physical properties of planetsphysical properties of planets … · 2016. 8. 6. · physical...

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Physical Properties of Planets Physical Properties of Planets Physical Properties of Planets Physical Properties of Planets Two distinct types of planets: Two distinct types of planets: Two distinct types of planets: Two distinct types of planets: Terrestrial Planets (Earth-like) Jovian Planets (Jupiter-like) Size: Size: Size: Size: Mass: Mass: Mass: Mass: Physical Property of Planets Physical Property of Planets Physical Property of Planets Physical Property of Planets Density: - measure of how compressed a substance is - determined by total mass & volume it occupies ρ = Mass Volume Examples: Water 1.0 g/cm 3 Air 0.0013 g/cm 3 Rocks 2.5-3.5 g/cm 3 Styrofoam 0.1 g/cm 3 Lead 12 g/cm 3 Ice 0.92 g/cm 3 Gold 19 g/cm 3 - indicates the composition composition composition composition of object! Density: Density: Density: Density: Terrestrial Planets: Terrestrial Planets: Terrestrial Planets: Terrestrial Planets: - large density ("rocky" composition) Jovian Planets: Jovian Planets: Jovian Planets: Jovian Planets: - small density ("Gas Giants") -mostly liquefied gas P rot rot rot rot : No. of Moons: No. of Moons: No. of Moons: No. of Moons: Mercury 0 Jupiter 67+rings Venus 0 Saturn 62+rings Earth 1 Uranus 27+rings Mars 2 Neptune 14+rings Pluto 5 Terrestrial Terrestrial Terrestrial Terrestrial Planets: Planets: Planets: Planets: - small size - small mass - large density - "rocky" composition - long rotational periods - hard surfaces with possible atmosphere -no atmosphere Mercury -very, very thick atm. Venus - few, if any moons All 4 Inner Planets All 4 Inner Planets All 4 Inner Planets All 4 Inner Planets (and (and (and (and some large moons) some large moons) some large moons) some large moons)

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  • Physical Properties of PlanetsPhysical Properties of PlanetsPhysical Properties of PlanetsPhysical Properties of Planets

    Two distinct types of planets:Two distinct types of planets:Two distinct types of planets:Two distinct types of planets: Terrestrial Planets (Earth-like) Jovian Planets (Jupiter-like)

    Size:Size:Size:Size:

    Mass:Mass:Mass:Mass:

    Physical Property of PlanetsPhysical Property of PlanetsPhysical Property of PlanetsPhysical Property of Planets

    Density: - measure of how compressed a substance is - determined by total mass & volume it occupies

    ρ = Mass Volume

    Examples: Water 1.0 g/cm3 Air 0.0013 g/cm3 Rocks 2.5-3.5 g/cm3 Styrofoam 0.1 g/cm3 Lead 12 g/cm3 Ice 0.92 g/cm3 Gold 19 g/cm3

    - indicates the compositioncompositioncompositioncomposition of object! Density:Density:Density:Density:

    Terrestrial Planets:Terrestrial Planets:Terrestrial Planets:Terrestrial Planets: - large density ("rocky" composition)

    Jovian Planets:Jovian Planets:Jovian Planets:Jovian Planets: - small density ("Gas Giants")

    -mostly liquefied gas

    PPPProtrotrotrot::::

    No. of Moons:No. of Moons:No. of Moons:No. of Moons:

    Mercury 0 Jupiter 67+rings Venus 0 Saturn 62+rings Earth 1 Uranus 27+rings Mars 2 Neptune 14+rings

    Pluto 5

    Terrestrial Terrestrial Terrestrial Terrestrial Planets:Planets:Planets:Planets:

    - small size - small mass - large density - "rocky" composition - long rotational periods - hard surfaces with possible atmosphere

    -no atmosphere � Mercury

    -very, very thick atm. � Venus - few, if any moons

    ���� All 4 Inner PlanetsAll 4 Inner PlanetsAll 4 Inner PlanetsAll 4 Inner Planets (and(and(and(and some large moons)some large moons)some large moons)some large moons)

  • Mercury Global ImageMercury Global ImageMercury Global ImageMercury Global Image

    Mercury surface close-up

    Mercury "Spider Crater"

    Mercury and Moon comparison

    Venus visual image

    Venus Radar Map

    Surface of Venus (Venera spacecraft)

    Maat Mons volcano from Magellan data

  • Mars Global Image

    Opportunity rover at Endeavour Crater

    Ice on Mars (Phoenix Lander)

    Ice on Mars (Phoenix Lander)

    Subsurface Water on Mars?

