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Page 1 Lecture 14: Lecture 14: Asteroids, Comets, and Pluto-Charon Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Page 1: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Lecture 14:Lecture 14:Asteroids, Comets, and Pluto-CharonAsteroids, Comets, and Pluto-Charon

Claire MaxMay 19, 2009

Astro 18: Planets and Planetary SystemsUC Santa Cruz

Page 2: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Outline of lectureOutline of lecture

• Overall significance of comets and asteroids Overall significance of comets and asteroids

• AsteroidsAsteroids

• Pluto and CharonPluto and Charon– The great “Planet Debate”The great “Planet Debate”– Two asteroids who went astray?Two asteroids who went astray?

• CometsComets

Please remind me to take a break at 2:45 pm

Page 3: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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First, some definitionsFirst, some definitions

• AsteroidAsteroid: a : a rockyrocky leftover planetesimal orbiting the Sun leftover planetesimal orbiting the Sun

• CometComet: an : an icyicy leftover planetesimal orbiting the Sun leftover planetesimal orbiting the Sun (regardless of whether it has a tail!)(regardless of whether it has a tail!)

• MeteorMeteor: a flash of light in the sky caused by a particle : a flash of light in the sky caused by a particle or chunk of rock entering the atmosphere. May come or chunk of rock entering the atmosphere. May come from comet or asteroid.from comet or asteroid.

• MeteoriteMeteorite: any piece of rock that fell to the ground from : any piece of rock that fell to the ground from space, whether from an asteroid, comet, or even from space, whether from an asteroid, comet, or even from another planetanother planet

Page 4: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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The Main PointsThe Main Points

• Asteroids and comets are leftovers from the early Solar System

– Studying them can tell us about Solar System origins

• Asteroids– Failed planetesimals in outer Solar System

– Most have fairly circular orbits

– Life stories dominated by collisions, orbital perturbations by Jupiter

Page 5: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Main Points, continuedMain Points, continued

• Comets–“Dirty snowballs” - rock and ice–Highly elliptical orbits–Develop tail when near Sun–Observe Kuiper belt, infer Oort Cloud of comets beyond Pluto’s orbit

• Pluto and Charon–Many characteristics in common with asteroids in the Kuiper Belt

–Main unusual characteristic: it’s a bit bigger than other Kuiper Belt objects

Page 6: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Significance of comets and asteroidsSignificance of comets and asteroids

• Possible future collisions with EarthPossible future collisions with Earth– We will discuss this in a future lectureWe will discuss this in a future lecture

• Understanding the Solar System’s originsUnderstanding the Solar System’s origins– Both asteroids and comets are left over from the Both asteroids and comets are left over from the

birth of the Solar Systembirth of the Solar System– Bodies that never coalesced into planetsBodies that never coalesced into planets– Many remain virtually unchanged from 4.5 billion Many remain virtually unchanged from 4.5 billion

years agoyears ago– Most of our modern theories of Solar System Most of our modern theories of Solar System

formation were developed based on evidence from formation were developed based on evidence from asteroids and cometsasteroids and comets

Page 7: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Some asteroids photographed by Some asteroids photographed by spacecraft (up close)spacecraft (up close)

a) Gaspra (16 km)b) Ida (53 km) and tiny Dactyl

Mathilde (59 km)Eros (40 km)

Page 8: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Naming asteroidsNaming asteroids

• Discoverer has privilege of suggesting name to a Discoverer has privilege of suggesting name to a committee of International Astronomical Union.committee of International Astronomical Union.

• Contrary to recent media reports it is not possible to Contrary to recent media reports it is not possible to buy a minor planet. buy a minor planet.

• Number before name is order in which asteroid was Number before name is order in which asteroid was discovereddiscovered

• Rock stars are well represented! Rock stars are well represented!

http://cfa-www.harvard.edu/iau/special/rocknroll/RockAndRoll.html

• Rogue's gallery of asteroids, in numerical order, atRogue's gallery of asteroids, in numerical order, athttp://www.geocities.com/zlipanov/selected_asteroids/selected_asteroids.html

Page 9: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Asteroids as seen from EarthAsteroids as seen from Earth

Vesta (525 km)Keck Tel. Adaptive Optics.

Movie in spectral line of pyroxene.

A piece of Vesta landed on Earth as a meteorite!

Made almost entirely of pyroxene.

Page 10: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Asteroids as seen from spaceAsteroids as seen from space

• NEAR spacecraft NEAR spacecraft orbited asteroid orbited asteroid Eros, then Eros, then landed on it!landed on it!

