Transcript Physics 117

Physics 117
Chapter 4
A brief history of astronomy
and
Gravity
Summary of the previous
lecture
• Motions in space: decompose them along the three spatial dimension
• Circular motion at constant speed:
• non-zero acceleration due to change in direction
• acceleration points toward the center
• F=mv2/r=m2r
where =2/T=v/r=rotational speed T=period of revolution
• Projectile motion: typical example of decomposition
• vx=(vx)initial=const
• vy =(vy)initial-gt
• Extended object when launched rotates around their center of mass meanwhile
it translates in space
• Torque: =r·F
Extra Ex. Ch.3: 13,17,25
Pag. 76
Babylonian cosmology
In Mesopotamia developed the most ancient civilization (2300-1600 B.C.)
and with it the most ancient cosmology.
The Earth was a flat disk surrounded by a river beyond which there were
high mountains which were supporting the sky. This was made of heavy iron
(siderurgy from Latin word siderus=iron sidera=sky). There was a tunnel
inside the mountains linking a door in the east to one in the west. It was used
by the sun in is cyclic motion.
Egyptian cosmology
For the ancient Egyptians the sky was a roof placed over the word and
supported by four columns placed at the four cardinal points. The Earth was a
rectangle, longer from north to south whose surface was bulgy and having at
the center the river Nile (obviously!). The stars were suspended from the sky
by strong cables.
An interesting creation myth is
that the goddess of the nigh,
Nuit, and her husband, Sibu,
the earth god, where separated
suddenly by the god Shu. She
was drag up in the sky and he
was frozen on earth. So the
earth is contorted and the night
sky lies above it.
Ancient Greek cosmology
Early physics
Eratosthenes
276-197 B.C.
The geocentric system
 All the ancient civilizations considered natural
to put the Earth at the center of the universe.
This vision was inherited by western Europe via
the ideas of the ancient Greeks.
 Aristotle: the Earth was the center of the universe and
the Sun and the other planets had to revolve around it in
perfect geometrical figures, circles. Later on (circa 150
A.D.) problems with variable motion of planets induced
Ptolemy to add epicyclical motion to planets.
Ptolemy
Copernicus and the heliocentric
universe
Nicolaus Copernicus (1473-1543):
Simplified explanation of planets’
motion via an heliocentric system
and simple circular orbits of
constant speed (uniform circular
motion)
The crisis of the Copernican paradigm
and the new astronomy of Kepler
Johannes Kepler (1571-1630) was a convinced Copernican
but studying new observations on the motion of Mars he
realized that they were not compatible with the
Copernican system.
After several years he realized that the only way to
conciliate the Copernican system with observation was to
abandon the idea of perfectly circular orbits.
This lead him to discovers the three laws of planetary
motions now called Kepler’s laws.
Kepler’s three laws
1.
2.
3.
Planets moves along elliptical paths with the sun at one focus of the ellipse
During a given interval of time a line drawn from the planet to the sun
sweeps out an equal area anywhere along its path
If T is the sidereal period of a planet (the time for a complete orbital
revolution) and Rm is the mean radius of the orbit of the planet then
T2=K(Rm)3
with K equal for all the planets of the solar system
Graphical representation of Kepler’s first law
Graphical representation of Kepler’s second law
Projectiles and Planets
The legend is that Newton saw an apple fall in his garden in Lincolnshire, thought of it in terms of an
attractive gravitational force towards the earth, and realized the same force might extend as far as
the moon. He was familiar with Galileo's work on projectiles, and suggested that the moon's motion
in orbit could be understood as a natural extension of that theory.
To see what is meant by this, consider a gun shooting a projectile horizontally from a very high
mountain, and imagine using more and more powder in successive shots to drive the projectile faster
and faster. The parabolic paths would become flatter and flatter, and, if we imagine that the
mountain is so high that air resistance can be ignored, and the gun is sufficiently powerful, eventually
the point of landing is so far away that we must consider the curvature of the earth in finding where it
lands.
In fact, the real situation is more dramatic---the earth's curvature may mean
the projectile never lands at all. This was envisioned by Newton in the
Principia.
