WEST VIRGINIA UNIVERSITY AT PARKERSBURG
ASTRONOMY 106 - INTRODUCTION TO ASTRONOMY
ORIGIN AND EVOLUTION OF THE UNIVERSE AND SOLAR SYSTEM
by
Edward L. Crisp, Ph. D.
Professor
of Geology
INTRODUCTION
The most accepted theory for the origin
of the Universe is the Big Bang Theory, which basically states that about
13 to 15 billion years ago (astronomers now estimate an age of 13.7
billion years for the Universe) an infinitely dense point of pure energy "exploded"
and expanded outward to eventually evolve into our present Universe.
The Universe was initially extremely hot (about 100 billion k), but as
expansion continued the Universe cooled, matter formed and clumped together
by gravity, and stars, planets, and galaxies formed.
Our Solar System started forming about
5 billion years ago. According to the Solar Nebula Theory, our Solar
System formed as the result of the contraction of a diffuse, gaseous nebular
cloud (consisting primarily of hydrogen and helium, but with some dust
containing heavier elements). As the nebular cloud contracted (perhaps
initiated by a nearby supernova explosion of a star) it flattened into a disk
shaped structure with 90% of the material going to the center (by gravity)
to eventual form the sun. Eddy currents in the disk attracted matter
that would eventually condense and coalesce to form the planets.
Our Solar System was pretty much as we see it today by about 4.6 billion
years ago.
THE COSMIC BACKGROUND RADIATION
Arno Penzias and Robert Wilson received
the Noble Prize in Physics in 1978 for their discovery of the cosmic
background radiation. In 1965, as astronomers with Bell Telephone
Laboratories in New Jersey, they discovered a background radiation coming
from outside our solar system that corresponded to a constant temperature
of 2.7 kelvin (or 2.7 oC above absolute zero). They postulated
that this 2.7 kelvin temperature is the relic of the initial high temperature
of the early Universe.
Wilson and Penzias with their historic horned antenna at Crawford Hill,
N.J. Wilson is on the left and Penzias on the right. (From:
Cosmology
- Penzias and Wilson's Discovery is One of the Century's Key Advances
at http://www.bell-labs.com/project/feature/archives/cosmology/)
This cosmic background radiation has a maximum
wavelength of about 2 mm (in the microwave range of the electromagnetic
spectrum). The radiation has all the characteristics of radiant heat
and is the same kind of radiant heat as emitted by an object with a temperature
of 2.7 oC above absolute zero. So the initial extremely
hot radiant heat from the primordial fireball (of the Big Bang) has cooled
down to 2.7 k, and will eventually cool to absolute 0. This
is direct evidence of the "Big Bang".
THE BIG BANG THEORY
According to the Big
Bang Theory, the Universe was initially concentrated into an extremely
dense region billions of times smaller than a proton. The initial
core exploded about 13 to 20 billion years ago (although most astronomers
think this happened about 13 to 15 billion years ago) and sent energy (and
eventually matter) expanding outward in all directions.
There are two main
lines of support for the Big Bang Theory and an expanding Universe (these
are the main lines of support, there are several others):
-
1) Distant galaxies are moving away from Earth
at high speed and the velocities of recession increase with distance from
Earth. Thus, the Universe is expanding. This was first discovered
by Edwin Hubble (1929).
-
Edwin
Hubble
-
From: Part 6:
Red Shift at http://www.arachnoid.com/sky/redshift.html
-
He noted that the spectral lines (wavelengths
of light) of the receding galaxies are shifted toward the red end of the
spectrum, thus a shift towards longer wavelengths. We say that the
light
is redshifted. This redshift of the
light from receding galaxies is caused by the Doppler
Effect.
-
2) The Cosmic Background Radiation permeating
the Universe as discovered by Penzias and Wilson (as discussed previously).
