+ All Categories
Home > Documents > Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton ry/newtongrav.html.

Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton ry/newtongrav.html.

Date post: 27-Mar-2015
Category:
Upload: trinity-ramos
View: 228 times
Download: 2 times
Share this document with a friend
Popular Tags:
132
Chapter 4 Gravitation Physics Beyond 2000
Transcript
Page 1: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Chapter 4 Gravitation

Physics Beyond 2000

Page 2: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravity

• Newton

• http://csep10.phys.utk.edu/astr161/lect/history/newtongrav.html

• http://www.britannica.com/bcom/eb/article/9/0,5716,109169+2+106265,00.html

• http://www.nelsonitp.com/physics/guide/pages/gravity/g1.html

Page 3: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravity

• The moon is performing circular motion round the earth.

• The centripetal force comes from the gravity.

Fc

earthmoon

v

Page 4: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravity

• Newton found that the gravity on the moon is the same force making an apple fall.

W

Ground

Page 5: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Newton’s Law of Gravitation

• Objects attract each other with gravitational force.• In the diagram,

m1 and m2 are the masses of the objects and r is the distance between them.

m1 m2

F F

r

Page 6: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Newton’s Law of Gravitation

• Every particle of matter attracts every other particle with a force whose magnitude is

m1 m2

F F

r

221.

r

mmGF G is a universal constant

G = 6.67 10-11 m3kg-1s-2

Note that the law applies to particles only.

Page 7: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 1

• Find how small the gravitation is.

Page 8: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Shell Theorem

• Extends the formula

to spherical objects like a ball, the earth, the sun and all planets.

221.

r

mmGF

Page 9: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Theorem 1a. Outside a uniform spherical shell.• The shell attracts the external particle as if a

ll the shell’s mass were concentrated at its centre.

221.

r

mmGF

F F

r

m1m2O

Page 10: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Theorem 1b. Outside a uniform sphere.

• The sphere attracts the external particle as if all the sphere’s mass were concentrated at its centre.

221.

r

mmGF

F F

r

m1m2O

Page 11: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 2 Outside a uniform sphere.

• The earth is almost a uniform sphere.

221.

r

mmGF

F

r

m1 m2O

earth

F

Page 12: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Theorem 2a. Inside a uniform spherical shell.

• The net gravitational force is zero on an object inside a uniform shell.

m2

m1

The two forceson m2 cancel.

Page 13: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Theorem 2b. Inside a uniform sphere.

221.

r

mmGF

m2m1

r

F

where m1 is the mass of the corewith r the distance from the centre to the mass m2

Page 14: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 3

• Inside a uniform sphere.

m2m1

r

F

Page 15: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational Field

• A gravitational field is a region in which any mass will experience a gravitational force.

• A uniform gravitational field is a field in which the gravitational force in independent of the position.

• http://saturn.vcu.edu/~rgowdy/mod/g33/s.htm

Page 16: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field strength, g

• The gravitational field strength, g, is the gravitational force per unit mass on a test mass.

test massF

m

m

Fg

F is the gravitational force

m is the mass of the test mass

g is a vector, in the same direction of F.SI unit of g is Nkg-1.

Page 17: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field strength, g

• The gravitational field strength, g, is the gravitational force per unit mass on a test mass.

test massF

m

m

Fg

F is the gravitational force

m is the mass of the test mass

SI unit of g isNkg-1.

Page 18: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field strength, g, outside an isolated sphere of mass M

• The gravitational field strength, g, outside an isolated sphere of mass M is

2r

GMg

Prove it by placing a test mass m at a point X with distance r from the centre of the isolated sphere M.

M r

field strengthat X

XO

Page 19: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 4

• The field strength of the earth at the position of the moon.

Page 20: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field strength, g

• Unit of g is Nkg-1.

• g is also a measure of the acceleration of the test mass.

• g is also the acceleration due to gravity, unit is ms-2.

Page 21: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field strength, g

• Field strength, g.

• Unit Nkg-1.

• A measure of the strength of the gravitational field.

• Acceleration due to gravity, g.