Page 11: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Asteroids as seen from spaceAsteroids as seen from space

• NEAR spacecraft orbited asteroid Eros, then NEAR spacecraft orbited asteroid Eros, then landed on it!landed on it!

Page 12: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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The asteroid beltThe asteroid belt

• Between orbits of Mars Between orbits of Mars and Jupiterand Jupiter

• ““Should” be a planet thereShould” be a planet there

• But Jupiter’s gravitational But Jupiter’s gravitational perturbations probably perturbations probably prevented coalescence prevented coalescence into a planetinto a planet

Cartoon

Page 13: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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The asteroid belt: actual positionsThe asteroid belt: actual positions

Trojan asteroids

Page 14: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Diagram of Trojan asteroid Diagram of Trojan asteroid positionspositions

• Same distance from Same distance from Sun as Jupiter, but 60 Sun as Jupiter, but 60 deg ahead or behinddeg ahead or behind

• Any asteroid that Any asteroid that wanders away from one wanders away from one of the these two areas of the these two areas is nudged back by is nudged back by Jupiter’s gravityJupiter’s gravity

• Only a fraction of the Only a fraction of the Trojan asteroids have Trojan asteroids have been discovered yet - been discovered yet - very far away!very far away!

Page 15: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Orbital resonances with Jupiter play role Orbital resonances with Jupiter play role in structure of asteroid beltin structure of asteroid belt

Orbital period of

asteroid orbital period of Jupiter

Page 16: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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More detailed view: gaps due to More detailed view: gaps due to orbital resonancesorbital resonances

Page 17: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Physics of orbital resonancesPhysics of orbital resonances

• Orbital resonance:Orbital resonance:– Whenever one object’s orbital period is a simple Whenever one object’s orbital period is a simple

ratio of another object’s orbital periodratio of another object’s orbital period

• For asteroids, Jupiter is the “other object”For asteroids, Jupiter is the “other object”

• At an orbital resonance, the asteroid and At an orbital resonance, the asteroid and Jupiter periodically line up with each otherJupiter periodically line up with each other– The extra gravitational attraction makes small The extra gravitational attraction makes small

changes to the asteroid’s orbit over and over againchanges to the asteroid’s orbit over and over again– Eventual result is to “nudge” asteroid out of Eventual result is to “nudge” asteroid out of

resonant position, form gapresonant position, form gap

Page 18: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Orbital resonances: a resonant system Orbital resonances: a resonant system forced at its natural frequencyforced at its natural frequency

• Like pushing a pendulum in Like pushing a pendulum in time with its natural swingtime with its natural swing

• A small push, repeated many A small push, repeated many times, can add a lot of energy times, can add a lot of energy to the pendulumto the pendulum

• In case of asteroid, pushes In case of asteroid, pushes change its orbit until it is no change its orbit until it is no longer resonant with Jupiterlonger resonant with Jupiter

Page 19: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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How did asteroid belt get there in How did asteroid belt get there in the first place?the first place?

• Current asteroid belt has total mass 5 x 10Current asteroid belt has total mass 5 x 10-4-4 x mass of Earth x mass of Earth

• Several lines of evidence suggest that the original asteroid Several lines of evidence suggest that the original asteroid belt was belt was 100 - 1000 times more massive100 - 1000 times more massive

• But once Jupiter fully formed (after ~ 10 million years), its But once Jupiter fully formed (after ~ 10 million years), its gravity strongly perturbed the orbits of almost all the asteroidsgravity strongly perturbed the orbits of almost all the asteroids

• Most of them got nudged into highly eccentric orbits, from Most of them got nudged into highly eccentric orbits, from which they either leave the Solar System or head inwards which they either leave the Solar System or head inwards toward the Suntoward the Sun

• A fraction of the asteroids headed inwards may have hit the A fraction of the asteroids headed inwards may have hit the early Earth!early Earth!

Page 20: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Asteroids are quite far apartAsteroids are quite far apart (not like in Star Wars) (not like in Star Wars)

• About 100,000 asteroids larger than 1 kmAbout 100,000 asteroids larger than 1 km

• Not much mass: if gathered in a sphere, they would Not much mass: if gathered in a sphere, they would make a body less than 1000 km in diametermake a body less than 1000 km in diameter

• Mean distance between asteroids is Mean distance between asteroids is several million km!several million km!

