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Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

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Page 1: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Astronomy 1 – Fall 2014

Lecture 7: October 23, 2014

Page 2: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Previously on Astro 1• Properties of the Planets:

– Orbits in the same plane and direction

– Inner (terrestrial) planets are small and made of heavy elements

– Outer (Jovian) planets are big and made of light elements

• Other bodies in the Solar system– There are seven large satellites (like the moon)

– Asteroids in Asteroid Belt between Mars and Jupiter

– Outer solar system is populated by TNO and comets

• How do we learn about solar system bodies?– We send probes

– Spectroscopy reveals the composition of atmospheres

– Craters are erased by plate geological processes

– Magnetic fields reveal the presence of a rotating liquid core

Page 3: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

The Diversity of the Solar System Results from Its Origin and Evolution

Page 4: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 5: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Today on Astro-1

The origin of the solar system

How old?

What did it form from?

How did it form?Clues from our solar system

Clues from other worlds

You’re Invited to a Special Event

Viewing of Today’s Partial Solar Eclipse!

Instructions to follow at the end of class.

Page 6: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

A meteorite: the surface shows evidence of having been melted by air friction as it entered our atmosphere at 40,000 km/h (25,000 mi/h). Meteorites are the oldest objects in the solar system.

Page 7: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

• Each type of radioactive nucleus decays at its own characteristic rate, called its half-life, which can be measured in the laboratory• This is used in radioactive age-dating to determine the ages of rocks• Age of oldest rocks in the solar system:

4.56 x 109 years

Page 8: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 9: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

The dying star Antares is shedding material from its outer layers, forming a thin cloud around the star.

Antares

Dust that used to be in Antares

Page 10: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

The abundances of the 30 lightest elements

Made in stars

All elements heavier than zinc (Zn) have abundances of fewer than1000 atoms per 1012 atoms of hydrogen.

Page 11: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 12: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Origin of the Chemical Elements(iclicker Question)

How has the present mix of chemical elements in the Universe been produced?

A) All the known elements have been formed by the radioactive breakup of the heavy elements formed in the initial Big BangB) All of the known elements were formed in the Big Bang.C) H and He were formed in the Big Bang, while the heavier elements have been slowly forming by collisions in cold interstellar gas cloudsD) H and some He were formed in the Big Bang, while the heavier elements have been slowly formed in the centers of stars over the life of the Universe.E) All the known elements were formed inside stars.

Page 13: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

The formation of the sun and its planets

Page 14: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Gravity Causes Interstellar Gas Clouds to Collapse

Page 15: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Planets Form Out of Gas Disks

Page 16: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 17: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Taking a Closer Look at a Stellar Nursery

Page 18: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 19: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Planets Are Likely Forming in These Disks

Page 20: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Inner Region: Only rocky and metallic materials remained solidOuter Region: Icy frost condensed beyond the snowline providing more mass for planet building.

Heat from the Hot Protosun Separated the Solar Nebular into Two Regions

Page 21: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 22: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 23: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Accretion of the Terrestrial Planets

Page 24: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Core accretion Theory vs Disk instability theory for Jovian planets

Page 25: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Planetary Migration

Page 26: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Planetary Migration

Page 27: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

A Smashed Up Planetesimal

Page 28: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

This highly magnified image showsa microscopic dust grain that came from interplanetary space. It entered Earth’s upper atmosphere and was collected by a high-flying aircraft. Dust grains of this sort are abundant in star-forming regions like the Orion nebula. These tiny grains were also abundant in the solar nebula and served as the building blocks of the planets.

Stardust – mission to collect dust from interplanetary space and Comet Wild 2.

Page 29: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

The Kuiper Belt: The gravitational influence of the Jovian planets pushed small, icy objects to the outer reaches of the solar system past Neptune. The result shown in this artist’s conception is the Kuiper belt, a ring populated by trans-Neptunian objects like Pluto, icy planetesimals, and dust.

Page 30: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 31: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 32: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

How did the Earth form?(iclickers Question)

• The formation of terrestrial planets around a star is thought to have occurred by what process?• A) Breakup of a large disk of matter which formed

around the star• B) Condensation of gas from the original star nebula• C) Capture by the star of objects traversing the depths

of space• D) Accretion or slow accumulation of smaller particles

by mutual gravitational attraction

Page 33: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Formation of Jupiter(iclickers Question)

• In order for the disk instability model to be able to account for the formation of the Jovian planets• A) The rocky material would have to be confined

completely to the inner parts of the solar system• B) The gas in the nebular disk would have to be at the

very high temperature• C) The gas in the nebular disk would have to be

clumpy rather than smooth • D) The gas in the nebular disk would have to be mostly

methane and ammonia rather than hydrogen and helium

Page 34: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Evidence from other worlds

Page 35: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Four Planets Orbit the Star HR 8799

Page 36: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

First Extrasolar Planet Visible in a Telescope Image

Page 37: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Detecting a Planet by Measuring Its Parent Star’s Motion

Page 38: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

The Wobble of 51 Pegasi

Page 39: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Many planets about the size of Jupiter orbit closer to their star than Mercury does to our Sun!

Hot Jupiters

Page 40: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 41: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Earth-Size Exoplanets

Page 42: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 43: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 44: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014
Page 45: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Summary

Solar System Formation: the nebular hypothesis.

The Sun:formed by gravitational contraction of the center of the nebula.

Terrestrial planets: formed through accretion of dust particles into planetesimals,

then into larger protoplanets.

Jovian planets:Began as rocky protoplanetary cores, similar in character to the

terrestrial planets. Gas then accreted onto these cores.

Alternatively, they formed directly from the gases of the solar nebula. In this model the cores formed from planetesimals falling into the planets.

Page 46: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

Homework

• Do all review questions from chapter 8 on your own.

• For TAs, do 8.46, 8.47, 8.49, 8.50

• Note: For Thursday October 30th, please read chapter 10 “Our Moon”.

Page 47: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

First Midterm on Tuesday!• You may use a calculator. Bring one.• Yes, graphing calculators are fine.

• No, you may not use a calculator application on your smartphone nor any other device that can connect to the internet.

• Exam has 50 multiple choice questions.• You must bring a ParSCORE sheet.

• You must bring a #2 pencil.

• Exam will include the equation sheet.• See example on course webpage.

• Do not bring an equation sheet.

Page 48: Astronomy 1 – Fall 2014 Lecture 7: October 23, 2014

How Should You Study?

• Go over the Key Ideas at the end of chapters 1-8.

• Go over the Review Questions for ch. 1-8.

• Go over the homework solutions for ch. 1-8.• We only grade a subset of the problems.

• You need to ‘check’ the solutions to the other problems yourself.

• Exam tests whether you understand the concepts and can apply them.

• It is not intended to be about memorization.