• Unit ms-2.• A description of

the motion of a test mass in free fall.

Page 22: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field lines

• We can represent the field strength by drawing field lines.

• The field lines for a planet are radially inward.

Radial fieldplanet

Page 23: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field lines

• We can represent the field strength by drawing field lines.

• The field lines for a uniform field are parallel.

Uniform field

earth’s surface

Page 24: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field lines

• The density of the field lines indicates the relative field strength.

g1= 10 Nkg-1 g2= 5 Nkg-1

Page 25: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Field lines

• The arrow and the tangent to the field lines indicates the direction of the force acting on the test mass.

test mass

direction of the force

Page 26: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

The earth’s gravitational field

• Mass of the earth Me 5.98 1024 kg

• Radius of the earth Re 6.37 106 m

Re

O

Page 27: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravity on the earth’s surface, go

• The gravitational field go near the earth’s surface is uniform and

2e

eo R

GMg

The value of go 9.8 Nkg-1

Page 28: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 5

• The gravity on the earth’s surface, go.

Page 29: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight

• Use a spring-balance to measure the weight of a body.

• Depending on the case, the measured weight R (the apparent weight) is not equal to the gravitational force mgo.

R

mgo

Page 30: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight

• The reading on the spring-balance is affected by the following factors:

1. The density of the earth crust is not uniform.

2. The earth is not a perfect sphere.

3. The earth is rotating.

Page 31: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight

1.The density of the earth crust is not uniform.

• Places have different density underneath. Thus the gravitational force is not uniform.

Page 32: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight

2. The earth is not a perfect sphere.

Points at the poles are closer to the centre than points on the equators.

rpole < requator

gpole > gequator N-pole

S-pole

Equator

Page 33: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight

3. The earth is rotating. Except at the pole, all

points on earth are performing circular motion with the same angular velocity . However the radii of the circles may be different.

X

Y

Page 34: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight

3. The earth is rotating. Consider a mass m is at p

oint X with latitude .

The radius of the circle is r = Re.cos .

X

rRe

m

O

Y

Page 35: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight

3. The earth is rotating. The net force on the mass

m must be equal to the centripetal force.

X

rRe

m

2mrFF cnet cos... 2

eRm

O

YFc

Note that Fnet points to Y.

Page 36: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight R

3. The earth is rotating. The net force on the mass m

must be equal to the centripetal force.

So the apparent weight (normal reaction) R does not cancel the gravitational force mgo.

X

r m

O

YFc

R

mgo

co FgmR

Page 37: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent Weight R

3. The earth is rotating. The apparent weight R is

not equal to the gravitational force mgo in magnitude.

X

r m

O

YFc

R

mgo

co FgmR

Page 38: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent weight R on the equator

2eo mRRmg 2eo mRmgR

emgThe apparent field strengthon the equator is

2eoe Rgg

mgo R

Page 39: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent weight R at the poles

0 Rmgo

omgR pmg

The apparent field strengthat the poles is

op gg

mgo

R

Page 40: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 6

• Compare the apparent weights.

Page 41: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Apparent weight at latitude

X

r m

O

YFc

R

mgo

2mrFF cnet cos... 2

eRm

co FgmR

Note that the apparent weight Ris not exactly along the line throughthe centre of the earth.

Page 42: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Outside the earth at height h.

h = height of the mass m from the earth’s surface

r m

hRe

Meg

O

Page 43: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Outside the earth at height h.

r m

hRe

Meg

O

2

22

2

).(

).(

r

Rg

r

R

R

GMr

GMg

eo

e

e

e

e

where go is the field strength on the earth’s surface.

2

1

rg

Page 44: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Outside the earth at height h.

r m

hRe

Meg

O

where go is the field strength on the earth’ssurface.

2

2

)1.(

).(

eo

e

eo

R

hg

hR

Rgg

Page 45: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Outside the earth at height h close to the earth’s surface. h<<Re.

r m

hRe

Meg

O

where go is the field strength on the earth’ssurface.