• If you were on an asteroid and looked up, you would If you were on an asteroid and looked up, you would see at most one other asteroid with your naked eyesee at most one other asteroid with your naked eye

• Bennett estimates there is ONE major collision in the Bennett estimates there is ONE major collision in the asteroid belt every 100,000 yearsasteroid belt every 100,000 years

• David Morrision estimates that an average 1-km David Morrision estimates that an average 1-km asteroid suffers ~2 collisions in life of Solar Systemasteroid suffers ~2 collisions in life of Solar System

Page 21: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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How do we study asteroids?How do we study asteroids?

• Detection: streaks on time-Detection: streaks on time-exposed imagesexposed images

• Spacecraft: directly Spacecraft: directly measure size, shape, etc measure size, shape, etc (only a handfull of (only a handfull of asteroids so far)asteroids so far)

Page 22: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Finding asteroids: they move fast Finding asteroids: they move fast with respect to the starswith respect to the stars

Page 23: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Studying asteroids, continuedStudying asteroids, continued

• Can bounce radar off asteroid, receive back at Can bounce radar off asteroid, receive back at Earth. Measures speed, shape.Earth. Measures speed, shape.

• Example: KleopatraExample: Kleopatra

Page 24: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Asteroid Toutatis: shape and Asteroid Toutatis: shape and rotation from radar imageryrotation from radar imagery

Page 25: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

Source: E. Asphaug, Scientific American

Page 26: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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ConcepTestConcepTest

• We've seen that many asteroids look like lumpy We've seen that many asteroids look like lumpy potatoes (very irregular shapes). potatoes (very irregular shapes).

• But some, such as Vesta, are pretty round.But some, such as Vesta, are pretty round.

• What physical properties could cause an What physical properties could cause an asteroid to be round?asteroid to be round?

Page 27: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Asteroid categories and Asteroid categories and characteristicscharacteristics

• Can categorize asteroids by albedo (reflectance)Can categorize asteroids by albedo (reflectance)

– Dark (low reflectance): C (carbon)Dark (low reflectance): C (carbon)– Medium reflectance: M (metallic)Medium reflectance: M (metallic)– High reflectance: S (silicates, rock)High reflectance: S (silicates, rock)– Meteorites hitting Earth have same categories!Meteorites hitting Earth have same categories!

• Categories correlate with distance from SunCategories correlate with distance from Sun

Page 28: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Binary asteroids give unique Binary asteroids give unique informationinformation

• Period of companion Period of companion mass of primary mass of primary

• Size of primary + mass Size of primary + mass avg density of primary avg density of primary

• Addresses important question: are asteroids “solid”, or Addresses important question: are asteroids “solid”, or are they “rubble piles” ?are they “rubble piles” ?

• About 30 asteroids are known to have companionsAbout 30 asteroids are known to have companions

Ida

Dactyl

Page 29: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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The few asteroid binaries analyzed The few asteroid binaries analyzed so far are not very denseso far are not very dense

• Example: EugeniaExample: Eugenia

– Made of carbonaceous Made of carbonaceous material, should have high material, should have high densitydensity

– Yet measured density is Yet measured density is only a bit higher than that only a bit higher than that of water!of water!

– Conclusion: Eugenia is a Conclusion: Eugenia is a loosely bound pile of loosely bound pile of individual pieces, with individual pieces, with cracks (“voids”) in cracks (“voids”) in betweenbetween

Page 30: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

The life story of an asteroid?The life story of an asteroid?Source: E. Asphaug, Scientific American

Page 31: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Computer simulation of asteroid-Computer simulation of asteroid-asteroid collision (E. Asphaug)asteroid collision (E. Asphaug)

Page 32: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Tidal formation of binary asteroids?Tidal formation of binary asteroids?

Page 33: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Differentiation in asteroidsDifferentiation in asteroids

• Most asteroids were not heated beyond stage a)Most asteroids were not heated beyond stage a)

• Vesta reached stage b)Vesta reached stage b)

• M and S type asteroids c) (M = metal)M and S type asteroids c) (M = metal)

Primitive, undifferentiated

Iron separates, sinks. Core forms.

Collisions expose iron core

Page 34: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Near Earth Asteroids: perturbed out Near Earth Asteroids: perturbed out of asteroid belt by Jupiterof asteroid belt by Jupiter

Page 35: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Pluto: Not Alone Any MorePluto: Not Alone Any More

Goals for learning:Goals for learning:

• How big can a comet be?How big can a comet be?

