Taking a Look at a Trojan Asteroid

Slides:



Advertisements
Similar presentations
Formation of the Solar System
Advertisements

The Edge of the Solar System The Oort Cloud. What is the Oort Cloud? Spherical area between 5,000 and 100,000 AU from the sun (Kuiper belt ends at 55.
Solar System Basics. Sun Inner Planets Mercury Mars Venus Earth.
Origin of the Solar System Astronomy 311 Professor Lee Carkner Lecture 8.
Asteroids By: Ethan and Kacey. What are they? Chunks of rock that measure in size from few feet to several miles in diameter Rocky remains from the formation.
Origin of the Solar System Astronomy 311 Professor Lee Carkner Lecture 8.
Origin of the Solar System Astronomy 311 Professor Lee Carkner Lecture 8.
The Terrestrial Planets Astronomy 311 Professor Lee Carkner Lecture 9.
The Terrestrial Planets Astronomy 311 Professor Lee Carkner Lecture 9.
ASTR-101 Section 020 Lecture 7 Comparative Planetology I: Our Solar System John T. McGraw, Professor Laurel Ladwig, Planetarium Manager.
Our Solar System I Origins of the Solar System Astronomy 12.
Introduction to the Solar System Chapter 6. The Sun.
Lesson 8a Moons, Asteroids and Rings. Europa These interactions also keep Europa in a slight elliptical orbit as well. But since Europa is farther from.
Lecture 34 The Outer Planets. The Moon. The Origin of the Moon The Outer Planet Family Chapter 16.9 
Comparative Planetology I: Our Solar System
Pre-solar nebula Protoplanetary disk: condensation and accretion Solar wind (beginning of fusion) Collisions continue Planetary migration (orbits shifting)
“ PHOBOS - SOIL ” Phobos Sample Return Mission 1. goals, methods of study A.Zakharov, Russian academy of sciences Russian aviation.
Comparative Planetology I: Our Solar System Chapter Seven.
Our Solar system YouTube - The Known Universe by AMNH.
Origin, Evolution, and Composition of the Atmosphere
Universe Eighth Edition Universe Roger A. Freedman William J. Kaufmann III CHAPTER 7 Our Solar System CHAPTER 7 Our Solar System.
Comparative Planetology I: Our Solar System. Guiding Questions 1.Are all the other planets similar to Earth, or are they very different? 2.Do other planets.
The Solar System Chapter 23, Section 1.
Forming Earth and Our Solar System By David and Jake Thank You!
Lecture 32: The Origin of the Solar System Astronomy 161 – Winter 2004.
Review Worksheet Solutions. 1. Describe the focus of comparative planetology and discuss its importance to solar system studies. Comparative planetology.
Universe Tenth Edition Chapter 7 Comparative Planetology I: Our Solar System Roger Freedman Robert Geller William Kaufmann III.
 The Sun  The Planets (Inner and Outer)  Satellites  Asteroids and Comets.
1 Chapter 13 Objectives: 1)List the major objects that make up our solar system. 2)Distinguish between a planet and a dwarf planet. 3)Define an Astronomical.
Warmup  What is the line of latitude that cuts through the center of the earth?  What is ZERO degrees longitude?  What is 180 degrees longitude?
The Formation of Our Solar System The Nebular Hypothesis.
Solar System Booklet Note: The information for Mercury to Neptune was available in the textbook, and is not listed in this presentation. Information on.
The Outer Planets. Discussion questions Compare and contrast the inner and outer planets? Compare and contrast the inner and outer planets? Why have we.
Our Solar System & Exoplanets (Chapter 15). Student Learning Objectives Identify and locate objects in our solar system Describe planet formation processes.
Comparative Planetology I: Our Solar System Chapter Seven.
Origins and Our Solar System
Habitable zone Earth: AU F. Marzari,
Unit 2 Lesson 6 Small Bodies in the Solar System
© 2017 Pearson Education, Inc.
Space.
Announcements Brooks Observatory tours (March )
Image of the day.
The Solar System: The Sun & the Planets
Overview of the Solar System
Section 2: The Inner and Outer Planets
The Solar System: The Sun & the Planets
THE SOLAR SYSTEM.
Meteors, Asteroids, & Comets
Inner Solar System (Terrestrial Planets)
Unit 3 Lesson 6 Small Bodies in the Solar System
Objects in Our Solar System
The Solar System 2014.
Solar System Formation
Solar System.
Comparative Planetology I: Our Solar System
Bell Ringer What is the order of the planets?
Small Solar System Bodies
Mrs. Niki Midyett 4th Grade Science.
Comparative Planetology I: Our Solar System
Asteroid Belt.
Meteors, Asteroids, & Comets
& Other Objects in Space
Any theory about the origin of the solar system must explain why all of the planets’ orbits lie more or less in a plane and all of the planets orbit the.
2. THE SOLAR SYSTEM’S EARLY HISTORY
3A Objectives Describe the nebular theory in detail.
1.1.1a and 1.1.1b ORIGIN OF THE EARTH’S MOTION BASED ON THE ORIGIN OF THE GALAXY AND SOLAR SYSTEM.
The Solar System 1 star 9 8 planets 63 (major) moons
The Structure of the Solar System
The Moon, Comets, and Asteroids
The archetype terrestrial planet
Presentation transcript:

Taking a Look at a Trojan Asteroid AJAX Mission Proposal Taking a Look at a Trojan Asteroid

Background •Group of asteroids that have the same orbit as Jupiter •Two stable La Grange points 60⁰ ahead (Trojans) and 60⁰ behind (Greeks)

Background They have orbits a little over 5 AU 6,704 found as of now Possibly over 1 million over 1km diameter and average rotational period of 11.2 hours These numbers are our best estimates ⅕ the mass of the asteroid belt

Background They have orbits a little over 5 AU 6,704 found as of now Possibly over 1 million over 1km diameter and average rotational period of 11.2 hours These numbers are our best estimates ⅕ the mass of the asteroid belt

Background Most are D-type asteroids Low albedo (~0.04) Reddish electromagnetic spectrum. Composed of: organic rich silicates, carbon, anhydrous silicates and maybe ice in the center. No probes have been sent to examine them yet

Background Most are D-type asteroids Low albedo (~0.04) Reddish electromagnetic spectrum. Composed of: organic rich silicates, carbon, anhydrous silicates and maybe ice in the center. No probes have been sent to examine them yet

Theories of Trojan Asteroids Formation Theory 1: Jupiter Capture Theory 2: Kuiper Belt and Planetary Migration

Theories of Trojan Asteroids Formation Theory 1: Jupiter Capture Theory 2: Kuiper Belt and Planetary Migration

Theories of Trojan Asteroids Formation Theory 1: Jupiter Capture Theory 2: Kuiper Belt and Planetary Migration

What we can learn: Formation of planets If asteroids are primordial objects, they may inform us of: The chemical/geological processes that changed the small bodies that later made up the planets

What we can learn: Terrestrial Materials The Jupiter trojans may inform us of: How volatiles, organic compounds, C, H, and prebiotic materials were delivered to the inner solar system during the Late Heavy Bombardment (LHB) The origin of the LMB (4.1-3.8 Ga)

AJAX’s Focused Payload Addresses: 2013-2022 Planetary Science Decadal Survey goals for Trojan missions: Geological Elemental composition Mineralogical Geophysical

Stage 1: Initial Approach Uses multispectral imaging at various phase angles to search for natural satellites and dust Could be signs of frequent comet impacts Determines shape and pole position of asteroid

Stage 2: Descent Into Lower Orbits Completes global mapping through high-resolution stereo and multispectral imaging Measures gravity field to determine density and estimate interior porosity

Stage 2: Descent Into Lower Orbits Creates a high-resolution representation of the surface during a low flyover Measures hydrogen abundance

Stage 3: Landed Package Measures abundance of 20 elements including C and H concentrations Measures physical and mechanical properties of asteroid’s regolith

What we learn from AJAX From composition measurement: Trojans’ possible role in delivering prebiotic materials to terrestrial planets From regolith and porosity measurements: How planetesimals form and merge into planets

Sustainability on Earth as a Result Would provide knowledge of planetary origins along with: The source of volatiles such as: Nitrogen Water Carbon Dioxide Organics on terrestrial planets

Sustainability as a Result Knowing how volatiles were formed can help learn about avoiding their destruction on Earth Could teach us about simulating the formation of these volatiles on Earth

Other Benefits Learning about how we came about and why Good return on investment High quality pictures and data of an unexplored area