)2

1.(e

o R

hgg

ee R

h

R

h 21)1( 2

Page 46: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Below the earth’s surface.

Re

rO d

Me

g

Only the core withcolour gives thegravitational force.

r = Re-d

Page 47: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Below the earth’s surface.

Re

rO d

Me

g

Find the mass Mr of

3)(e

er R

rMM

r = Re-d

Page 48: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Below the earth’s surface.

Re

rO d

Me

g 32

2

)(e

e

r

R

r

r

GMr

GMg

r = Re-d

Page 49: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

• Below the earth’s surface.

Re

rO d

Me

g )1(

)(2

eo

ee

e

R

dg

R

r

R

GMg

r = Re-dg r

Page 50: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Variation of g with height and depth

earth

ggo

0r distance from the centreof the earthRe

1. r < Re , g r.

2. r > Re , 2

1

rg

Page 51: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential energy Up

• Object inside a gravitational field has gravitational potential energy.• When object falls towards the earth, it gains kinetic energy and

loses gravitational potential energy.

This objectpossesses Up

earth

Page 52: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Zero potential energy

• By convention, the gravitational potential energy of the object is zero when its separation x from the centre of the earth is .

Up = 0earth

x O

Page 53: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Negative potential energy

• For separation less than r, the gravitational potential energy of the object is less than zero. So it is negative.

Up < 0earth

O r

Page 54: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential energy Up

• Definition 1

• It is the negative of the work done by the gravitational force FG as the object moves from infinity to that point.

earth

O r

FG

dx

Page 55: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential energy Up

• Definition 1

earth

O r

FG

dx

WU p

Page 56: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential energy Up

• Definition 2

• It is the negative of the work done by the external force F to bring the object from that point to infinity.

earth

O r

F

dx

Me

m

Page 57: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential energy Up

• Definition 2

earth

O r

F

dx

r

P dxFU .

Me

m

Page 58: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential energy Up

2x

mGMFFrom e

r

mGMU eP

earth

O r

Me

m

Page 59: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 7

• Conservation of kinetic and gravitational potential energy.

Page 60: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 8

• - Work done

= gravitational potential energy

Page 61: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 9

• Two particles are each in the other’s gravitational field.

• Thus each particle possesses gravitational energy.

Page 62: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

System of three particles• Each particle is in another two particles’

gravitational fields.

• Each particle possesses gravitational potential energy due to the other two particles.

m

M1 M2

r1r2

Up of

2

2

1

1

r

GmM

r

GmM

Page 63: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

System of three particlesUp of

Up of

m

M1 M2

r1r2

r3

2

2

3

12

r

GmM

r

MGM

1

1

3

12

r

GmM

r

MGM

Page 64: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Example 10

• Up of the moon due to the earth’s gravitational field.

r

earth

moon

What is the Up of the earth due to the moon’s gravitational field?

Page 65: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

• Escape speed ve is the minimum projection speed required for any object to escape from the surface of a planet without return.

ve

Page 66: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

• Escape speed ve is the minimum projection speed required for any object to escape from the surface of a planet without return.

ve

Page 67: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

• On the surface of the planet, the body possesses both kinetic energy Uk and gravitational potential energy Up.

veR

mM

Uk

2

2

1emv

UP

R

GMm

Page 68: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

• If the body is able to escape away, it means the body still possesses kinetic energy at infinity.

• Note that the gravitational energy of the body at infinity is zero.

veR

mM

Page 69: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

veR

mM

• If there is not any loss of energy on projection,

the total energy of the body at lift-off

= the total energy of the body at infinity

Page 70: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

veR

mM

)(2

1 2

r

GMmmve = kinetic energy at infinity

≧0

Page 71: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

veR

mM

RgR

GMv o2

2where go is the gravitational acceleration on the surfaceof the earth.