• What are the large objects of the Kuiper belt What are the large objects of the Kuiper belt like?like?

• Are Pluto and Eris planets?Are Pluto and Eris planets?

Page 36: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Pluto is not alonePluto is not alone

Claire Max
update this image
Page 37: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Pluto and Charon: orbit is elliptical, Pluto and Charon: orbit is elliptical, out of plane of rest of Solar Systemout of plane of rest of Solar System

• Pluto wasn't discovered till 1930!Pluto wasn't discovered till 1930!

Page 38: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Pluto and CharonPluto and Charon

• Pluto's avg density ~ 2 g/ cmPluto's avg density ~ 2 g/ cm33..– Pluto is 50% to 75% rock mixed with ices.Pluto is 50% to 75% rock mixed with ices.

• Charon's density is ~1.6 g/cmCharon's density is ~1.6 g/cm33, indicating it contains , indicating it contains little rock. little rock.

• Differences in density tell us that Pluto and Charon Differences in density tell us that Pluto and Charon formed independentlyformed independently

Page 39: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Pluto has an atmosphere Pluto has an atmosphere (sometimes)(sometimes)

• Pluto's icy surface: Pluto's icy surface:

– 98% nitrogen (N98% nitrogen (N22).).

– Methane (CHMethane (CH44), carbon monoxide (CO), H), carbon monoxide (CO), H22OO

– Solid methane Solid methane Pluto's surface is colder than 70 Kelvin. Pluto's surface is colder than 70 Kelvin.

• Pluto's temperature varies widely during the course of Pluto's temperature varies widely during the course of its orbit since Pluto can be as close to the sun as 30 its orbit since Pluto can be as close to the sun as 30 AU and as far away as 50 AU. AU and as far away as 50 AU.

• Hence is a thin atmosphere that freezes and falls to the Hence is a thin atmosphere that freezes and falls to the surface as the planet moves away from the Sun. surface as the planet moves away from the Sun.

Page 40: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Is Pluto just the largest Kuiper Belt Is Pluto just the largest Kuiper Belt Object?Object?

• Orbits in same vicinity as Kuiper Belt cometsOrbits in same vicinity as Kuiper Belt comets

• Comet-like compositionComet-like composition

• Stable orbital resonance with Neptune, like many Stable orbital resonance with Neptune, like many cometscomets

• But: Pluto is much more highly reflectiveBut: Pluto is much more highly reflective

– Perhaps ices that sublime when Pluto is closer to Sun stay Perhaps ices that sublime when Pluto is closer to Sun stay with Pluto, and re-freeze on surface, whereas they are lost to with Pluto, and re-freeze on surface, whereas they are lost to less-massive comets.less-massive comets.

• One theory is that Charon was formed from Pluto in One theory is that Charon was formed from Pluto in same way our Moon was formed from Earth mantle same way our Moon was formed from Earth mantle materialmaterial

Page 41: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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NASA missions to Pluto have NASA missions to Pluto have had a checkered historyhad a checkered history

• The only planet that hasn't been explored by a The only planet that hasn't been explored by a spacecraftspacecraft

• Initially planned missions were cancelledInitially planned missions were cancelled

• Latest version: New Horizons Pluto Kuiper Belt Latest version: New Horizons Pluto Kuiper Belt MissionMission– Launched to Pluto by way of Jupiter in January Launched to Pluto by way of Jupiter in January

2006. 2006. – New Horizons passed through the Jupiter system New Horizons passed through the Jupiter system

at 50,000 mph, ending up on a path that will get at 50,000 mph, ending up on a path that will get the spacecraft to Pluto and Charon in July 2015the spacecraft to Pluto and Charon in July 2015

– Then it will explore a Kuiper Belt Object Then it will explore a Kuiper Belt Object

Page 42: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Hubble’s view of Pluto & its MoonsHubble’s view of Pluto & its Moons

Page 43: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Are Pluto and Eris planets?Are Pluto and Eris planets?

Claire Max
update this image
Page 44: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Is Pluto a Planet?Is Pluto a Planet?

• By far the smallest planet By far the smallest planet – Pluto’s size was overestimated after its discovery in Pluto’s size was overestimated after its discovery in

19301930

• Not a gas giant like other outer planetsNot a gas giant like other outer planets

• Has an icy composition like a cometHas an icy composition like a comet

• Has a very elliptical, inclined orbitHas a very elliptical, inclined orbit

• Pluto has more in common with comets than Pluto has more in common with comets than with the eight major planetswith the eight major planets

Page 45: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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What is a planet?What is a planet?