Projectiles and Planets:
a never ending fall
The following diagram is from his later popularization,
A Treatise of the System of the World, written in the 1680's:
The mountaintop at V is supposed to be above the earth's atmosphere, and for a suitable initial
speed, the projectile orbits the earth in a circular path. In fact, the earth's curvature is such that the
surface falls away below a truly flat horizontal line by about five meters in 8,000 meters (five miles).
Recall that five meters is just the vertical distance an initially horizontally moving projectile will fall
in the first second of motion. But this implies that if the (horizontal) muzzle velocity were 8,000
meters per second, the downward fall of the cannonball would be just matched by the earth's surface
falling away, and it would never hit the ground!
[This is just the motion, familiar to us now, of a satellite in a low orbit, which travels at about 8,000
meters (five miles) a second, or 18,000 miles per hour. ]
Newton realized that the moon's circular path around the earth could be caused in this
way by the same gravitational force that would hold such a cannonball in low orbit, in
other words, the same force that causes bodies to fall.
Tides
The tides vary along the shores of the oceans of the earth with
a period of about 12.5 hours. Curiously, the circadian
rhythm period of 25 hours, corresponding to two tidal
periods, subconsciously affects a large variety of animal life,
including humans.
Tides are due to the gravitational attraction of moon and to
a lesser extent, the sun on the Earth. Because the moon is
closer to the Earth than the sun, it has a larger effect and
causes the Earth to bulge toward the moon. At the same
time, a bulge occurs on the opposite side of the Earth due to
inertial forces
Mt. St. Michel on the north coast of France
at low tide (up) and high tide (down).
The water surrounding this island is the Gulf
of Saint-Malo.
High and low tides
These bulges remain stationary while Earth rotates. The tidal bulges result in a rhythmic rise and fall
of ocean surface, which is not noticeable to someone on a boat at sea, but is magnified along the coasts.
Usually there are two high tides and two low tides each day, and thus a variation in sea level as the
tidal bulge passes through each point on the Earth's surface.
Because the Sun also exerts a gravitational
attraction on the Earth, there are also monthly
tidal cycles that are controlled by the relative
position of the sun and moon.
The highest high tides occur when the Sun and
the moon are on the same side of the Earth
(new moon) or on opposite sides of the Earth
(full moon). The lowest high tides occur when
the Sun and the moon are not opposed relative
to the Earth (quarter moons).
Gravitational locking
The tidal bulges are not aligned with the Earth-Moon direction, due to the
rotation of the Earth they precede the moon so the high tide do not occur when
the moon is overhead but later (as much as 6 hours later)
The bulge nearest the Moon is actually a bit ahead of the
Earth-Moon line. That bulge has mass; not a lot, but some.
Since it has mass, it has gravity, and that pulls on the Moon.
It pulls the Moon forward in its orbit a bit. This gives the
Moon more orbital energy.
An orbit with higher energy has a larger radius, and so as
the bulge pulls the Moon forward, the Moon gets farther
away from the Earth. This has been measured and is
something like a few centimeters a year.
Of course, the Moon is pulling on the bulge as well (Newton’s third law!). Since the Moon is "behind"
the bulge (relative to the rotation of the Earth), it is pulling the bulge backwards, slowing it down.
Because of friction with the rest of the Earth, this slowing of the bulge is actually slowing the rotation
of the Earth! This is making the day get longer.
Gravitational locking
Eventually, the Earth's rotation will slow down so much that the bulge will line up exactly
between the centers of the Earth and the Moon. When this happens, the Moon will no longer be
pulling the bulge back, and the Earth's spin will stop slowing. But when this happens, the time it
takes for the Earth to rotate once will be slowed to exactly the same time it takes for the Moon to
go around the Earth once! If you were to stand on the Moon and look at the Earth, you would
always see the same face of the Earth.
Does this sound familiar?
It should. Since Earth's gravity is much stronger than the
Moon's, the tides from the Earth on the Moon are much
stronger than the Moon's tides on the Earth. The Moon has
tidal bulges just like the Earth, and so it too was slowed by the
Earth's pull on its nearer bulge. Eventually, the Moon's rotation
was locked so that it took the same time to spin once on its axis
as it takes to go around the Earth. This is why we always see the
same face of the Moon! And this happened to the Moon before
the Earth because the Earth's tides are so much stronger.