Page 72: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

veR

mM

RgR

GMv oe 2

2

So the escape speed from earth is

Page 73: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Escape speed ve

veR

mM

Example: Find ve

Page 74: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential V

• Definition: The gravitational potential at a point is the

gravitational potential energy per unit test mass.

m

UV

where U is the gravitational potential energy of a mass m at the point

Page 75: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential V

• Definition: The gravitational potential at a point is the

gravitational potential energy per unit test mass.

m

UV unit of V is J kg-1

Page 76: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Gravitational potential V

• Example 12 – to find the change in gravitational potential energy.

• ΔU = U – Uo

• If ΔU >0, there is a gain in U.

• If ΔU <0, there is a loss in U.

Page 77: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Equipotentials

• Equipotentials are lines or surfaces on which all points have the same potential.

• The equipotentials are always perpendicular to the field lines.

Page 78: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Equipotentials• The equipotentials around the earth are ima

ginary spherical shells centered at the earth’s centre.

Page 79: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Equipotentials• The field is radial.

Page 80: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Equipotentials• The equipotentials near the earth’s surface a

re parallel and evenly spaced surface.

• The field is uniform.

surface

Page 81: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Equipotentials

• Example 13 – Earth’s equipotential.

Page 82: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Potential V and field strength g

dr

dVg

rr

MGV

2r

GMg

Page 83: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Potential V and field strength g

rr

MGV

2r

GMg

If we consider the magnitude of g only,

dr

dVg

Page 84: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

• http://tycho.usno.navy.mil/vphase.html• The potential is the sum of the potentials due to the earth and the moon.

earth

moonP

D

r

D-r

Me

Mm

Page 85: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

earth

moonP

D

r

D-r

Me

Mm

rD

GM

r

GMV meP

Page 86: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

earth

moon

r

V

0

Page 87: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

earth

moon

r

V

0

dr

dVg

Page 88: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

earth

moon

r

V

0

dr

dVg

g

Page 89: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

earth

moon

r

V

0g=0

g = 0 at a point X between the earthand the moon. X is a neutral point.

X

Page 90: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

earth

moon

r

V

0

g>0

g points to the centre of the earth if it is positive.

X

Page 91: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

earth

moon

r

V

0g<0

g points to the centre of the moon if it is negative.

X

Page 92: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon systemGiven: Me = 5.98 × 1024 kg Mm = 7.35 × 1022 kg D = 3.84 × 108 m G = 6.67 × 10-11 Nm2kg-2

Find: the position X at which g = 0.

earth

moon

X

x

Hint: 0dr

dVg

Page 93: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon systemGiven: Me = 5.98 × 1024 kg Mm = 7.35 × 1022 kg D = 3.84 × 108 m G = 6.67 × 10-11 Nm2kg-2

Find: the position X at which g = 0.

earth

moon

X

x

Answer: x = 3.46 × 108 m

Page 94: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Earth-moon system

• Example 14 – potential difference near the earth’s surface.

Page 95: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion• The description of the motion of a planet

round the sun.

sun

Page 96: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion• Kepler’s law:

1. The law of orbits.

All planets move in elliptical orbits, with the sun at one focus.

sun

Page 97: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion• Kepler’s law:

2. The law of areas.

The area swept out in a given time by the line joining any planet to the sun is always the same.

sun

Page 98: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion• Kepler’s law:

3. The law of periods.

The square of the period T of any planet about the sun is proportional to the cube of their mean distance r from the sun.

sun 32 rT

Page 99: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion

• Basically, we only study the simple case of circular orbit.

r

Page 100: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motionA satellite of mass m performs circular motion round the earth with speed vc .The radius of the orbit is r.

r

satellite

earth

vc

Page 101: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion

The centripetal force is provided by the gravitational force.

r

satellite

earth

vc

Fc

Page 102: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion

Show that

r

satellite

earth

vc

Fc

r

GMv ec where Me is the

mass of the earth

Page 103: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Orbital motion

• Example 15 – find the speed of a satellite.

r

satellite

earth

vc

Page 104: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Proof of Kepler’s 3rd law in a circular orbit

32 rT

r1

satellite 1

earth

vc1

r2satellite 2

vc2

Page 105: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Proof of Kepler’s 3rd law in a circular orbit

r1

satellite 1

earth

vc1

r2satellite 2

vc2

Note that the proof is true for satellites round the same planet.

