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The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? The Sun Planets Moons and Rings Comets Asteroids (size > 100 m) Meteoroids (size < 100 m) Kuiper Belt Oort cloud Zodiacal dust A lot of nearly

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Page 1: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

The Solar SystemChapter 4 – Part 3:

Early Solar System & Formation of Planets

Ingredients?

● The Sun● Planets● Moons and Rings● Comets ● Asteroids (size > 100 m) ● Meteoroids (size < 100 m)● Kuiper Belt● Oort cloud● Zodiacal dust● A lot of nearly empty space

Page 2: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Pluto is smaller than the other planets and the moonSun, Planets, and Pluto to scale

Smallest planet Mercury is 2x bigger (diameter) than Pluto

Page 3: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Pluto and the Dwarf Planets

Presented by: Jeff Saul <[email protected]>University of New Mexico Department of Physics and Astronomy

Page 4: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Clicker Question 1:

Which of the following is a Terrestrial planet:

A: Jupiter

B: Saturn

C: Mercury

D: Pluto

E: Neptune

Page 5: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Question 2

Compared to asteroids, comets show all of these properties EXCEPT

a) their densities are higher.

b) their orbits tend to be more elliptical.

c) they tend to be made of ice.

d) they can look fuzzy, whereas asteroids appear as moving points of light.

e) their average distances from the Sun are far greater.

Page 6: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Question 2

Compared to asteroids, comets show all of these properties EXCEPT

Comets have densities much lower than asteroids or

planets.

a) their densities are higher.

b) their orbits tend to be more elliptical.

c) they tend to be made of ice.

d) they can look fuzzy, whereas asteroids appear as moving points of light.

e) their average distances from the Sun are far greater.

Page 7: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

What causes a meteor shower?

Question 3a) A comet and an asteroid collide.

b) Earth runs into a stray swarm of asteroids.

c) Earth runs into the debris of an old comet littering its orbit.

d) Meteorites are ejected from the Moon.

e) Debris from a supernova enters Earth’s atmosphere

Page 8: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

What causes a meteor shower?

Question 3

Meteor showers can generate a few shooting stars, to hundreds of thousands, seen in an hour.

a) A comet and an asteroid collide.

b) Earth runs into a stray swarm of asteroids.

c) Earth runs into the debris of an old comet littering its orbit.

d) Meteorites are ejected from the Moon.

e) Debris from a supernova enters Earth’s atmosphere

Page 9: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Hubble’s view of Dwarf Planets:

Pluto Eris Ceres

Page 10: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

How did the Solar System Form?

We weren't there (it was 5 billion years ago). We need a good theory. We can try to check it against other forming solar systems. What must it explain?

- Solar system is very flat.

- Almost all moons and planets (and Sun) rotate and revolve in the same direction.

- Planets are isolated in space.

- Terrestrial - Jovian planet distinction.

- Leftover junk (comets and asteroids).

Not the details and oddities – such as Venus’ and Uranus’ retrograde spin.

Page 11: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

A cloud of interstellar gas

The associated dust blocks starlight. Composition mostly H, He.

a few light-years,or about 1000times bigger thanSolar System

Too cold for optical emission but some radio spectral lines from molecules. Doppler shifts of lines indicate clouds rotate at a few km/s.

Clumps within such clouds collapse to form stars or clusters of stars. They are spinning at about 1 km/s.

Page 12: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Solar System Formation Video

Page 13: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Clicker Question:

In the leading theory of solar system formation, the planets:

A: were ejected from the Sun following a close encounter with another star.

B: formed from the same flattened, swirling gas cloud that formed the sun.

C: were formed before the Sun.

D: were captured by the Sun as it traveled through the galaxy.

Page 14: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

But why is Solar System flat?

Pierre Laplace (1749 - 1827): an important factor is "conservation of angular momentum":

When a rotating object contracts, it speeds up.

"angular momentum" =(a property of a spinning or orbiting object)

mass x velocity x “size” = constant

of spin or orbit

of spinning object or orbit

Well demonstrated by ice skaters . . .

