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Structure of the Solar System

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Planets move around the Sun in elliptical orbits, with Sun as ... Similar in size and colour to Phoebe *(Sat Moon) Orbit 8.5 - 19 au. Fits definition of comet ... – PowerPoint PPT presentation

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Title: Structure of the Solar System


1
Structure of the Solar System
  • Where and why it is what it is

2
Laws of motion
  • Planets move around Sun
  • Not always a given,
  • Anthropic Earth-centered Ptolomaic cosmology
  • Copernicus published his seminal work on his
    deathbed (1543)
  • A case of publish and perish
  • De revolutionibus orbium celestium
  • Conservation of angular momentum
  • v1r1 v2r2 constant (for constant mass)
  • The two body problem

3
Keplers Laws
  • Planets move around the Sun in elliptical orbits,
    with Sun as one of the foci
  • A radius vector sweeps out equal area in equal
    time
  • Squares of the periods of the revolutionof the
    planets are proportional to the cubes of their
    distance from the Sun

4
Titius-Bode Law
  • Distances of planets from Sun
  • 0.4, 0.7, 1.0, 1.6, 2.8, 5.2,
  • Can be formulated
  • R 0.4 0.3k
  • K 0, 1, 2, 4, 8, 16, 32
  • 0.4, 0.7, 1.0, 1.6, 2.8, 5.2,
  • Titius 1729-1776, Bode 1747-1826

5
Titius-Bode Law
  • Planet missing between Mars and Jupiter
  • At 2.8 au
  • Ceres discovered in 1801 at 2.77 au
  • Pallas, Juno, Vesta by 1804
  • Exploded planet
  • No common origin point
  • Failed planet

6
Titius-Bode Law
  • Okay for Uranus, not so good for Neptune (38
    predicted vs 30 actual au)
  • No other correlation with planetary properties
  • Secondary effect after formation
  • Related to stable resonances of orbital periods
  • Planets have moved

7
Asteroids
Vesta, Ceres, Moon
  • Total mass less than 5 of Moon
  • 1-2 Million asteroids with size gt 1km
  • Asteroid belt
  • Gaps/concentrations due to resonances with
    Jupiter (Kirkwood Gaps)
  • Gaps at 21 (3.28 au) and 31 (2.50 au)
  • Concs at 11 32 (3.97 au) 43 (4.2 au)

8
Orbital resonances
  • Fractional orbital periods have greater orbital
    stability to perturbation
  • Constructive or destructive interference
  • Gaps or concentrations

9
Asteroids
  • Resonances and gaps

10
Asteroids
  • Trojan Asteroids
  • Lagrange points
  • Gravitation centripetal
  • L4 and L5 60
  • Equal gravity to Jup Sol

L1, L2, L3 unstable L4,L5 stable
11
Asteroids
  • Several hundred thousand discovered
  • 26 gt 200 km
  • Solid rock bodies
  • Rubble piles
  • Visits by NEAR, Hayabusa
  • NEAR landed on Eros
  • Hayabusa landed on Itokawa
  • Plus flybys of other missions on way to Jupiter

12
Asteroid Spectral Classes
  • Definition
  • Based on light reflectance (Albedo)
  • Spectral features
  • Spectral shape
  • Mineralogical features
  • e.g. olivine, pyroxene, water,
  • Chapman 1975
  • 3 types (C-carbonaceous, S-stony, and U)
  • Tholen 1984
  • used spectra 0.31-1.06 µm
  • Types A-X (23)

13
Spectral Class
Mathilde
  • C-type (Most abundant 75 )
  • Low albedo (0.03-0.10)
  • Strong UV absorption below 0.4 µm
  • Longer wavelengths featureless
  • Reddish
  • Water feature at 3 µm
  • Type 10-Hygeia
  • 4th largest asteroid

14
Spectral Class
Ida Dactyl
  • S Class (17)
  • Moderately bright
  • Albedo 0.10-0.22
  • Metallic Fe-Ni magnesium silicate
  • Spectrum has steep slope lt 0.7µm
  • Absorption features around 1 and 2 µm
  • Largest is 15 Eunomia (330 km diam)

15
Spectral Class
  • M class (3rd abundant)
  • Metallic Fe-Ni
  • Moderately bright (0.10-0.18)
  • Spectrum is flat to reddish
  • Absorption features at 0.55 and 0.75 µm
  • 16 Psyche (330 km)

16 Psyche
16
Asteroids
  • Compositional trends?
  • Igneous inside 2.8 au (S class)
  • Metamorphic around 3.2 au (M class)
  • Primitive outside 3.4 au (C class)