Red Shift and the Doppler Effect
-
Doppler Effect: The apparent shift of the
wavelength of waves caused by movement of the source of the waves relative
to an observer. The Doppler Effect is commonly observed by most people
when moving vehicles approach and pass. The sound waves from the
moving vehicle are shifted towards shorter wavelength as the vehicle approaches
an observer (the observer hears a higher pitched sound) and is shifted
towards longer wavelengths as the vehicle moves away from an observer (the
observer hears a lower pitched sound). A source of light that is
moving towards an observer will have an apparent shift of the wavelengths
to shorter wavelengths (blueshifted), where as a source of light moving
away from an observer will appear to have the wavelengths shifted to longer
wavelengths ( redshifted).
-

-
From: Doppler
Effect at http://www.ncsa.uiuc.edu/Cyberia/Bima/doppler.html
-
Red Shift of Stars and Galaxies:
Light coming from receding stars or galaxies appears to be more red, that
is, the wavelengths are shifted towards the red end of the spectrum.
If the stars or galaxies were moving towards us, the wavelengths would
be shifted towards the shorter wavelengths and the light would appear more
blue.
-
Hydrogen Spectra: The wavelengths
of hydrogen spectra from receding galaxies are shifted to progressively
longer wavelengths for galaxies at larger and larger distances from Earth.
-
The velocity of recession of galaxies from each
other is proportional to the distance between them, thus farther galaxies
are receding with higher velocities.
-

-
From: Expanding
Universe at http://bustard.phys.nd.edu/Phys171/lectures/expandu.html
-
We can compare the expansion of the Universe to expanding raisins in
a loaf of rising (and baking) raisin bread.
-
Based on the idea of an expanding Universe and the rate of recession
of galaxies from each other, astronomers can use the expansion rate to
calculate how long ago the galaxies were together at a single point.
-
The estimate works out to 13 to 20 billion years (depending on the value
of the Hubble constant). Most astronomers believe the Universe is
about 13 to 15 billion years old. Has the recessional velocity been
constant with time? What is the gravitational effect? How much matter
is in the Universe? What is "Dark Matter" and how much of it is in
the Universe?
EARLY HISTORY OF THE UNIVERSE
From: Mysteries
of Deep Space - History of the Universe Timeline at http://www.pbs.org/deepspace/timeline/index.html
(At the site containing this graphic timeline each stage is a link to a
discussion of what was happening at that time)
Astrophysicists can theoretically go back
to a fraction of a second (10-43seconds) following the "Big
Bang". Beyond this the Universe consisted of pure energy and the
four major forces of nature that we recognize were not distinct entities
(they may have been unified). Those four major forces of nature are
1)
the gravitational force, 2) the electromagnetic
force, 3) the strong nuclear force (holds
nuclear particles together), and 4) the weak nuclear
force (involved in radioactive decay). At the birth of the
Universe the temperature and density were extremely high and only pure
energy could exist.
-
Within the first second after the "Big Bang":
-
The four forces of nature separated out.
-
The Universe inflated rapidly.
-
Quarks and electrons started forming, as did antiquarks and antielectrons
(antimatter).
-
Matter and antimatter collided and annihilated each other, but fortunately
the Universe was asymmetrical and had more matter than antimatter.
Thus a slight excess of matter was left over, which makes up our present
Universe.
-
Quarks formed protons and neutrons.
-
-
By three minutes after the "Big Bang":
-
The temperature had cooled to about 1 billion kelvin.
-
Protons and neutrons fuse to form hydrogen and helium nuclei.
-
By about 300,000 years after the "Big Bang":
-
The temperature had cooled to about 3000 kelvin.
-
Electrons combined with nuclei to form complete atoms of hydrogen and
helium.
-
Photons separated from matter and light burst forth for the first time.
-
By about 200 to 300 million years after the "Big Bang":
-
Matter began collecting into clouds of various sizes that eventually
collapsed due to gravity to form stars and galaxies. In other words,
the Universe became "clumpy".
-

Birth of Stars and Galaxies - 300 million years
"Gravity amplifies slight irregularities in the density
of the primordial gas. Even as the universe continues to expand rapidly,
pockets of gas become more and more dense. Stars ignite within these pockets,
and groups of stars become the earliest galaxies. This point is still perhaps
12 to 15 billion years before the present. The Hubble Space Telescope recently
captured some of the earliest galaxies ever viewed. They appear as tiny
blue dots in the Hubble Deep Field, the image on the left."