Page 15: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

So, as nebula contracted it rotated faster.

Could not remain spherical! Faster rotation tended to fling stuff outwards, so it could only collapse along rotation axis => it became a flattened disk, like a pizza crust. Hubble Space Telescope

is seeing these now!

Page 16: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Now to make the planets . . .

Solar Nebula:

98% of mass is gas (H, He) 2% in dust grains (Fe, C, Si . . .)

Condensation theory: 3 steps:

1) Dust grains act as "condensation nuclei": gas atoms stick to them => growth of first clumps of matter.

2) Accretion: Clumps collide and stick => larger clumps. Eventually, small-moon sized objects: "planetesimals".

3) Gravity-enhanced accretion: objects now have significant gravity. Mutual attraction accelerates accretion. Bigger objects grow faster => a few planet-sized objects.

Page 17: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Artist’s view of early Solar System

Page 18: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

initial gas and dust nebula

dust grains grow by accreting gas, colliding and sticking

continued growth of clumps of matter, producing planetesimals

planetesimals collide and stick, enhanced by their gravity

result is a few large planets

Hubble Space Telescope observation of disk around young star with ring structure. Unseen planet sweeping out gap?

Page 19: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Terrestrial - Jovian Distinction

Jovian solid cores ~ 10-15 MEarth . Strong gravity => swept up and retained large gas envelopes.

Outer parts cooler: ices form (but still much gas), also ice "mantles" on dust grains => much more solid material for accretion => larger planetesimals => more gravity => even more material.

Inner parts of Solar Nebula hotter (due to forming Sun): mostly gas. Accretion of gas atoms onto dust grains relatively inefficient.

Composition of Terrestrial planets reflects that of initial dust – it isnot representative of Solar System, or Milky Way, or Universe.

Terrestrial planets:

Jovian planets:

Page 20: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Asteroid Belt

Perhaps a planet was going to form there. But Jupiter's strong gravity disrupted the planetesimals' orbits, ejecting them out of Solar System. The Belt is the few left behind.

And Finally . . .

Remaining gas swept out by Solar Wind.

Page 21: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Zodiacal dust

Dust particles on the plane of the orbits of the planets. (size: 1 to 300 x 10-6 m)

Page 22: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Dinosaur Killer Impact 65 million years ago: an asteroidwith diameter roughly 10 km

High levels of iridium in RatonPass (I25)

Page 23: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

The Fossil Record is Marked by Mass Extinction Events

Extinction Genus loss

End Ordovician 60%

End Devonian 57%

End Permian 82%

End Triassic 53%

End Cretaceous 47%

From Solé & Newman 2002

Page 24: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids
Page 25: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Result from computer simulation of planet growth

Shows growth of terrestrial planets. If Jupiter's gravity not included, fifth terrestrial planet forms in Asteroid Belt. If Jupiter's gravity included, orbits of planetesimals there are disrupted. Almost all ejected from Solar System.

Simulations also suggest that a few Mars-size objects formed in Asteroid Belt. Their gravity modified orbits of other planetesimals, before they too were ejected by Jupiter's gravity.

Asteroid Ida

Page 26: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Clicker Question:

We can tell something of the composition of the planets by looking at their:

A: spectra

B: radius

C: mass

D: magnetic fields

Page 27: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Stellar Spectra

Spectra of stars are different mainly due to temperature and composition differences.

Star

'Atmosphere', atoms and ions absorb specific

wavelengths of the black-body spectrum

Interior, hot and dense, fusion

generates radiation with black-body

spectrum

Page 28: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

We've used spectra to find planets around other stars.

Page 29: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

Star wobbling due to gravity of planet causes small Doppler shift of its absorption lines.

Amount of shift depends on velocity of wobble. Also know period of wobble. This is enough to constrain the mass and orbit of the planet.

Page 30: The Solar System Chapter 4 – Part 3: Early Solar System & Formation of Planets Ingredients? ● The Sun ● Planets ● Moons and Rings ● Comets ● Asteroids

As of today ~400 extrasolar planets known. Here are the first few discovered.