Characteristic Properties- Solar System 1. Planets isolated in space=cleared orbit 2. Disk shape of solar system- small orbit inclination; prograde

Similar documents
Solar System. Sun, 8 planets, hundred moons, thousand.dwarf.planets million asteroids, billion comets etc.

Extrasolar Planets = 403

Chapter 15: The Origin of the Solar System

Comparative Planetology I: Our Solar System

Chapter 19 The Origin of the Solar System

9/22/ A Brief Tour of the Solar System. Chapter 6: Formation of the Solar System. What does the solar system look like?

What is it like? When did it form? How did it form. The Solar System. Fall, 2005 Astronomy 110 1

Chapter 8 Lecture. The Cosmic Perspective Seventh Edition. Formation of the Solar System

Astronomy. physics.wm.edu/~hancock/171/ A. Dayle Hancock. Small 239. Office hours: MTWR 10-11am

-Melissa Greenberg, Arielle Hoffman, Zachary Feldmann, Ryan Pozin, Elizabeth Weeks, Christopher Pesota, & Sara Pilcher

1star 1 star 9 8 planets 63 (major) moons asteroids, comets, meteoroids

Formation of the Solar System Chapter 8

Making a Solar System

Origin of the Solar System

9. Formation of the Solar System

Radioactive Dating. U238>Pb206. Halflife: Oldest earth rocks. Meteors and Moon rocks. 4.5 billion years billion years

What does the solar system look like?

The Solar Nebula Theory. This lecture will help you understand: Conceptual Integrated Science. Chapter 28 THE SOLAR SYSTEM

The Formation of the Solar System

The Coriolis effect. Why does the cloud spin? The Solar Nebula. Origin of the Solar System. Gravitational Collapse

Today. Solar System Formation. a few more bits and pieces. Homework due

Lecture Outlines. Chapter 15. Astronomy Today 7th Edition Chaisson/McMillan Pearson Education, Inc.

Comparative Planetology II: The Origin of Our Solar System. Chapter Eight

Solar System Formation

Planets: Name Distance from Sun Satellites Year Day Mercury 0.4AU yr 60 days Venus yr 243 days* Earth 1 1 yr 1 day Mars 1.

The History of the Solar System. From cloud to Sun, planets, and smaller bodies

Comparative Planetology II: The Origin of Our Solar System. Chapter Eight

Chapter Outline. Earth and Other Planets. The Formation of the Solar System. Clue #1: Planetary Orbits. Clues to the Origin of the Solar System

Astronomy 1 Winter Lecture 11; January

Solar System Formation

m V Formation of the Solar System and Other Planetary Systems Questions to Ponder about Solar System

Solar System Formation

Formation of the Solar System and Other Planetary Systems

m V Density Formation of the Solar System and Other Planetary Systems Questions to Ponder

Our Planetary System & the Formation of the Solar System

The Cosmic Perspective Seventh Edition. Asteroids, Comets, and Dwarf Planets: Their Natures, Orbits, and Impacts. Chapter 12 Review Clickers

3. Titan is a moon that orbits A) Jupiter B) Mars C) Saturn D) Neptune E) Uranus

Why are Saturn s rings confined to a thin plane? 1. Tidal forces 2. Newton s 1st law 3. Conservation of energy 4. Conservation of angular momentum

Astro 1: Introductory Astronomy

Starting from closest to the Sun, name the orbiting planets in order.

Formation of the Solar System. What We Know. What We Know

Chapter 4 The Solar System

Astronomy 405 Solar System and ISM

Chapter 15 The Formation of Planetary Systems

on it, can still ripen a bunch of grapes as though it had nothing else in the Universe to do. Galileo Galilei

HNRS 227 Fall 2006 Chapter 13. What is Pluto? What is a Planet? There are two broad categories of planets: Terrestrial and Jovian

Chapter 8 Formation of the Solar System

Which of the following statements best describes the general pattern of composition among the four jovian

Clicker Question: Clicker Question: Clicker Question:

The History of the Earth

Astronomy 1504 Section 10 Final Exam Version 1 May 6, 1999

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question.