• International Astronomical Union meeting in International Astronomical Union meeting in Prague 3 years ago Prague 3 years ago

• Agreed that a "planet" is defined as a celestial Agreed that a "planet" is defined as a celestial body that body that

(a) is in orbit around the Sun(a) is in orbit around the Sun

(b) has sufficient mass for its self-gravity to overcome (b) has sufficient mass for its self-gravity to overcome rigid body forces so that it assumes a hydrostatic rigid body forces so that it assumes a hydrostatic equilibrium (nearly round) shape, and equilibrium (nearly round) shape, and

(c) has cleared the neighborhood around its orbit. (c) has cleared the neighborhood around its orbit.

Slide credit: John Wilson, Georgia State U.

Page 46: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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What is a planet?What is a planet?

Page 47: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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What is Pluto? IAU decision, cont’dWhat is Pluto? IAU decision, cont’d

• Defined new class of objects called "dwarf planets"Defined new class of objects called "dwarf planets"

• ““Planets" and "dwarf planets" are two distinct classes Planets" and "dwarf planets" are two distinct classes

• First members of the "dwarf planet" category are First members of the "dwarf planet" category are Ceres, Pluto and 2003 UB313 (Eris)Ceres, Pluto and 2003 UB313 (Eris)

• More "dwarf planets" are expected to be announced by More "dwarf planets" are expected to be announced by the IAU in the coming years the IAU in the coming years

– Currently a dozen candidate "dwarf planets" are on Currently a dozen candidate "dwarf planets" are on IAU's "dwarf planet" watch listIAU's "dwarf planet" watch list

– Keeps changing as new objects are foundKeeps changing as new objects are found

• ””Dwarf planet" Pluto is recognized as an important Dwarf planet" Pluto is recognized as an important proto-type of a new class of trans-Neptunian objects proto-type of a new class of trans-Neptunian objects

Slide credit: John Wilson, Georgia State U.

Page 48: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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What have we learned?What have we learned?

• How big can a comet be?How big can a comet be?– The Kuiper belt from which comets come contains The Kuiper belt from which comets come contains

objects as large as Pluto.objects as large as Pluto.

• What are the large objects of the Kuiper belt What are the large objects of the Kuiper belt like?like?

– Large objects in the Kuiper belt have orbits and icy Large objects in the Kuiper belt have orbits and icy compositions like those of comets.compositions like those of comets.

• Are Pluto and Eris planets?Are Pluto and Eris planets?– While the IAU considers Pluto and Eris to be “dwarf While the IAU considers Pluto and Eris to be “dwarf

planets”, the topic is still under some debate. planets”, the topic is still under some debate.

Page 49: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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CometsComets

Goals for learning:Goals for learning:

• What are comets like?What are comets like?

• Where do comets come from?Where do comets come from?

Page 50: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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What are comets like?What are comets like?

Page 51: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Comet FactsComet Facts

• Formed beyond the frost line, comets are icy Formed beyond the frost line, comets are icy counterparts to asteroidscounterparts to asteroids

• Nucleus of comet is a “dirty snowball” (ice with rock)Nucleus of comet is a “dirty snowball” (ice with rock)

• Most comets do not have tailsMost comets do not have tails

• Most comets remain perpetually frozen in the outer Most comets remain perpetually frozen in the outer solar system solar system

• Only comets that enter the inner solar system grow Only comets that enter the inner solar system grow tailstails

Page 52: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Sun-grazing CometSun-grazing Comet

Page 53: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Nucleus of a Comet, from Nucleus of a Comet, from a close-up spacecrafta close-up spacecraft

• A “dirty snowball”A “dirty snowball”

• Source of material Source of material for comet’s tailfor comet’s tail

Page 54: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Deep Impact Spacecraft sent Deep Impact Spacecraft sent projectile into Comet Tempel 1projectile into Comet Tempel 1

• Mission to study Mission to study nucleus of Comet nucleus of Comet Tempel 1Tempel 1

• Projectile hit surface Projectile hit surface on July 4, 2005on July 4, 2005

• Recorded by the Recorded by the “mother ship”“mother ship”

• Many telescopes Many telescopes from Earth studied from Earth studied aftermath of impactaftermath of impact

Page 55: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Anatomy of a CometAnatomy of a Comet

• Gas “coma”Gas “coma” is is atmosphere that atmosphere that comes from heated comes from heated nucleusnucleus

• Plasma tailPlasma tail is gas is gas escaping from escaping from coma, pushed by coma, pushed by solar windsolar wind

• Dust tailDust tail is pushed is pushed by photons from the by photons from the SunSun

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Length of comet tail is hugeLength of comet tail is huge

• Tail size many millions Tail size many millions of kmof km

• By comparison, Jupiter By comparison, Jupiter is about 150,000 km in is about 150,000 km in diameterdiameter

Page 57: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Tail grows as comet comes Tail grows as comet comes closer to Suncloser to Sun

Page 58: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

Comets eject small particles that follow the comet around in its orbit and cause meteor showers when Earth crosses the comet’s orbit.

