From Heritage of Astronomy to Space Technological Heritage: A Perspective
Astronomy: Perspective
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Transcript of Astronomy: Perspective
Astronomy: Perspective
Bob Rood
U. Virginia
The Milky Way might look like this.
It contains billyuns & billyuns of stars
25,000 lySun
Green Bank Scale Model
On GB scale model Ceti is at geosynchronous orbit
Center of Milky Way close to Mercury’s orbit
The age of the oldest stars in the Milky Way is about 13Gyr
1Gyr = 1 billion years
The age of the oldest meteorites, and by inference the Solar System, is 4.57 Gyr, i.e., << Age of MW
SN1054
Supernovae & other stars make heavy elements.
Molecules
Volatile
Hydrogen H2
Water H2O
Carbon monoxide CO
Carbon dioxide CO2
Methane CH4
Ammonia NH3
Refractory
Silicon dioxide SiO2
Number of atoms per 10,000,000 of
hydrogen
hydrogen 10,000,000 sulfur 95
helium 1,400,000 iron 80
oxygen 6,800 argon 42
carbon 3,000 aluminum 19
neon 2,800 sodium 17
nitrogen 910 calcium 17
magnesium 290 all other elements 50
silicon 250
“Heavy or metals”
• We are made out of common stuff• The ratios of the various elements
are pretty much the same throughout the MW
• H2O should be ubiquitous
Age (Gyr)
Meta
llici
ty
Metallicity built up rapidly and has remained almost constant
Emission nebula
Reflection Nebula
Dust lanes
Embedded newly formed stars
Star formation continues in Giant Molecular Clouds
The Ophiuchi molecular cloud: one of the closest of the “dark clouds.”
This is it
And smaller cold dark clouds
The rate of star formation was much higher early in the Galaxy
If the best targets are solar type stars close (< 3000 ly) to the Sun and 5 Gyr old then
R = 1 star/1000 yr
disk
Protostars are typically surrounded by a dusty disk
The dust collects into km size planetestimals.
These collide and build up planets or planet cores.
A surviving rocky planetesimal: the asteroid Gaspara
An evaporating icy planetesimal: Comet West
Gas being entrained in the Solar windDust being blown away
by Solar radiation pressure
Closeup of an evaporating icy planetesimal:The nucleus of Comet Halley in 1986
Nucleus covered with a layer of black crud
Gas boils out of cracks
Classical Planet Formation
Terrestrial planets form in inner Solar System from rocky planetesimals
In outer SS icy planetesimals accrete to form a core of perhaps 10M which has sufficient gravity to suck on H and He to make Jovian planets.
Stellar Mass-Luminosity Relation
Luminosity increases rapidly as mass increases
Stellar lifetime decreases rapidly as stellar mass increases
Stars with M > 1.2M don’t live long enough for complex life to develop.
Of the 30 brightest stars, all except 2 are more luminous than the Sun. Almost half are more luminous than 1000 L .
In an unbiased sample of all stars closer than 10 pc, the vast majority are less luminous than the Sun. The typical star is a dinky little thing with L < L /100.
The consequence is that the familiar bright stars are not good SETI targets.
SETI scientists are aware of this. The general public and most science fiction writers are not.
In the 4.6 Gyr since the Sun formed its luminosity has increased by 25%. This has important consequences for the Earth.
Ice ages: -7C 8% change in L
CO2 Greenhouse: 3C 4% change in L
Major climate change with if L changesby a few %
Faint young Sun problem
Early Greenhouse must have been substantially enhanced
Greenhouse must evolved as L increases keeping T just right. (The Goldilocks Problem)
Potential crisis when the atmosphere becomes oxidizing.
Evolution of the early terrestrial Greenhouse
• mid 1970’s: ammonia
• late 1970’s: methane + ammonia
• late 1980’s: lots and lots of CO2
• 2000’s: methane protected by photochemical haze
• 2010’s: ?
What is an Earthlike planet?
Liquid H2O on the surface for Gyrs
There’s certainly more to it than M<few M and roughly the right distance from the star. E.g.,
• Too massive initial outgassing of CO2 leads to runaway greenhouse
• Too small vulcanism stops and atmosphere almost vanishes like Mars
Cosmic Catastrophes
ImpactsOn the 108 year timescale there is an impact large enough to lead to a major extinction event.KT event:Bad for dinosaursGood for mammals
Nearby Supernova
E.g., Fields & Ellis, (1999, New Astronomy, 4, 419) suggest that deep-ocean 60Fe is a fossil of a near-earth (30 pc) supernova and might be associated with a mini-extinction event.
Galactic -ray burst
A -ray burst at a distance of 10kpc and pointed at the Earth would produce a radiation dose of 6500 rads (65 grays) inside the ISS. 65 x fatal.
Very bad for a civilization that had moved to space colonies.
Galactic -ray burst (cont)
Worse than biggest solar flares because:
1.No warning
2.No shielding by magnetic fields
3.Requires more mass shielding than protons from flares
Galactic -ray burst (cont)
Worse than biggest solar flares because:
1.No warning
2.No shielding by magnetic fields
3.Requires more mass shielding than protons from flares
Galactic -ray burst (cont)
Frequency perhaps one per 107 yr even correcting for the fact that bursts are more common in lower metallicity galaxies
“Gotchas:” we’re playing Calvinball
There is no fJ in the Drake Equation
Fragments of Comet Shoemaker-Levy 1993
Last big accretion event in the Solar System.
An ETI Gotcha
Jupiter eats comets
Without Jupiter there would be a major extinction event every 100,000 years. (Wetherill, 1994, Ap & Sp Sci, 212, 23)
Classical picture: Whether you get a Jupiter or not is a contest between building the core of icy plantesimals and the star’s blowing away the H & He.
If the star wins: no Jupiter
On the other hand if a Jupiter is formed too quickly while there is still a lot material in the disk, it spirals inward to become a hot Jupiter and eats any Earth-like planets on the way.
Time to wakeup for
Coffee