useful for physisc

166
r m1 m2 F F G-1 Gravity Newton's Universal Law of Gravitation (first stated by Newton): any two masses m 1 and m 2 exert an attractive gravitational force on each other according to This applies to all masses, not just big ones. G = universal constant of gravitation = 6.67 10 –11 N m 2 / kg 2 (G is very small, so it is very difficult to measure!) Don't confuse G with g: "Big G" and "little g" are totally different things. Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.] Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this. Example: Force of attraction between two humans. 2 people with masses m 1 m 2 70 kg, distance r = 1 m apart. 1/21/2022 University of Colorado at Boulder

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Page 1: Useful for Physisc

r

m1

m2F F

G-1

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 2: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-2

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 3: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-3

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 4: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-4

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 5: Useful for Physisc

M

m

r

v

period T

G-5

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 6: Useful for Physisc

G-6

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 7: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-7

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 8: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-8

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 9: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-9

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 10: Useful for Physisc

r

m1

m2F F

G-10

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 11: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-11

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 12: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-12

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 13: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-13

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 14: Useful for Physisc

M

m

r

v

period T

G-14

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 15: Useful for Physisc

G-15

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 16: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-16

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 17: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-17

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 18: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-18

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 19: Useful for Physisc

r

m1

m2F F

G-19

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 20: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-20

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 21: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-21

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 22: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-22

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 23: Useful for Physisc

M

m

r

v

period T

G-23

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 24: Useful for Physisc

G-24

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 25: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-25

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 26: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-26

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 27: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-27

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 28: Useful for Physisc

r

m1

m2F F

G-28

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 29: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-29

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 30: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-30

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 31: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-31

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 32: Useful for Physisc

M

m

r

v

period T

G-32

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 33: Useful for Physisc

G-33

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 34: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-34

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 35: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-35

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 36: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-36

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 37: Useful for Physisc

r

m1

m2F F

G-37

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 38: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-38

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 39: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-39

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 40: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-40

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 41: Useful for Physisc

M

m

r

v

period T

G-41

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 42: Useful for Physisc

G-42

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 43: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-43

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 44: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-44

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 45: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-45

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 46: Useful for Physisc

r

m1

m2F F

G-46

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 47: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-47

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 48: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-48

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 49: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-49

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 50: Useful for Physisc

M

m

r

v

period T

G-50

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 51: Useful for Physisc

G-51

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 52: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-52

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 53: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-53

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 54: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-54

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 55: Useful for Physisc

r

m1

m2F F

G-55

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 56: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-56

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 57: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-57

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 58: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-58

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 59: Useful for Physisc

M

m

r

v

period T

G-59

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 60: Useful for Physisc

G-60

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 61: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-61

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 62: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-62

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 63: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-63

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 64: Useful for Physisc

r

m1

m2F F

G-64

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 65: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-65

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 66: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-66

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 67: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-67

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 68: Useful for Physisc

M

m

r

v

period T

G-68

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 69: Useful for Physisc

G-69

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 70: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-70

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 71: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-71

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 72: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-72

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 73: Useful for Physisc

r

m1

m2F F

G-73

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 74: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-74

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 75: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-75

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 76: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-76

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 77: Useful for Physisc

M

m

r

v

period T

G-77

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 78: Useful for Physisc

G-78

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 79: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-79

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 80: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-80

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 81: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-81

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 82: Useful for Physisc

r

m1

m2F F

G-82

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 83: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-83

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 84: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-84

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 85: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-85

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 86: Useful for Physisc

M

m

r

v

period T

G-86

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 87: Useful for Physisc

G-87

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 88: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-88

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 89: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-89

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 90: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-90

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 91: Useful for Physisc

r

m1

m2F F

G-91

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 92: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-92

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 93: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-93

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 94: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-94

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 95: Useful for Physisc

M

m

r

v

period T

G-95

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 96: Useful for Physisc

G-96

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 97: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-97

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 98: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-98

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 99: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-99

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 100: Useful for Physisc

r

m1

m2F F

G-100

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 101: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-101

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 102: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-102

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 103: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-103

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 104: Useful for Physisc

M

m

r

v

period T

G-104

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 105: Useful for Physisc

G-105

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 106: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-106

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 107: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-107

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 108: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-108

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 109: Useful for Physisc

r

m1

m2F F

G-109

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 110: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-110

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 111: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-111

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 112: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-112

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 113: Useful for Physisc

M

m

r

v

period T

G-113

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 114: Useful for Physisc

G-114

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 115: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-115

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 116: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-116

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 117: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-117

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 118: Useful for Physisc

r

m1

m2F F

G-118

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 119: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-119

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 120: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-120

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 121: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-121

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 122: Useful for Physisc

M

m

r

v

period T

G-122

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 123: Useful for Physisc

G-123

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 124: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-124

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 125: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-125

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 126: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-126

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

Gravity

Newton's Universal Law of Gravitation (first stated by Newton): any two masses m1 and m2 exert an attractive gravitational force on each other according to

4/18/2023 University of Colorado at Boulder

Page 127: Useful for Physisc

r

m1

m2F F

G-127

This applies to all masses, not just big ones.