From: Mysteries
of Deep Space - History of the Universe Timeline at http://www.pbs.org/deepspace/timeline/index.html
-
The early Universe consisted of 100% hydrogen and helium. Today
the Universe has about 98% hydrogen and helium.
-
THE SYNTHESIS OF HEAVIER ELEMENTS AND THE CHANGING COMPOSITION OF THE
UNIVERSE
After stars began forming, heavier elements
formed in the cores of stars by a process known as
nucleosynthesis. Stars are born when
hydrogen in the core starts fusing into helium. Low mass stars (about
the size of our Sun or a little more massive) will start fusing helium
into carbon when they use up the hydrogen in the core. When the core
has be converted to carbon, these low mass stars cannot generate enough
pressure by gravitational collapse (the core will collapse because of gravity
if no energy is pushing out due to fusion) to fuse carbon into higher elements.
They will collapse to the size of the Earth and become extremely hot (a
white
dwarf), but they will never fuse again so
will eventually cool off to become a
black
dwarf (a burned out chunk of carbon).
High mass stars can generate enough pressure to fuse carbon into heavier
elements. However, as these stars successively fuse elements higher
than carbon, a problem occurs when the core is fused into iron. Iron
absorbs the energy of gravitational collapse and will not fuse into higher
elements. This results in rapid collapse (implosion) of the star
and a rapid rebound (i.e., the star explodes). The explosion
of a massive star is called a supernova.
During a supernova explosion nuclear particles are rammed together at extremely
high velocities. This results in further fusion to form all the elements
heavier than iron.
The Crab Nebula (supernova remnant). From: The
Crab nebula (M1) at http://www.aao.gov.au/images.html/captions/crab.html
As a result of the
explosion of stars, hydrogen, helium, and the heavier elements are returned
to space to form clouds of dust and gases (nebula) that can then collapse
to form additional stars. Our Sun is a second or third generation
star that has abundant heavy elements (although it still is mostly hydrogen
and helium).
ORIGIN AND HISTORY OF THE SOLAR
SYSTEM
Any theory to explain the origin and evolution
of the solar system must explain the following observations about the solar
system:
-
All planets revolve around the Sun on or near
the plane of the ecliptic (exceptions: Pluto about 17 degrees
off plane of ecliptic and Mercury about 7 degrees off the plane of the
ecliptic). Pluto is thought to have been a moon of Neptune, but possibly
escaped the gravitational pull of Neptune and took up its own orbit around
the Sun. Pluto's composition is similar to the moons of the Jovian
planets.
-
All the planets (except Venus and Uranus) and most of the moons in our
solar system rotate on their axis in a counterclockwise
direction (as viewed from above the north pole of the Sun and looking
down on the solar system). Venus rotates slowly to the right,
possibly due to a catastrophic collision early in the evolution of the
solar system. Uranus is tilted on its side with the north pole pointing
towards the Sun, again possibly due to a catastrophic collision early in
the evolution of the solar system.
-
All the planets revolve around the Sun in a counterclockwise
direction.
-
All the planets (except Pluto and Uranus) have a rotational
axis that is near perpendicular to the plane of the ecliptic.
-
The difference in chemical composition and characteristics
of the inner Terrestrial planets as compared to the outer Jovian planets.
The Terrestrial planets have high densities (about 4 to 5.5 g/cm3),
no or few moons, and are primarily composed of metals and silicate rocks.
The Jovian planets have low densities (about 0.7 to 1.76 g/cm3),
many moons, and are primarily composed of gases (hydrogen, helium, methane,
ammonia, and water vapor) and frozen compounds rich in hydrogen.
-
The slow rotation of the Sun.
-
Asteroids, comets, and interplanetary debris and
dust must be explained.
-
The relatively slow axial rotation of the Sun
must be explained.
