Midterm 3 Flashcards
(174 cards)
What is in our solar system?
Early astronomers knew Moon, stars, Mercury, Venus, Mars, Jupiter, Saturn, comets, and meteors. Now: ● 1 star ● 8 planets (add Uranus & Neptune) ● 166 moons ● >660,000 asteroids ● comets, meteoroids ● ~50 dwarf planets, ● Kuiper Belt objects
What are terrestrial planets?
Close to the Sun. Made of rocks (silicon) and iron.
High density
Small (10000 km in diameter)
What are Jovian Planets?
Farther from the Sun. Made of gases (H, He, methane, water, ammonia), lower density, large
How do the planets orbit the Sun?
The planets orbit the sun from W to E along the plane of the ecliptic – looking down from the Earth’s North pole, planets orbit counterclockwise
Can we develop a model for the formation of the solar system that explains these properties?
The nebular hypothesis suggests that the planets formed from a gas cloud which collapsed into a disk.
This gas cloud has roughly the same composition as the Sun (mostly hydrogen, helium, + a trace of carbon, oxygen, nitrogen, iron etc)
The idea that the planets form from a disk is called
The nebular hypothesis.
This idea was proposed by
many people, one of which
was Pierre Simon Laplace, a mathematician in 18th century France
However, this was not the only idea
Alternatives to the nebular hypotheses
Tidal model: a passing star ripped material from the Sun and that material collapsed to form the planets
Capture model: The sun and planets formed separately, but the planets were captured later by the Sun
Accretion model: The sun moved through a gas cloud, got some gas and that gas formed the planets
What should we remember about the mass of our solar system?
Remember that most of the mass of the solar system is in the Sun. So the formation of the solar system is a footnote to the formation of the Sun.
Recall that stars form from molecular clouds.
What is a protostar
The collapse of a molecular cloud from a star forms a protostar and the disk of gas that surrounds it
What is Disk Formation
As the cloud collapses, the angular momentum in the gas makes it spin faster and faster until the the gas moves fast enough to orbit the protostar.
This is a general principle in astronomy. Collapse of stuff leads to the formation of a disk due to angular momentum
What is the concept of angular Momentum?
Hint: think of an ice skater
Angular momentum: spinning things keep spinning, and in the same direction Conservation of angular momentum says that product of radius and rotation rate must be constant.
→ Therefore, as a dust cloud collapses, its rate of
rotation will increase.
What is the condensation of the planets?
● Gas does not condense (because it remains gas), but dust can gather – tiny chunks of rocky and icy matter, with sizes of about 10-5 m
● Dust grains form in cool atmospheres of old stars, are ejected, grow by accumulating molecules from interstellar gas
● Dust collects into larger bodies: dust bunnies!
What is the process of clumps of dust growing larger?
accretion
What is happens when objects get large enough to create gravity strong enough to affect their neighbors?
Planetesimals
Eventually nearly all material is wept up into ________?
Protoplanets
What happens to the stuff that escapes capture and is left over?
Asteroids and Comets
How did the Moon form
During the formation of the Earth, the young Earth suffered a collision with a Mars-sized body that threw up material into orbit that condensed to form the Moon.
This is a rare event, and Earth is the only terrestrial planet with a large moon
How are Jovians formed?
To form the Jovian planets, we need one more stage of planet formation in which the gas accretes onto these rocky cores
However, to accrete gas we need a big core!
Bigger cores are possible if you can gather more material. In regions where the gas is so cold that ices form – beyond the snow line or frost line – we have the extra stuff to make this possible.
What is Scattering and Ejection
The larger pieces of this debris in the early solar system are called planetesimals. The ejection and scattering of planetesimals allowed the planets to change their orbits.
Generally Neptune, Uranus and Saturn move outward at the expense of Jupiter, which moves inward.
Jupiter being the biggest planet tends to fling stuff out of the solar system, causing it to move inward, while the other three planets tend to move planetesimals inward – so they move outward.
The Nebular Hypothesis and the Solar System
● Planets form in a rotating disk
○ Planets are all (nearly) in a plane to about 1%
○ All orbit in a counterclockwise direction and nearly all
rotate in the same direction as well.
○ Orbits are nearly circular
● Planets are relatively isolated – far away from their neighbors
○ Planets accrete all the material in their neighboring orbits
What are good indicators of the past composition?
The small bodies that have the best clues are asteroids, comets, meteoroids (coming from asteroids and comets) and plutoids.
The age and chemical composition of these things can tell us about the early solar system
What are Asteroids?
● Rocky bodies that are held together by gravity and internal forces
● Most live in a belt between Mars and Jupiter at 2.8 A.U. called the asteroid belt
● about 100,000 rocky objects bigger than 1 km exist
● Ceres is the largest asteroid with a diameter of ~1000 km
● A few thousand have orbits that cross Earth’s orbit –
called near-Earth asteroids (NEAs)
● Some are near Jupiter (60 degrees ahead and behind)
and are called Trojans
Why do we care about Asteroids?
● Asteroids are left-over material from formation of the solar system
→ ideal laboratory to study formation of earth and other planets
● Potential source of water on earth
What are Meteors, Meteorids, and Meteorites
Although these terms sounds very similar, they describe different phenomena that can be arranged by time:
A meteoroid is a piece of interplanetary matter that is smaller than a kilometer and frequently only millimeters in size.
Most meteoroids that enter the Earth’s atmosphere are so small that they vaporize completely and never reach the planet’s surface.
The flash of light we see while they burn up in the atmosphere is what we call a meteor (or fireball, for the brightest ones)
Whatever is left once it hits the ground (anywhere between the size of a sand grain to a giant boulder) is a meteorite.