Formation of the Solar System

Planetary Interiors. Earth s Interior Structure Hydrostatic Equilibrium Heating Constituent Relations Gravitational Fields Isostasy Magnetism

Lecture Outlines. Chapter 6. Astronomy Today 7th Edition Chaisson/McMillan Pearson Education, Inc.

Astronomy 103: First Exam

Astronomy A BEGINNER S GUIDE TO THE UNIVERSE EIGHTH EDITION

Earth Science 11 Learning Guide Unit Complete the following table with information about the sun:

Origin of the Solar System

Gravity: Motivation An initial theory describing the nature of the gravitational force by Newton is a product of the resolution of the

Test 2 Result: Sec 1. To see the scantron & problem set, contact the TA: Mr. He Gao

Nature and Origin of Planetary Systems f p "

Astronomy Ch. 6 The Solar System. MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question.

HW #2. Solar Nebular Theory. Predictions: Young stars have disks. Disks contain gas & dust. Solar System should contain disk remnants

Astronomy Ch. 6 The Solar System: Comparative Planetology

Origin of the Solar System

Comparative Planetology I: Our Solar System. Chapter Seven

Moon Obs #1 Due! Moon visible: early morning through afternoon. 6 more due June 13 th. 15 total due June 25 th. Final Report Due June 28th

The Big Bang Theory (page 854)

9.2 - Our Solar System

see disks around new stars in Orion nebula where planets are probably being formed 3

Solar System Formation/The Sun

Jovian Planet Properties

Ag Earth Science Chapter 23

OUR SOLAR SYSTEM. James Martin. Facebook.com/groups/AstroLSSC Twitter.com/AstroLSSC

23.1 The Solar System. Orbits of the Planets. Planetary Data The Solar System. Scale of the Planets The Solar System

1. Cosmology is the study of. a. The sun is the center of the Universe. b. The Earth is the center of the Universe

Brooks Observatory telescope observing this week

Chapter 11 Review Clickers. The Cosmic Perspective Seventh Edition. Jovian Planet Systems Pearson Education, Inc.

Chapter 19: Meteorites, Asteroids, and Comets

Astronomy Wed. Oct. 6

Prentice Hall EARTH SCIENCE

Class 15 Formation of the Solar System

Physics Homework 5 Fall 2015

Physics Homework 5 Fall 2015

Astronomy 405 Solar System and ISM

CHAPTER 11. We continue to Learn a lot about the Solar System by using Space Exploration

! Group project! a)! 65% b)! 70% c)! 75% d)! 80% e)! 85%

Two Kinds of Planets. "Terrestrial" "Jovian" Mercury, Venus, Earth, Mars. Jupiter, Saturn, Uranus, Neptune

Comparative Planetology I: Our Solar System. Chapter Seven

Overview of Solar System

The Solar System. Tour of the Solar System

Stellar Astronomy Sample Questions for Exam 3

The Solar Nebula Theory

Cosmology Vocabulary

Initial Conditions: The temperature varies with distance from the protosun.

The Solar System consists of

Solar System revised.notebook October 12, 2016 Solar Nebula Theory

The Planets. Discovering our Solar System. Chapter 6: The Solar System An Introduction to Comparative Planetology. What s in the Solar System?

At this point of its orbit, any solar satellite such as a comet or a planet is farthest away from the sun. What is the aphelion?