G = universal constant of gravitation = 6.67 10–11 N m2 / kg2 (G is very small, so it is very difficult to measure!)

Don't confuse G with g: "Big G" and "little g" are totally different things.

Newton showed that the force of gravity must act according to this rule in order to produce the observed motions of the planets around the sun, of the moon around the earth, and of projectiles near the earth. He then had the great insight to realize that this same force acts between all masses. [That gravity acts between all masses, even small ones, was experimentally verified in 1798 by Cavendish.]

Newton couldn't say why gravity acted this way, only how. Einstein (1915) General Theory of Relativity, explained why gravity acted like this.

Example: Force of attraction between two humans. 2 people with masses m1 m2 70 kg, distance r = 1 m apart.

This is a very tiny force! It is the weight of a mass of 3.4 10–5 gram. A hair weighs 210–3 grams – the force of gravity between two people talking is about 1/60 the weight of a single hair.

Computation of g

Important fact about the gravitational force from spherical masses: a spherical body exerts a gravitational force on surrounding bodies that is the same as if all the sphere's mass were concentrated at its center. This is difficult to prove (Newton worried about this for 20 years.)

4/18/2023 University of Colorado at Boulder

Page 128: Useful for Physisc

sphere, mass M

mass m

Fgrav

mass m

Fgrav (same as with sphere)point mass M

r

RE

mass ME

mass m, dropped near surface

Earth

G-128

We can now compute the acceleration of gravity g ! (Before, g was experimentally determined, and it was a mystery why g was the same for all masses.)

Fgrav = m a = m g

(since r = RE is distance from m to center of Earth)

m's cancel !

If you plug in the numbers for G, ME, and RE, you get g = 9.8 m/s2.

Newton's Theory explains why all objects near the Earth's surface fall with the same acceleration

(because the m's cancel in .) Newton's theory also makes a quantitative prediction for the value of g, which is correct.

Example: g on Planet X. Planet X has the same mass as earth (MX = ME) but has ½ the radius (RX = 0.5 RE). What is gx , the acceleration of gravity on planet X?

Planet X is denser than earth, so expect gx larger than g.

. Don't need values of G, ME, and RE!

Method II, set up a ratio:

4/18/2023 University of Colorado at Boulder

Page 129: Useful for Physisc

h

earth

v

Earth

Fgrav

Fgrav

N

astronaut

G-129

_________________ * __________________

At height h above the surface of the earth, g is less, since we are further from the surface, further from the earth's center.

r = RE + h

The space shuttle orbits earth at an altitude of about 200 mi 1.6 km/mi 320 km. Earth's radius is RE = 6380 km. So the space shuttle is only about 5% further from the earth's center than we are. If r is 5% larger, then r2 is about 10% larger, and

Astronauts on the shuttle experience almost the same Fgrav as when on earth. So why do we say the astronauts are weightless??

"Weightless" does not mean "no weight".

"Weightless" means "freefall" means the only force acting is gravity.

If you fall down an airless elevator shaft, you will feel exactly like the astronauts. You will be weightless, you will be in free-fall.

An astronaut falls toward the earth, as she moves forward, just as a bullet fired horizontally from a gun falls toward earth.

OrbitsConsider a planet like Earth, but with no air. Fire projectiles horizontally from a mountain top, with faster and faster initial speeds.

4/18/2023 University of Colorado at Boulder

Page 130: Useful for Physisc

orbits!

Planet

would go straight,if no gravity

Sun

Planet

Sslower

faster

same time intervals,same areas

G-130

The orbit of a satellite around the earth, or of a planet around the sun obeys Kepler's 3 Laws.

Kepler, German (1571-1630). Before Newton. Using observational data from Danish astronomer Tycho Brahe ("Bra-hay"), Kepler discovered that the orbits of the planets obey 3 rules.

KI : A planet's orbit is an ellipse with the Sun at one focus.

KII : A line drawn from planet P to sun S sweeps out equal areas in equal times.

KIII: For planets around the sun, the period T and the mean distance r from the sun are related

by . That is for any two planets A and B, . This means that planets further from the sun (larger r) have longer orbital periods (longer T).