17
Origin of asteroid belt
  • Failed planet
  • Meteorites
  • Iron meteorites from core
  • Pallasites show mantle olivine
  • Igneous achondrites
  • Crustal carbonaceous chondrites
  • But not from single body
  • Oxygen isotopes, chemistry

18
Origin of asteroid belt
  • Planetoids form in early SS
  • Coalesce to form planets
  • Presence of Jupiter
  • Pumped up the eccentricities
  • Limits growth
  • Many small bodies
  • No planet at 2.8 au

19
Near-Earth asteroids
  • Apollos, Atens and Armors
  • Few thousand gt 1km
  • 107 10-100m
  • 1036 Ganymed, 433 Eros
  • Source of meteorites?
  • Eros could survive 50-100 Myr
  • 5 chance of hitting Earth

20
Spectrophotometric Paradox
  • Most common meteorites are chondrites
  • Parent body apparently absent
  • 3628 Boznemcová
  • 8km body with Ord-chondrite spectrum
  • Of 35 NEA, 6 have Ord-chondrite spectra
  • Plus 10 of Main Belt asteroids of size 1km
  • Chondrites dominate meteorites,
  • But not asteroids

21
Asteroids to Meteorites
  • Relative frequency of meteorites depends on
    efficiency of delivery
  • Meteorites unlikely to be sourced from deep
    within asteroid belt
  • Asteroids must be close to resonances to supply
    meteorites into Earth-crossing orbit
  • 6 Hebe near 31(2.50 au)
  • Source of H-Chondrites IIE Irons

22
Missing Olivine Meteorites
  • Iron Meteorites
  • Cores
  • Pallasites
  • Core-mantle
  • Achondrites, Chondrites
  • Crust
  • Wheres the mantle olivine?

23
Individual asteroids
  • 1 Ceres
  • Largest 933 km diameter
  • 2.7 g/cm3
  • 2.77 au
  • C class
  • 9/13 largest asteroids similar

24
Individual asteroids
  • 4 Vesta
  • Irregular shape (460 km across)
  • 3.7 g/cm3
  • Intact differentiated crust (basalt)
  • Source of HED meteorites (4.560 Gyr)
  • 460 km crater, 13 km deep
  • Two more large craters (100 km)

25
Individual asteroids
  • 433 Eros
  • S class
  • 2nd largest NEA
  • 33x13x13 km
  • Density 2.5 0.8 km
  • Coherent rather than rubble pile

26
Individual asteroids
  • NEAR Lands on Eros - 2001
  • Boulders on surface from 250 m

5 m
27
Individual asteroids
  • 25143 Itokawa (1998)
  • S class
  • 500 m long
  • 2.0 g/cm3
  • Rubble pile

Hayabusa (Muses-C)
28
Individual asteroids
  • Visits to Mathilde, Gaspra, Ida
  • Ida has satellite (Dactyl)

NEAR Mission
29
Interplanetary dust
  • Sources
  • Asteroids (5 km/s)
  • Comets (20-60 km/s)
  • Interstellar grains?
  • 10,000 tons/year to Earth
  • Fluffy grains can survive atmospheric entry
  • Many carbonaceous

30
Moving Giant Planets
  • Jupiter moved sunwards depleting asteroid belt
    beyond 4 au
  • Saturn, Uranus, Neptune move out
  • Saturn now in 21 resonance with Jupiter
  • Produced by bombardment of centaurs

31
Centaurs
  • Between Saturn and Uranus
  • 2060 Chiron - 1977
  • 182 km
  • Dark-grey-black object (albedo 0.1)
  • Similar in size and colour to Phoebe (Sat Moon)
  • Orbit 8.5 - 19 au
  • Fits definition of comet
  • 5145 Pholus - 1992
  • 185 km, red
  • Nessus, Asbolus, Chariklo

32
Moving Giant Planets
  • Neptune plows into and depletes inner zone of
    Kuiper Belt (30-35 au)
  • Pluto swept into a 32 orbital resonance at high
    eccentricity and inclination

33
Moving Giant Planets
  • can throw KBO out to the Oort Cloud
  • Only few retained from Jupiter
  • Rest lost
  • 5-10 from Saturn
  • 10-40 from Uranus
  • 40 from Neptune
  • Can throw out Rocky and Icy bodies
  • Oort cloud primitive?
  • Throws objects in
  • The late heavy bombardment for inner SS

34
Solar System
  • Dynamic
  • Many time scales
  • 4 Vesta has survived 4.56 Gyr
  • But Exposure ages of HED meteorites 5-80 Myr
  • Survival time of some asteroids
  • 50,000 years

35
Near Earth Asteroid Orbits
  • http//neo.jpl.nasa.gov/orbits/
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