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EART160 Planetary Sciences
Meteorites, Asteroids, and Minor Bodies
Meteorite-Asteroid Connections
From Kring (2006), Unlocking the solar system’s past, Astronomy, August, pp. 33-37.
Asteroid Belt
Formation/evolution• Mass: ~5% of Moon’s mass• Previously believed to be an exploded or
disrupted planet.• Now believed to closer to “failed planet.”• Gravitational perturbations by Jupiter prevented
final accretion of planetesimals and promoted large orbital changes, and ejections.– Initial mass of belt may have been 100-1000 times
greater.– Cleared within millions of years– Ceres (500 km radius) is the largest body left.
Historical aside: Titus Bode “Law” (year 1715)
Believed to be a coincidence, more of a “rule” than a “law.”Asteroid belt approximately takes the position of a predicted planet (Ceres discovered 1801)
Neptune doesn’t work (1846). Pluto? Not the best rule or law!
a = 0.4 + 0.3 2n
n = -inf, 0, 1, 2…
(k=2n)
Kirkwood Gaps – evidence of Jupiter’s effect
• Destabilizing mean motion resonances with Jupiter deplete zones of semimajor axis.
Lagrangian Points & Trojans
Definition: Points where the gravity of two large bodies provide a centripetal acceleration that permits a third body to remain stationary in a rotating reference frame.
Trojans (and Greek camp) – Dynamical group: occupy Sun-Jupiter L4 and L5.L4 and L5 are stable like the bottom of a valley (attractor)
L1-L3 points are stable like a ball on a hill (or ridge)
Hildas – dynamical group
• 3:2 Mean motion resonance with Jupiter• Smaller semi-major axis than the Trojans• Moderate eccentricities• Triangular distribution
Large asteroids
Now a dwarf planet
Ceres (more later)
Hubble image, contrast enhanced
Dwarf Planet Definition
• International Astronomical Union (IAU): A celestial body orbiting a star that is massive enough to be spherical as a result of its own gravity, but has not cleared its neighboring region of planetesimals and is not a satellite.– Hydrostatic equilibrium
• Problems with this definition?• Still debated
Dwarf Planets
Name Region ofSolar System
Orbitalradius (AU)
Orbital period(years)
Mean orbitalspeed (km/s)
Inclination to ecliptic (°) Eccentricity
Equatorial Diameter
(km)
Ceres Asteroid belt 2.77 4.60 17.882 10.59 0.080 974.63.2
Pluto Kuiper belt 39.48 248.09 4.666 17.14 0.249 230610
Haumea Kuiper belt 43.34 285.4 4.484 28.19 0.189 1150 +250 -100
Makemake Kuiper belt 45.79 309.9 4.419 28.96 0.159 1500 +400 -200
Eris Scattered disc 67.67 557 3.436 44.19 0.442 2340
Asteroid Classifications
• Spectral categories• C-group: carbonaceous, ~75%, albedo < 0.1• S-type: siliceous composition (stony), ~17% • M-group: metallic, but diverse interpretations• Other, less common types exist• Generally, people think of C-group, S-group, and
M-group corresponding to meteorites of carbonaceous, siliceous, and metallic composition.
Near Earth Objects (asteroids)• More easily accessible
by spacecraft.• Impact the inner planets• Perihelion < 1.3 AU – but
could have high e• There are about 7000
documented NEOs, almost all asteroids (NEAs).
• The largest is ~32 km in diameter (1036 Ganymed).
NEA examples
433 Eros, 34 x 11 x 11 kmSecond largest NEO
Why go to an asteroid?
• Can’t you just study meteorites?
Just One Reason: Space Weathering• Vapor is produced by impacts of solar wind and
micrometeorites.• Iron particles condense out of the vapor, with
nanometer length scales• This reddens and darkens the surface• Fresh materials appear bright, and old
materials are darker and have weaker spectral bands.
• This makes it difficult to determine what an asteroid (or the Moon) is really made of.
Other reasons
• What do they look like?– How did they form?
NEAR mission
• Gamma ray spectrometer• Measure spectral
properties• Study regolith processes• One goal was to link the
asteroid (S-type) to meteorites on the ground– Didn’t really work out, but
still learned a lot.
Launched in 1996, arrived in 2000
NEAR at Eros
Shape model
Geology highlights: regolith exists, ponding and albedo changes
Itokawa• Goal: return a sample, study a much smaller
size asteroid.
Itokawa
Highlights: regolith sorting, color contrasts. Sample returned! (?)
Rosetta Mission• ESA Rosetta Spacecraft
– Land on a comet in 2014
Lutetia July 2010• Rosetta flyby at
3000 km.• 120 km length• Mass and
density?
Doppler shift
Deep Space Station 63
70 meter antenna in Madrid, Spain
Lutetia July 2010• Density of 3.4 g/cm3.
– Greater than stony meteorites.– Partially differentiated?
Dawn – Main belt mission
• Energetically difficult, uses ion propulsion.• Targets two very different bodies:
– 1 Ceres (largest asteroid) – carbonaceous– 4 Vesta (third largest asteroid) – basaltic (melted,
differentiated)
Ceres
Hubble image
Mysterious bright spot.
An intact, surviving protoplanet!1/3rd the asteroid belt’s mass.Density: 2.1 g/ccmEquatorial radius: 487 kmAlbedo: 0.09Carbonaceous (C-type)Hydrated minerals.Possibly partially differentiated.
??????
Vesta
Hubble image
Much less spherical.
Mean radius: 265 kmAlbedo: 0.43Density: 3.42 grams/ccm !Unique V-type (Vestoid)Much drier than Ceres.Differentiated, likely formed a core, basaltic eruptions. Magma ocean?Why so hot? Why so different?What does its shape tell you?Only asteroid definitively linked to meteorites (HED meteorites).
Dawn at Vesta
Asteroid spin rates
Meteorites
“Meteorite belts”
• Antarctica• Deserts in NW Africa
– Fall vs. find
Meteorite classifications
Chondrules• Small spherules. Rapidly heated
and cooled grains found in chondrite meteorites. Made of mostly olivine and pyroxene.– Can make up a large (>50%)
fraction of meteorite mass.– Some of the earliest solid
material in the SS.• Formation mechanism not
understood– Shock processes in the nebular
gas?– Droplets from impacts?
Millimeter scale bar
Meteorite Classifications• Chondrites (ordinary)
– 80% of all meteorites. Not melted, but more processed than CCs. Represent terrestrial planet materials.
• Carbonaceous chondrites– 5% of meteorites. Carbon and water rich. Not significantly
heated. Close to solar nebular composition.• Achondrites: no chondrules, igneous processes and
heating.– 8% of all meteorites.– Mostly HED’s– Lunar and martian meteorites
• Irons: rich in iron, large crystal sizes in the metal means long cooling times deep in a planetesimal core.
HED meteorites & Vesta
Why does Vesta yield such nice spectra?
Vesta + fresh eurcrite
Why does Vesta yield such nice spectra?
Vesta + fresh eurcrite
Magnetic shielding of solar wind?
Key concepts
• Asteroid belt, Kirkwood gaps• Lagrangian points• Near earth objects• Space weathering• Some geologic observations of asteroids• Vesta vs. Ceres• Chondrules and chondrite meteorites• HED meteorites and Vesta