formation of the solar system. simulation terrestrial & jovian planets

67
Formation of the Solar System

Upload: homer-lee

Post on 23-Dec-2015

243 views

Category:

Documents


2 download

TRANSCRIPT

Page 1: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Formation of the Solar System

Page 2: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Simulation

Page 3: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Terrestrial & Jovian planets

Page 4: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Given the composition of the solar nebula, why do you think all the terrestrial planets have smaller masses than the Jovian planets? 98% hydrogen and helium1.4% hydrogen compounds – CH4, NH3, H2O0.4% silicate rocks0.2% metals

Page 5: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 6: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 7: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Can the Earth hold hydrogen and helium gas in its atmosphere? How do you know?

Page 8: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Do you think any of the other terrestrial planets hold hydrogen and helium gas?

Page 9: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Why do you think the cores of all the Jovian planets have a mass about 10 times the mass of the Earth?

Page 10: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Jovian Planets

Once at protoplanet reaches a mass of about 10 times that of the Earth, it can capture large amounts of gas directly from the solar nebular, becoming a Jovian planet.

Page 11: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Why do you think Uranus and Neptune didn’t get as big as Jupiter and Saturn?

Page 12: Formation of the Solar System. Simulation Terrestrial & Jovian planets

What about Pluto and the other TNO’s

Just the proto-cores of would-be Jovian planets that never got massive enough to hold H and He.

Page 13: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Doppler method for extra solar planet detection

Page 14: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

What planet characteristics (mass and distance from the star) will be easiest to find with the Doppler method? Explain your reasoning.

Page 15: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Extra Solar planets

Many extra-solar planets are Jupiter-like planets which lie very close to their star.

NASA’s Kepler mission indicates that hot Jupiter’s are not very common.

Page 16: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Kepler results

Page 17: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Planetary Migration

Most likely these hot Jupiters formed beyond the frost-line, but due to close encounters with other protoplanets lost orbital speed and spiraled in toward the star.

Page 18: Formation of the Solar System. Simulation Terrestrial & Jovian planets

The Sun

Page 19: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Why does the Sun shine?

Page 20: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

How do you know the Sun is hot?

Page 21: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

How do we know the temperature of the Sun?

Page 22: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 23: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Why is there less solar intensity at sea level than there is at the top of Earth’s atmosphere?

Page 24: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Where do you think that energy goes?

Page 25: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Why isn’t the Sun a perfect blackbody?

Page 26: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 27: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Solar Data

Radius: 109 Earth radiiMass: 333,000 Earth massesComposition: 74% hydrogen

25% heliumMean density: 1.41 g/cm3

Luminosity: 3.86 1026 Watts

Page 28: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

How do we know the mass of the Sun?

Page 29: Formation of the Solar System. Simulation Terrestrial & Jovian planets

The Sun as a big cosmic light bulb

Suppose every human being on Earth turned on 1000, 100-watt light bulbs. With about 6 billion people this would only be 6 1014 watts. We would need 670 billion more Earth’s doing the same thing to equal the energy output of the Sun.

Page 30: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Anaxagoras (500 – 428 B.C.E.) believed the Sun was a very hot, glowing rock about the size of Greece.

Cooling Ember theory

Page 31: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

If the Sun were cooling down over time, how could we tell?

Page 32: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Thermal equilibrium

The Sun is not measurably heating up or cooling down.

Page 33: Formation of the Solar System. Simulation Terrestrial & Jovian planets

No cooling ember

At the rate that the Sun is emitting energy, the Sun must have been much hotter just a few hundred years earlier, making life on Earth impossible.

The Sun must have an energy source; a way of generating its own heat.

Page 34: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Given the composition of the Sun, why is it unlikely that it could be heated by the burning of wood or coal?

Page 35: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Kelvin-Helmoltz contraction

As things contract gravitationally, they become hotter.

Page 36: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Why do you think gravitational contraction leads to a temperature increase?

Page 37: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

If the Sun is getting its energy from Kelvin-Helmoltz contraction, how could you prove this? Do you think this is an easy thing to do? Explain.

Page 38: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Hydrostatic Equilibrium

The Sun is not measurably expanding or contracting

Page 39: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Sedimentary rocks on Earth which were deposited in liquid water are 3.8 billion years old.

Rocks containing fossils are 3.5 billion years old. The Sun must have been shining for at least this long.

The age of the Sun

Page 40: Formation of the Solar System. Simulation Terrestrial & Jovian planets

What energy source can keep the Sun hot for 3.8 billion years?

