Bit of Administration . Bit of Administration . Reading - - PowerPoint PPT Presentation
Bit of Administration . Bit of Administration . Reading - - PowerPoint PPT Presentation
Bit of Administration . Bit of Administration . Reading Reading BSNV Chaps. 9 and 15 BSNV Chaps. 9 and 15 No Mathieu office hours today (Monday)! No Mathieu office hours today (Monday)! Additional
Bit of Administration …. Bit of Administration ….
- Reading
Reading – – BSNV Chaps. 9 and 15 BSNV Chaps. 9 and 15
- No Mathieu office hours today (Monday)!
No Mathieu office hours today (Monday)!
- Additional observations for Lab 2, through April 5
Additional observations for Lab 2, through April 5
– – Due April 7 in lecture or April 9 at Mathieu office Due April 7 in lecture or April 9 at Mathieu office
- 12
12-
- week exam in two weeks
week exam in two weeks -
- April 12, 7:15 pm
April 12, 7:15 pm
– – Review session, Sunday, April 11, 6:30 pm Review session, Sunday, April 11, 6:30 pm
The Solar System The Solar System
- A Sense of Scale
A Sense of Scale
Around Earth Distance to Moon = 0.1= Around Europe Distance to North America
The Solar System The Solar System
- A Sense of Scale
A Sense of Scale
The Solar System The Solar System
- A Sense of Scale
A Sense of Scale
The Solar System The Solar System
- Inventory
Inventory
- Sun
Sun 99.85% by mass 99.85% by mass
- Planets 0.1 % by mass
Planets 0.1 % by mass
- Satellites and Rings
Satellites and Rings
- Asteroids
Asteroids
- Comets
Comets
- Meteroids
Meteroids
- Dust
Dust
- Solar Wind (ionized gas)
Solar Wind (ionized gas)
The Solar System The Solar System
- Inventory
Inventory -
- “
“Sedna Sedna” ”
The Solar System The Solar System
- General Characteristics of
General Characteristics of Major Major Planets Planets -
- Dynamical
Dynamical
- Nearly circular orbits (Mercury and Mars most eccentric)
Nearly circular orbits (Mercury and Mars most eccentric)
The Solar System The Solar System
- General Characteristics of Major Planets
General Characteristics of Major Planets -
- Dynamical
Dynamical
- Nearly circular orbits (Mercury and Mars most eccentric)
Nearly circular orbits (Mercury and Mars most eccentric)
- All orbit within 10
All orbit within 10o
- of Earth’s orbital plane
- f Earth’s orbital plane
The Solar System The Solar System
- General Characteristics of Major Planets
General Characteristics of Major Planets -
- Dynamical
Dynamical
- Nearly circular orbits (Mercury and Mars most eccentric)
Nearly circular orbits (Mercury and Mars most eccentric)
- All orbit within 10
All orbit within 10o
- of Earth’s orbital plane
- f Earth’s orbital plane
- All revolve in the same direction
All revolve in the same direction
- All rotate in the same direction (except Venus)
All rotate in the same direction (except Venus)
The Solar System The Solar System
- General Characteristics of Major Planets
General Characteristics of Major Planets -
- Radius
Radius
The Solar System The Solar System
- General Characteristics of Major Planets
General Characteristics of Major Planets -
- Age
Age
- Earth
Earth -
- Oldest rocks 3.9 billion yr (4.5 billion yr inferred)
Oldest rocks 3.9 billion yr (4.5 billion yr inferred)
- Moon
Moon -
- 4.5 billion yr
4.5 billion yr
- Meteorites
Meteorites -
- 4.6 billion yr
4.6 billion yr
- Sun
Sun -
- 4.6 billion (theoretical)
4.6 billion (theoretical)
- Universe
Universe -
- 12 billion yr
12 billion yr
The Solar System The Solar System
- General Characteristics of Major Planets
General Characteristics of Major Planets -
- Physical Properties
Physical Properties
Terrestrial Terrestrial Location Inner Location Inner Size Small (10 Size Small (104
4 km)
km) Mass 0.1 Mass 0.1 -
- 1.0
1.0 M MEarth
Earth
Density 5 gm cm Density 5 gm cm-
- 3
3
Appearance Rock with craters, Appearance Rock with craters, volcanos volcanos Composition Heavy elements Composition Heavy elements 7 Giant Satellites 7 Giant Satellites Outer Outer Small (4000 km) Small (4000 km) 0.01 0.01 M MEarth
Earth
2 2-
- 3 gm cm
3 gm cm-
- 3
3
Rock, ice with craters, Rock, ice with craters, volcanos volcanos Heavy elements, ices Heavy elements, ices Jovian Jovian Outer Outer Large (10 Large (105
5 km)
km) 15 15 -
- 300
300 M MEarth
Earth
1 gm cm 1 gm cm-
- 3
3
Gaseous, with Gaseous, with rock cores rock cores Hydrogen, helium Hydrogen, helium
Mercury Venus Earth Mars Jupiter Saturn Uranus Nepture
Notes: Notes: 1) 1) Densities: Rock = 3 gm cm Densities: Rock = 3 gm cm-
- 3
3, Water = 1 gm cm
, Water = 1 gm cm-
- 3
3
2) 2) Composition of Sun and Universe by numbers of atoms: Composition of Sun and Universe by numbers of atoms: 94% H, 6% He, 2% all else 94% H, 6% He, 2% all else
Io Europa Ganymede Callisto
The Formation of the Solar System The Formation of the Solar System
The Formation of the Solar System The Formation of the Solar System
- Interstellar Clouds
Interstellar Clouds
By By Mass Mass
- 73% Molecular Hydrogen
73% Molecular Hydrogen
- 25%Atomic Helium
25%Atomic Helium
- 2% Dust (Metals)
2% Dust (Metals)
ConcepTest ConcepTest! !