The most accepted theory for the formation
of the solar system (which explains all of the above observations) is the
Solar
Nebula Theory. The Solar Nebula Theory states the following:
-
About 5 billion years ago a portion of a large nebular cloud of interstellar
material in a spiral arm of the Milky Way Galaxy began to collapse due
to gravity. The initiation of gravitational collapse may have been
due to a pressure wave from a nearby supernova explosion (which pushed
matter closer together in the cloud and caused a stronger gravitational
force within the cloud - remember Newton's inverse square law of gravitation).
-
As the interstellar material collapsed it began to rotate in a counterclockwise
direction with 90% of the material collapsing to the center of rotation.
Due to the increasing rate of spin as the material collapsed (due to conservation
of angular momentum), the material flattened into a disk shaped structure
(a solar nebula).
-
As the solar nebula continued to concentrate material in the center
and the disk, the embryonic Sun formed with a rotating, turbulent cloud
of material around it.
-
Gases and solids began to condense in localized turbulent eddies to
form particles that then collided because of gravitational attraction to
form planetesimals (from a few meters
to a few tens of meter in size). Dust from the original interstellar
material may have served as nuclei for condensation.
-
Planetesimals collided with each other to accrete into protoplanets
and eventually into the planets we know today. This process to form
the planets probably took about a million years or so.
-
The inner (Terrestrial) planets, being near the evolving Sun (which
was growing very hot due to gravitational collapse) could only form from
condensation of metals and silicates (refractory elements) due to the high
temperature. So not much gas could accumulate in the inner solar
system due to the high temperature.
-
The outer (Jovian) planets, which formed far from the embryonic Sun,
in the outer much cooler region of the solar system were formed from condensation
of metals, silicates, and gases (because all could condense at the cooler
temperatures). However, because gases (primarily hydrogen and helium)
were much more abundant in the original interstellar material than refractory
elements, the outer planets are primarily gaseous giants, but do have rocky,
metallic cores.
-
Eventually the core of the embryonic Sun grew so hot and was under such
high pressure that hydrogen was fused into helium. This provided
an outward pressure from the core that halted the gravitational collapse.
Thus our modern Sun came into existence as a nuclear fusion furnace.
When our Sun "turned on", solar radiation and particles (protons,
neutrons, and electrons) began streaming outward from the Sun into the
solar system. This is referred to as the solar wind. The solar
wind blew any additional gas and dust out of the inner part of the solar
system (most being captured by the Jovian planets). (Our Sun has
been fusing hydrogen into helium for about 5 billion years and has enough
hydrogen to continue this process for about another 5 billion years.
When the hydrogen is used up in the core, our Sun will start to die..........another
story for another time)
-
Planetisimals between Mars and Jupiter was affected by the gravitational
fields of the two planets (particularly Jupiter) and could not accrete
into a planet, thus the asteroid belt was formed.
-
Icy planetesimals that formed in the outer solar system were attracted
to the large Jovian planets, if they missed collision with them they were
gravitational flung into a spherical region surrounding the solar system
known as the Oort Cloud. These icy planetesimals are incipient comets
and perhaps are occasionally pulled into the inner solar system as another
star comes close to our Sun (maybe we have a sister star that revolves
around our Sun). Comets often hit planets and moons.
-
A small amount of dust and gases still remain in interplanetary space
that was never accreted into larger bodies. Collisions of asteroids
with each other generate fragmentary material (meteoroids) that move out
of the asteroid belt, sometimes impacting planets and moons as meteorite
collisions.
-
The slow rotation of the Sun on its axis is due to the magnetic field
lines of the Sun interacting with ionized gases that were in the solar nebula.
This is referred to as magnetic braking.
-
The formation of our solar system was complete by about 4.6 billion
years ago.
So the Solar Nebular Theory explains all the
observations relative to our solar system.
METEORITES AND THE AGE OF THE EARTH
Meteorites are thought to be primeval material
left over from the formation of the solar system that has not evolved since
formation. Much of the meteorite bombardment of planets and moons
in the early history of our solar system was from material that had not
accreted into a planet or moon. Many meteorites that hit planets
and moons today are the pieces of asteroids that have collided and fragmented
(asteroids have also not evolved much since the formation of the solar
system). (Note: chunks of material moving through
interplanetary space are called meteoroids; when a meteoroid enters an
atmosphere of a planet and heats up it is called a meteor {a "shooting
star"}, and when a meteoroid or meteor hits a planet or moon it is called
a meteorite.)
