this backward, he started with Kepler's 3rd Law and

    deduce his law of gravitaiton.

    Note : We can use Kepler's 3rd law to calculate the mass of the Sun

    based on the radius and the period of the Earth's orbit around the Sun.

    Copyright © 2008 Pearson Education Inc., publishing as Pearson Addison-Wesley

    Sun and planet revolve about the center of mass.

    We have assumed the Sun was stationary while the planet orbits around the Sun.

    In fact, a better way to view their motion is that they both revolve about their center of mass.