Transcription:

Characteristic Properties- Solar System 1. Planets isolated in space=cleared orbit 2. Disk shape of solar system- small orbit inclination; prograde circular motion; same tilt&direction of rotation axes (almost) 3. Jovian/Terrestrial planets: low/high density, huge/small atmospheres, fast/slower rotation rates, many/few moons & rings 4. Space Debris icy comets, rocky asteroids, meteoroids, Kuiper Belt 5. Common ages of Earth, Moon, Mars, meteorites, Sun

Tidal=Passing Star Hypothesis Buffon in 1745 Catastrophic process Low probability of encounter Hot gasses would dissipate before they could condense Predicts few stars with planets

Nebular Theory Descartes 1644 envisioned vortices Laplace 1796 added Newton s gravity Evolutionary process Sun and planets formed from a vast rotating cloud of gas and dust called the solar nebula

Solar Nebula All the stars form from dust clouds Most dust &gas falls on Protosun Cloud is spinning so dust falls in faster along poles forms protoplanetary disk Lumps in disk become planets Predicts the many stars with planets

Protoplanetary Disks =Proplyds Sun & planets clean out inner disk ending planet building 2MASS and Gemini AO observations of binary star with disk 5 disks in Orion Nebula

NOT evidence that the planets formed in a disk surrounding the Sun is: a) The planets orbits are inclined only a few degrees to the equator of the Sun (=ecliptic) b) The planets all orbit in the same direction as the Sun rotates c) We see protoplanetary disks around other stars in star formation regions d) We see many extrasolar planets as predicted by the Solar Nebula Theory which includes disks e) The Solar Nebula Theory by Laplace & Descartes

Kepler-56 Has 2 planets not in equatorial plane of star Companion star pulls on planets & misaligns them

Protosun Most of the material fell to the centre of the Solar Nebula forming the Sun in ~100 Million years Becoming a star with hydrogen fusion in its core

Condensation Theory Shuttle experiment done in no gravity found dust forms grains very quickly around condensation nuclei A layer of atoms condenses at a time to form snowflakes

Hot Disk and Frost Line (Snow Line) Gas & dust in solar nebula heated by protosun Nebula is hotter closer to sun and colder in outer orbits Beyond frost line, H 2 O forms snowflakes & Jupiter

Condensation Temperature Metals freeze out first, then rock, then ices Planets close to sun form from metals, then rocks, then ice Density of planets goes from dense to less dense Terrestrial to Jovian

Accretion Gradual growth by collision & sticking Snowflakes become snowballs

Planetesimals Eventually massive enough to grow by gravity A few kilometers in size Pandora & Hyperion; Low density moons of Saturn

Protoplanets The more massive they are the more planetesimals they collect; the faster they grow At more than 15 earth masses gravitational collapse starts Capturing Hydrogen and Helium directly from nebula

Core-Accretion / Gravitational Instability Model Disk blown away by sun and other stars in a few million years Core accretion model= (Iron+rock+ice) core then gas too slow Disk Instability=Density enhancement draws in gas directly from disk Movie by Phil Armitage 2005 shows density waves excited by planet

Migrating Planets Encounters with planetesimals sweep/ eject planetesimals into asteroid belt, Kuiper belt, Oort cloud Move Jovian planets out/in depending on if they pass in front or behind planet

Planetary Migration Jupiter and Saturn may have formed much further from Sun & moved in Uranus and Neptune moved further out from Sun

Fragmentation High speed collisions between protoplanets & planetesimals creates a debris disk P/2010A2 comet? Collision of 2 small asteroids

Debris Disk Not the dense protoplanetary disks that form planets Cold debris disks are left Made from asteroid, comet, planetesimal collisions

Large Impacts In final stages a planet would have had many collisions with bodies the size of planets Such impacts could tilt the rotation axis of Uranus, Pluto + rotation speed of Venus Solar system is like a full coffee cup some coffee probably got spilled

Processes That Cleared the Inner Solar System Radiation pressure from sun&stars Protosun s wind (&stellar) blows away gas & dust Planetesimals incorporated into planets or ejected All done in millions of years

Overview of Planet Formation Common orbital and rotation direction & plane =>protoplanetary disk Jovian / Terrestrial => range of temperatures in disk / frost line Interplanetary debris left over from formation = asteroids, comets, Common ages => simultaneous formation in disk Collisons of protoplanets = irregularities in Solar System