Page 106: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Kepler’s 3rd law

• Example 16 – apply Kepler’s 3rd law.

Page 107: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Satellites

• Natural satellites – e.g. moon.

• Artificial satellites –

e.g. communication satellites,

weather satellites.

http://weather.yahoo.com/graphics/satellite/US.html

http://www.smgaels.org/physics/97/MGRAHLFS.HTM

Page 108: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Geosynchronous satellites

• A geosynchronous satellite is above the earth’s equator.

• It rotates about the earth with the same angular speed as the earth and in the same direction.

• It seems stationary by observers on earth.

Page 109: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Geosynchronous satellites

ω

equator

axis

satellite

h

Re

Page 110: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Geosynchronous satellitesFind the radius of the orbit of a geosynchornoussatellite.

ω

equator

axis

satelliteh Re

rs

h + Re = rs

Page 111: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Geosynchronous satellites

rs = 4.23×107 m

ω

equator

axis

satelliteh Re

r

h + Re = rs

Page 112: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Geosynchronous satellites

h = 3.59×107 m

ω

equator

axis

satelliteh Re

r

h + Re = rs

Page 113: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Parking OrbitNote that there is only one such orbit.It is called a parking orbit.

ω

equator

axis

satelliteh Re

r

h + Re = rs

Page 114: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Satellites Near the Earth’s surface

• Assume that the orbit is circular with radius r Re , the radius of the earth.

• The gravitational field strength go is almost a constant (9.8 N kg-1).

• The gravitational force provides the required centripetal force.

Page 115: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Satellites Near the Earth’s surface

r Re satellite

earth

vr

Find vr

Page 116: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion

• Find v and the kinetic energy Uk of the satellite.

r

satellite

earth Me

v

m

Page 117: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion• The satellite in the orbit possesses both

kinetic energy and gravitational energy.

r

satellite

earth Me

v

m

Page 118: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion

r

satellite

earth Me

v

m

r

GMv e2

r

mGMU ek 2

Note that Uk > 0

Page 119: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion

• Find Up the gravitational potential of the satellite.

r

satellite

earth Me

v

m

Page 120: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion

r

satellite

earth Me

v

mr

mGMU ep

Note that Up < 0

Page 121: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion

r

satellite

earth Me

v

m

Find U, the total energy of the satellite.

Page 122: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion

r

satellite

earth Me

v

m

r

mGMUUU epk 2

Note that U < 0

Page 123: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Energy and Satellite Motion

r

satellite

earth Me

v

m

U : Up : Uk = -1 : -2 : 1

Page 124: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Falling to the earth

r

satellite

earth Me

v

m

The satellite may lose energy due to airresistance. The total energy becomes more negative and r becomes less.

r

mGMU e

2

Page 125: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Falling to the earth

r

satellite

earth Me

v

m

The satellite follows a spiral path towardsthe earth.

r

mGMU e

2

Page 126: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Falling to the earth

r

satellite

earth Me

v

m

As r decreases, the kinetic energy of the satellite increases and the satellite moves faster.

r

mGMU ek 2

Page 127: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Falling to the earth

Example 17 – Loss of energy

Page 128: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Weightlessness in spacecraft

mg

vv

The astronaut is weightless.

Page 129: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Weightlessness in spacecraft

• We fell our weight because there is normal reaction on us.

mg

Normal reaction

ground

Page 130: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Weightlessness in spacecraft

• If there is not any normal reaction on us, we feel weightless. e.g. free falling

mg

Page 131: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Weightlessness in spacecraft

v

mg The gravitational forcemg on the astronaut isthe required centripetalforce. He does not requireany normal reaction toact on him.

Page 132: Chapter 4 Gravitation Physics Beyond 2000 Gravity Newton  ry/newtongrav.html.

Weightlessness in spacecraft

v

mg

The astronaut isweightless.

http://www.nasm.edu/galleries/gal109/NEWHTF/HTF611A.HTM


Recommended