The Taurus clouds are thought to be rather cold, with The Taurus clouds are thought to be rather cold, with temperatures of perhaps 30 K. If you wanted to test this temperatures of perhaps 30 K. If you wanted to test this hypothesis by looking for light hypothesis by looking for light emitted emitted by the Taurus clouds, in by the Taurus clouds, in what wavelength would you want to observe? what wavelength would you want to observe? A) X A) X-
- ray
ray B) Ultraviolet B) Ultraviolet C) Optical C) Optical D) Infrared D) Infrared E) Radio E) Radio
The Formation of the Solar System The Formation of the Solar System
- Dense Molecular Cores
Dense Molecular Cores (“ (“Bok Bok Globules”) Globules”)
- ≈ 1 M
≈ 1 Mo
- ≈ 50,000 AU
≈ 50,000 AU
- ≈ 10
≈ 10 o
- K
K
The Formation of the Solar System The Formation of the Solar System
The Formation of the Solar System The Formation of the Solar System
- Protoplanetary
Protoplanetary Disks Disks
- ≈ 0.01 M
≈ 0.01 Mo
- ≈ 100 AU
≈ 100 AU
- ≈ 3000
≈ 3000 -
- > 10
> 10 o
- K
K
The Formation of the Solar System The Formation of the Solar System
The Formation of the Solar System The Formation of the Solar System
- Condensation Sequence
Condensation Sequence
- Condensation Temperature
Condensation Temperature Temperature at which Solid Gas Temperature at which Solid Gas
T > 50 T > 50 o
- K
K T > 200 T > 200 o
- K
K T > 1000 T > 1000 o
- K
K Hydrogen (H) Hydrogen (H) Helium (He) Helium (He) H H2
20, Methane (CH
0, Methane (CH4
4)
) CO CO2
2, Ammonia (NH
, Ammonia (NH3
3)
) Iron (Fe), Silicon ( Iron (Fe), Silicon (Si Si) ) Metal Compounds Metal Compounds Gas Gas Gas Ice Gas Gas Rock Rock Gas
The Formation of the Solar System The Formation of the Solar System
- Condensation Sequence
Condensation Sequence
1000 K 200 K
Rock Grains Rock, Ice Grains No Grains
M M J E V
The Formation of the Solar System The Formation of the Solar System
The Formation of the Solar System The Formation of the Solar System
- Grain
Grain Collisions Collisions ==> ==> Planetesimals Planetesimals (100 km) (100 km) random random 100 km 100 km
The Formation of the Solar System The Formation of the Solar System
- Planetesimal
Planetesimal Accretion Accretion ==> ==> Rocky Planets and Rocky Planets and Jovian Jovian Cores Cores gravity gravity
The Formation of the Solar System The Formation of the Solar System
- Gas
Gas Accumulation Accumulation ==> ==> H and He onto H and He onto Jovian Jovian Cores Cores gravity gravity Protomoons Protomoons
ConcepTest ConcepTest! !
Most comets have orbits that take them well beyond Jupiter. You Most comets have orbits that take them well beyond Jupiter. You would expect their composition to be: would expect their composition to be: A) Rocks and heavy elements only A) Rocks and heavy elements only B) Rocks and ices only B) Rocks and ices only C) Rocks, ices, and hydrogen and helium C) Rocks, ices, and hydrogen and helium
The Formation of the Solar System The Formation of the Solar System
The Formation of the Solar System The Formation of the Solar System
- Dispersal of Hydrogen and Helium Gas
Dispersal of Hydrogen and Helium Gas
- Solar Wind?
Solar Wind?
- Jets?