Kepler's Laws were empirical rules, based on observations of the motions of the planets in the sky. Kepler had no theory to explain these rules.

4/18/2023 University of Colorado at Boulder

Page 131: Useful for Physisc

M

m

r

v

period T

G-131

Newton (1642-1727) started with Kepler's Laws and NII (Fnet = ma) and deduced that

. Newton applied similar reasoning to the motion of the Earth-Moon

system (and to an Earth-apple system) and deduced that .Newton then made a mental leap, and realized that this law applied to any 2 masses, not just to the Sun-planet, the Earth-moon, and Earth-projectile systems.

Starting with Fnet = ma and Fgrav = G Mm / r2, Newton was able to derive Kepler's Laws (and much more!). Newton could explain the motion of everything!

Derivation of KIII (for special case of circular orbits). Consider a small mass m in circular orbit about a large mass M, with orbital radius r and period T. We aim to show that T2 / r3 = const.

Start with NII: Fnet = m a

The only force acting is gravity, and for circular motion a = v2 / r

[recall the v = dist / time = 2r / T ]

( Deriving this result for elliptical orbits is much harder, but Newton did it. )

An extra result of this calculation is a formula for the speed v of a satellite in circular orbit:

. For low-earth orbit (few hundred miles up), this orbital speed is about 7.8 km/s 4.7 miles/second. The Space Shuttle must attain a speed of 4.7 mi/s when it reaches the top of the atmosphere (and it fuel has run out) or else it will fall back to Earth.

4/18/2023 University of Colorado at Boulder

Page 132: Useful for Physisc

G-132

Measurement of Big G

The value of G ("big G") was not known until 1798. In that year, Henry Cavendish (English) measured the very tiny Fgrav between 2 lead spheres, using a device called a torsion balance.

( If Fgrav, r, and m's known, can compute G.)

Before Cavendish's experiment, g and RE were known, so using , one could compute the product GME, but G and ME could not be determined separately.

With Cavendish's measurement of G, one could then compute ME. Hence, Cavendish "weighed the earth".

Gravitational Potential Energy

Previously, we showed that PEgrav = mgh. But to derive PE = mgh, we assumed that Fgrav = mg =

constant, which is only true near the surface of the Earth. In general,

(it depends on r). We now show that for the general case,

This is the gravitational potential for two masses, M and m, separated by a distance r. By

convention, the zero of gravitational potential energy is set at r = ∞. [ I will use the common

notation U(r) , instead of PE. ]

Recall the definition of PE: . Here, we have used the definition

of work for the case of 1D motion: .

4/18/2023 University of Colorado at Boulder

Page 133: Useful for Physisc

xx1

M m

0

Fgrav

dx∞

G-133

Consider a mass M at the origin and a mass m at position x1, as shown in the diagram. We

compute the work done by the force of gravity as the mass m moves from x = x1 to x = ∞.

The force F(x) on mass m is in the negative direction, so, indicating direction with a sign, we

have . Here, the work done by gravity is negative, since force and

displacement are in opposite directions:

From the definition of PE, . Calling the

initial position r (instead of x1), we have .

A slight notation change now: r is the radial distance from the origin, so r is always positive

(unlike x which can be positive or negative.) Plotting U(r) vs. r, we see a “gravitational potential

well”.

4/18/2023 University of Colorado at Boulder

Page 134: Useful for Physisc

r r

U(r) r = 0 U(r)

r

The "Potential Well"

rU(r)

r = Rearth

h = r Rearth

U = mgh

U(h)

G-134

Recall that negative potential energy simply means less energy than the zero of energy.

Question: How is PE = mgh a special case of U(r) = GMm/r ?

Escape Speed vescape

Throw a rock away from an (airless) planet with a speed v. If v < vescape , the rock will rise to a maximum height and then fall back down. If v > vescape , the rock will go to r = ∞ , and will still have some speed left over and be moving away from the planet. If v = vescape , the rock will have just enough initial KE to escape the planet: its distance goes to r = ∞ at the same time its speed approaches zero: v 0 as r ∞.

We can use conservation of energy to compute the escape speed vesc (often called , incorrectly, the "escape velocity" ).

4/18/2023 University of Colorado at Boulder

Page 135: Useful for Physisc

r

U(r)

KE

Etot = KE+PE

PE

G-135

Initial configuration: r = R (surface of planet), v = vesc. Final configuration: r = ∞ , v = 0.

Notice that

If the rock is thrown with speed v > vesc , it will go to r = ∞, and will have some KE left over, vfinal > 0.

4/18/2023 University of Colorado at Boulder