Burning coal: Sun would last 10,000 years

Kelvin-Helmholtz contraction: if the Sun’s heat were generated from contraction of the Sun’s mass, it would shine for only 25 million years.

Page 41: Formation of the Solar System. Simulation Terrestrial & Jovian planets

E = m c2

Matter is a form of frozen energy.

Energy equals the mass times the speed of light squared.

Page 42: Formation of the Solar System. Simulation Terrestrial & Jovian planets

The Sun is huge!

A little bit of matter can be turned into a large amount of energy. If the Sun’s mass could be converted to energy it could shine for hundreds of billions of years.

The Sun needs to convert 4.3 million tons of matter to energy every second.

Page 43: Formation of the Solar System. Simulation Terrestrial & Jovian planets

The Sun’s Mass is Converted to Energy

4 hydrogen atoms have a mass of 6.693 10-27 kg

(four protons)

1 helium atom has a mass of 6.645 10-27 kg

(two protons and two neutrons)

Thus, 0.048 10-27 kg are converted to energy.

Page 44: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Thermonuclear Fusion

The Sun fuses 4 hydrogen atoms together to produce 1 helium atom releasing energy. In the Sun about 600 million tons of hydrogen is converted to helium per second.

Page 45: Formation of the Solar System. Simulation Terrestrial & Jovian planets

How does it work?

We need a new form of matter called anti-matter. Antimatter is made up of anti-particles which have the same mass as ordinary particles but opposite charge.

Matter and antimatter will annihilate each other if they come in contact producing energy.

Page 46: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Proton-Proton chain

Helium nuclei can be built up one proton at a time in what we call the proton-proton chain.

Normally, two protons will repel each other with the electrostatic force, but if they are smashed together with enough force they can stay together via the strong nuclear force.

Page 47: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Changing protons into neutrons is a very slow process, at the Sun’s temperature, it takes billions of years to convert two protons into a deuterium nucleus.

Page 48: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Neutrinos

Neutrinos () are particles that only interact with matter via the weak nuclear force (the force responsible for radioactive decay).

To stop a typical neutrino emitted from the Sun would require 1 light-year (5 trillion miles) of lead.

Page 49: Formation of the Solar System. Simulation Terrestrial & Jovian planets

How do we know thermonuclear fusion is taking place in the Sun?

“We do not argue with the critic who urges that stars are not hot enough for this process; we tell him to go and find a hotter place.”

Eddington (1926)

Page 50: Formation of the Solar System. Simulation Terrestrial & Jovian planets

We can test the theory that the Sun is powered by

thermonuclear fusion by:

1. Modeling the solar interior2. Direct observations of solar neutrinos

Page 51: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 52: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Which acrobat would you rather be and why?

Page 53: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 54: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

What does this mean for the pressure on the gas as you descend into the interior of the Sun?

Page 55: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Pressure increases toward the center of the Sun

To maintain equilibrium, the pressure below each layer of the Sun must be greater than the pressure above that layer.

Page 56: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 57: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

What happens if you squash a gas?

Page 58: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Density increases toward center of the Sun

The Sun is gaseous. If you apply pressure to a gas is compresses, i.e. it’s density goes up.

Page 59: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Temperature increases toward the center of the Sun

As the pressure goes up toward the center of the Sun, the temperature also increases.

Page 60: Formation of the Solar System. Simulation Terrestrial & Jovian planets
Page 61: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

According to the previous graphs, where is fusion taking place in the Sun? Explain.

Page 62: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Fusion only takes place in the Sun’s core

In the inner 1/4 of the Sun’s radius can fusion take place.

Even at 15 million K, it takes on average 14 billion years at a rate of 100 million collisions per second to fuse two protons to produce a deuterium atom.

Page 63: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

Fusion keeps the Sun hot, but fusion requires the Sun to be hot. How did the Sun ever get hot enough to start fusion?

Page 64: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

What would happen if the Sun started to contract? What happens to the density, temperature, pressure, rate of fusion etc?

Page 65: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

What would happen if the Sun started to expand? What happens to the density, temperature, pressure, rate of fusion etc?

Page 66: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Negative feedback

The Sun is stabilized by this negative feedback. Contraction/higher core temperatures, increased fusion rates, expansion and cooling.

Expansion/core cooling, decreased fusion rates, contraction.

Page 67: Formation of the Solar System. Simulation Terrestrial & Jovian planets

Discussion

What happens if all fusion in the Sun ceases?