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Transcript
Chapter 27
Formation of the Solar System
The sun and all of the planets and other
bodies that revolve around the sun.
It all started with a Big Bang (theory).
The Nebular Hypothesis
* 1796 (Immanuel Kant)
• The sun and the planets condensed at about the same time
out of a collapsing cloud of gas and dust called a
solar nebula.
– About 4.6 billion years ago, the amount of gravity near one of these
clouds increased as a result of a nearby supernova (or some other
force).
– The rotating cloud of gas and dust from which the sun and planets
formed is called the solar nebula.
– Energy from collisions and pressure from gravity caused the center of
the solar nebula to become hotter and denser (10,000,000oC).
– Hydrogen fusion began… a star formed (we call ours the sun).
– The sun contains about 99% of all the matter contained in the solar
nebula.
– Planets started out as small bodies called
planetesimals.
– Some planetesimals joined together through
collisions and the force of gravity to form
protoplanets.
– Collisions added mass to the protoplanets to
become planets and some moons.
– the four inner planets are the terrestrial planets
of Mercury, Venus, Earth, and Mars.
– The four outer planets are the gas giants of
Jupiter, Saturn, Uranus, and Neptune.
Formation of solid Earth
• When Earth first formed, it was very hot.
(hot enough to melt iron)
– energy was produced when
• the planetesimals collided during formation
• The outer layers compressed the inner layers
• Radioactive materials present emitted high energy
particles.
• Heat caused denser materials to sink toward the center, a
process called differentiation, which led to the layers of the
earth (crust, mantle, and core).
• Earth’s surface cooled and solid rock at the surface formed.
Formation of Earth’s atmosphere
– Hydrogen and helium gas (less dense) rose to the
surface of the earth and were then released into the
atmosphere. They eventually escaped into space.
– As Earth’s surface continued to form, volcanic eruptions
were frequent and water vapor (H2O), carbon dioxide
(CO2), nitrogen (N2), methane, sulfur dioxide, and
ammonia were released.
– This outgassing formed the atmosphere.
– These gases reacted with radiation from the sun to
form other components such as ozone (O3).
– As life evolved, other gases, namely oxygen (O2), were
added to the atmosphere (2 billion years ago).
Formation of Earth’s Oceans.
• Some scientists think that, in addition to
outgassing, some of Earth’s water may have come
from space in the form of ice from comets.
• As Earth cooled, water vapor condensed to form
rain that collected on the surface.
• First it was all freshwater then later minerals such
as salt (halite) were washed and eroded in to it.
Aristotle’s Model
Geocentric Model of the Solar System
•
•
•
•
•
1st model of the solar system
Planets, stars and sun revolved around the earth.
Geocentric means “earth-centered”
Heavens are unchanging (perfect)
Theory lasted about 2000 years
• Problem:
– It did not explain how planets sometimes appear to move backwards
in the sky relative to the stars = retrograde motion.
Link
Ptolemy’s Model
• Greek philosopher –
proposed changes
• Planets moved in
small circles
(epicycles) as they
revolved around the
Earth.
• It actually explained
retrograde motion
pretty well.
Copernicus’ Heliocentric model
• 1543, polish astronomer Nicolaus Copernicus
• Heliocentric model of the Universe – “sun-centered”
• Planets revolve around the sun in the same direction
but at different speeds and distances from the sun.
• Explained retrograde motion the best
• Fast moving planets passed
slow moving planets which
made them appear to move
backwards.
Galileo Galilei
• Observed that four moons traveled around
the planet Jupiter.
• Showed him that objects can revolve around
other objects other than Earth.
Galileo Galilei
• Observed that mountains exist on
Earth’s moon.
• Showed him that objects don’t have to be
perfectly spherical and can be more like Earth
Kepler’s Laws #1
(based on observations by Tycho Brahe)
1. Law of ellipses
- each planet orbits the sun in a path called an ellipse
(oblong or oval, not a circle).
- eccentricity is the degree of elongation of an
elliptical orbit. The more eccentric the orbit the more
elongated it is.
(an eccentricity near “0” is almost a perfect circle).
Kepler’s Laws #2
(based on observations by Tycho Brahe)
2. Law of equal areas
– describes the speed at
which objects travel at
different points in their orbits.
- Objects move faster in their
orbit when they are closer
the sun.
- equal areas are covered in
equal amounts of time
as an object orbits the sun.
Kepler’s Laws #3
(based on observations by Tycho Brahe)
3. Law of periods
- describes the relationship between the average distance of a
planet from the sun and the orbital period of the planet.
- Orbital period is the time required for a body to complete a
single orbit (planets further away take longer to complete an orbit).
- allows Scientists to determine how far away a planet is from
the sun.
2
T
=
3
a
T = earth years and
Example: Jupiter’s orbital period is 11.9 Earth years (T),
the square is 142;
142 is 5.2 cubed
Jupiter is 5.2 AU from the sun.
a = AU
Newton’s laws of motion
• 1st Law: a moving body will remain in motion and resist a change
in motion until an outside force acts on it – inertia.
• Because a planet does not follow a straight path, an outside force
must cause the orbit to curve.
• Gravity! The gravitational pull of a larger object (sun) is that force.