-
Stones - of all meteorites found on Earth, 93% of them are stones.
Stones are of two types: Chondrites and Achondrites.
-
Chondrites are composed of olivine and pyroxene. The olivine and
pyroxene compose the chondrules, small spherical
grains that represent the original rapid cooling and condensation to form
the meteorite. Most stoney meteorites are thse ordinary chondrites;
however, some chondrites contain a small percentage of organic compounds,
such as amino acids. The chondrites that contain organic compounds
are called carbonaceous chondrites.
The organic compounds found in these meteorites are not of biologic origin,
but may represent precursors of biologic organisms.
-
Achondrites contain no chondrules and have a composition much like terrestrial
basalts. They probably are pieces of large differentiated asteroids
that have fragmented due to collision.
-
-
Irons - make up about 6% of all meteorites found on Earth. They
are
composed of large crystals of iron and nickel alloys and probably formed
in the interior of large differentiated asteroids where relatively slow
cooling took place.
-
Stoney-irons - make up only about 1% of all meteorites that impact the
Earth. They are composed of about equal amounts of iron/nickel and
silicates and probably represent broken fragments from the zone between
the metallic and rocky portions of large differentiated asteroids.
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Another class of meteorites that are found on Earth (relatively rare)
are chunks of rock that (based on their composition) represent surface
material from the Moon or Mars. These meteorites formed when Mars
or the Moon were hit by meteorites with a glancing blow that shattered
surface rock with such force as to knock some of the material into space,
where it eventually hit the Earth.
Radiometric dating of most meteorites yields an age of 4.6 billion years,
thus this is thought to represent the age of the solar system.
DIFFERENTATION OF THE EARLY EARTH OR HOMOGENEOUS ACCRETION VERSUS
INHOMOGENEOUS ACCRETION OF THE EARLY EARTH
-
How did the Earth become stratified into layers of different densities
and compositions?
-
Homogeneous Accretion Model: The
Earth formed as a homogeneous mixture of silicates and metals, but due
to meteorite bombardment, gravitational compression, and radioactive decay
the Earth become molten soon after formation. Once molten, the heavier
metals (iron and nickel) settled to the core and was surrouned sequential
by lighter and lighter silicate minerals.
-
Inhomogeneous Accretion Model: The
layers of the Earth condensed sequentially (as cooling progressed) from
the hot gaseous material of the inner solar system.
-
At present, geologists and astronomers favor the homogeneous accretion
model for the formation of the Earth's internal structure.
ORIGIN OF OUR MOON
-
Our moon is thought to have formed early in the history of the solar
system by the impact of a Mars sized planetesimal with the Earth some 4.6
to 4.4 billion years ago. Material that was liquified and vaporized
from the impact took up orbit around the Earth and eventually coalesced
by gravity to form the moon.
"Half
an Hour After the Giant Impact,
based on computer modeling by A. Cameron, W. Benz, J. Melosh, and others.
Copyright
William K. Hartmann" From: The
Origin of the Moon at http://www.psi.edu/projects/moon/moon.html (GO
TO THIS SITE AND READ ABOUT THE ORIGIN OF THE MOON).
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The Moon's original crust cooled about 4.4 billion years ago.
Rocks sampled by the Apollo Missions from the lunar highlands (light colored
areas on the moon) and thought to represent the original cooled crust of
the Moon have been radiometrically dated at about 4.4 billion years.
The maria (dark areas on the Moon) formed later due to volcanic lava flows
which filled in low places and date from 3.2 to 3.8 billion years
old.
THE PLANETS
HERE IS A LINK THAT HAS A TREMENDOUS AMOUNT OF INFO. AND LINKS ABOUT
THE PLANETS: The Nine
Planets at http://www.seds.org/billa/tnp/