The main reason terrestrial planets are more dense than Jovian planets is: a) The Jovian planets migrated thru the disk more b) The Jovian planets formed outside the frost line c) The less dense compounds rose to the outer orbits d) The solar wind blew away the terrestrial planet s less dense elements e) The protosun absorbed all the less dense elements in the inner solar system so none were left for the terrestrial planets

Chemical Differentiation of Planets Young planet very hot due to impact heating (=heat of formation) +Radioactive decay in core of planet Iron, Nickel, Iridium settle to the core Silicates rise above iron Ices/water next

Outgassing Water, carbon dioxide, sulfur dioxide, nitrogen released by volcanoes Forms atmosphere

Angular Momentum Problem The protosun rotates rapidly and has huge convection cells so it generates a strong magnetic field The magnetic field tries to accelerate the disk and solar wind, slowing rotation by magnetic braking Observations of stars with known ages in Hyades etc. show that the older stars rotate more slowly

Late Heavy Bombardment Late Heavy Bombardment second surge in impacts When Jupiter, Saturn, Uranus, Neptune change orbits scattering planetesimals?

MOST: Jaymie Matthews UBC Observed HD209458 for months and Saw no eclipses from Earth sized planets Timed transits showing no Earth sized planets-so far No opposition effect so low 50% albedo

Comet Lulin Dirty Snowball or Icy Mudball Nucleus ~10km Tail ~1 million km 3572 comets 2000 short period

Comet NEAT 29Jan & 2Feb03 Dirty snowball or maybe icy mud ball is better Nucleus ~ 10km Tail ~1,000,000km to 1 astronomical unit Very eccentric elliptical orbit

Coronographic Image of Debris Disk Star is masked by black spot in original and untilted image Notice cleared inner disk(30au) and spiral wave features ~320 light years distance, 300AU diameter, 5 Million years old

Gravity Assist Throws ball on parked car Throws ball on moving car Throws ball on orbiting car

Impact Crater Formation Impactor has velocity 10 times rifle bullet Releases energy 10 times equal mass of dynamite Impactor vaporized when temperature reaches millions K Shock wave forms shocked quartz found only in impacts Rebound can launch rocks without destroying them

Rocky Surfaces Saturated with Craters Planets formed from many meteorite impacts Circular craters due to explosion caused by impact Solar System Full?

Erosion of Craters Craters hidden by: 1. Volcanoes lava flows 2. Continental drift 3. Erosion by atmosphere 4. Oceans

Younger Terrain = Fewer Craters The larger the terrestrial world; the more internal heat it will retain = higher temperature in core The higher temperature; more geologically active so more craters are covered = fewer craters showing Older terrains = more craters

Comet Impacts on Jupiter Painting shows Jul94 impacts of Comet Shoemaker-Levy 9 HST photo from 20Jul09 Comets deposit ice Heating planet

03Jun10 Jupiter Impact Last June Jupiter became a little more massive Two amateur astronomers recorded the impact 2009 impact left scar Notice missing SE belt

Planetary Magnetic Fields Jovian planets plus Earth have magnetic fields Various directions and strengths and offsets

Planetary Dynamo Conducting, convecting/circulating, rotating core generates magnetic field Earth: Iron core; Jupiter: liquid metallic hydrogen Uranus, Neptune: water with ions

Magnetometer Measures the strength & direction of Magnetic field Can probe the interior of the planet

Elemental Abundances Element determined by number of protons=atomic number Neutrons determine Isotope Elemental abundances on Earth Not the same as in stars, Jupiter, Saturn

Elements Forged In Star s Cores You are made of star dust Stars have died so you may live

Chondrules Many meteorites contain small glassy inclusions Formed by rapid melting and solidified in hours Chondrules date from formation of Solar System