Page 59: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Where do comets come from?Where do comets come from?

Page 60: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

Kuiper belt:On orderly orbits from 30-100 AU in disk of solar system

Oort cloud:On random orbits extending to about 50,000 AU

Very few comets enter inner solar system - most stay far from the Sun

Page 61: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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How did they get there?How did they get there?

• Kuiper belt cometsKuiper belt comets formed in the Kuiper belt: formed in the Kuiper belt: flat plane, aligned with plane of Solar System, flat plane, aligned with plane of Solar System, orbiting in same direction as the planets.orbiting in same direction as the planets.

• Oort cloud cometsOort cloud comets were once closer to the were once closer to the Sun, but they were kicked out there by Sun, but they were kicked out there by gravitational interactions with jovian planets: gravitational interactions with jovian planets: spherical distribution, orbits in any direction.spherical distribution, orbits in any direction.

Page 62: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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The Oort Cloud is almost spherical, The Oort Cloud is almost spherical, beyond orbit of Plutobeyond orbit of Pluto

• In 1950 Jan Oort noticed thatIn 1950 Jan Oort noticed that– no comet orbit observed no comet orbit observed

suggesting it came from suggesting it came from interstellar spaceinterstellar space

– strong tendency for aphelia of strong tendency for aphelia of long period comet orbits to lie at long period comet orbits to lie at distance ~ 50,000 AUdistance ~ 50,000 AU

– there is no preferential direction there is no preferential direction from which comets come.from which comets come.

• He proposed that comets He proposed that comets reside in a vast cloud at the reside in a vast cloud at the outer reaches of the solar outer reaches of the solar systemsystem

• Up to a trillion comets in Oort Up to a trillion comets in Oort cloud!cloud!

Page 63: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

Kuiper belt:On orderly orbits from 30-100 AU in disk of solar system

Oort cloud:On random orbits extending to about 50,000 AU

Only tiny number of comets enter inner solar system - most stay far from the Sun

Page 64: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Comet nucleusComet nucleus

Nucleus of Halley’s Comet

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Dust is ejected from nucleus as it Dust is ejected from nucleus as it heats up, makes comet tailheats up, makes comet tail

Electron Electron microscope microscope

image of dustimage of dust

Page 66: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Concept QuestionConcept Question

• Remembering the division between the inner Remembering the division between the inner Solar System's rocky "terrestrial planets" and Solar System's rocky "terrestrial planets" and the outer Solar System's icy satellites, where in the outer Solar System's icy satellites, where in the Solar System might comets have originally the Solar System might comets have originally formed?formed?

Page 67: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Stardust spacecraft has flown to a Stardust spacecraft has flown to a comet, brought dust back to Earthcomet, brought dust back to Earth

Stardust images of the nucleus

Page 68: Page 1 Lecture 14: Asteroids, Comets, and Pluto-Charon Claire Max May 19, 2009 Astro 18: Planets and Planetary Systems UC Santa Cruz

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Stardust spacecraft, continuedStardust spacecraft, continued

• Gathered cometary dust using Gathered cometary dust using aerogelaerogel targets targets

– The least dense substance that is still solidThe least dense substance that is still solid

• Brought back to Earth, being analyzedBrought back to Earth, being analyzed

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The Main PointsThe Main Points

• Asteroids and Comets: leftovers from early Solar System

• Asteroids– Failed rocky planetesimals in outer Solar System– Didn't form planets because Jupiter kept stirring the pot

– Most have fairly circular orbits– Dominated by collisions, orbital perturbations by Jupiter

• Comets– “Dirty snowballs” - icey, develop tail when near Sun

– Highly elliptical orbits; Observe Kuiper belt, infer Oort Cloud

• Pluto and Charon– Pluto as the largest Kuiper Belt object? Prototype of new class of dwarf planets