    Eroded pebbles in sediment = fast flowing water.

    Curiosity rover at Gale Crater

    Ancient Mars ??

  • Jovian Planets:Jovian Planets:Jovian Planets:Jovian Planets:

    -large size -large mass -small density "Gas Giants" -mostly liquefied gas -short rotational periods -ring systems and many moons

    ���� All 4 Large Outer PlanetsAll 4 Large Outer PlanetsAll 4 Large Outer PlanetsAll 4 Large Outer Planets

    http://solarsystem.nasa.gov/planets/profile.cfm?Object=Jupiter&Display=http://solarsystem.nasa.gov/planets/profile.cfm?Object=Jupiter&Display=http://solarsystem.nasa.gov/planets/profile.cfm?Object=Jupiter&Display=http://solarsystem.nasa.gov/planets/profile.cfm?Object=Jupiter&Display=GalleryGalleryGalleryGallery

    Jupiter's Rings discovered by Voyager 1

    Voyager 1 image of Saturn

  • Scattered light seen from behind Saturn (Cassini)

    Titan and Epimetheus behind Saturn's rings

    (Cassini)

    Saturn in infrared

    Recent Storm (2010 - now) on Saturn

    Enceladus (300 mi across) in front of Saturn

    North Pole of Saturn with “Hexagon”

  • Neptune's rings (Voyager 2)

    Neptune and Triton (Voyager 2)

    Plutonian (Pluto-like) Objects ---- Small mass, sizeSmall mass, sizeSmall mass, sizeSmall mass, size ---- Small density (mostly ice)Small density (mostly ice)Small density (mostly ice)Small density (mostly ice) ---- Very Elliptical orbitsVery Elliptical orbitsVery Elliptical orbitsVery Elliptical orbits with hwith hwith hwith high inclinationsigh inclinationsigh inclinationsigh inclinations ---- Beyond orbit of NeptuneBeyond orbit of NeptuneBeyond orbit of NeptuneBeyond orbit of Neptune (Kuiper Belt(Kuiper Belt(Kuiper Belt(Kuiper Belt, Oort Cloud, Oort Cloud, Oort Cloud, Oort Cloud))))

  • PlutoPlutoPlutoPlutoniannianniannian / Dwarf Planets/ Dwarf Planets/ Dwarf Planets/ Dwarf Planets

    NameNameNameName aaaa diameterdiameterdiameterdiameter Eris (2003) * 68 AU 1450145014501450 mimimimi Pluto (1930)Pluto (1930)Pluto (1930)Pluto (1930) 39 AU39 AU39 AU39 AU 1430 mi1430 mi1430 mi1430 mi Makemake (2005) 46 AU 1200 mi 2007 OR10 67 AU ~800 mi Haumea (2004) 43 AU ~780 mi Quaoar (2002) 43 AU ~700 mi Sedna (2004) 530 AU ~650 mi Orcus (2004) 39 AU ~610 mi 2002 MS4 41 AU ~600 mi Salacia 42 AU ~575 mi

    * * * * http://www.gps.caltech.edu/~mbrown/planetlila/index.html http://www.gps.caltech.edu/~mbrown/dwarfplanets/http://www.gps.caltech.edu/~mbrown/dwarfplanets/http://www.gps.caltech.edu/~mbrown/dwarfplanets/http://www.gps.caltech.edu/~mbrown/dwarfplanets/

    Likely Likely Likely Likely Candidates Candidates Candidates Candidates

    NameNameNameName aaaa DiameterDiameterDiameterDiameter Varuna (2000) 43 AU ~475 mi 2013 FY27 59 AU ~475 mi 2003 AZ84 40 AU ~465 mi Varda 46 AU ~430 mi Ixion (2001) 40 AU ~420 mi Chaos 46 AU ~380 mi

    Formation of the Solar SystemFormation of the Solar SystemFormation of the Solar SystemFormation of the Solar System

    Sun, planets and all of solar system -formed from gravitational collapse of large cloud of gas & dust - mostly Hydrogen, Helium

    Properties of Gravitational CollapseProperties of Gravitational CollapseProperties of Gravitational CollapseProperties of Gravitational Collapse

    Heating of gas & dust -gravitational energy released -increases temperature of cloud - hotter at center - cooler at edges

    Rotation -during collapse, rate of rotation increases -all parts of the cloud rotate in the same direction -causes cloud to flatten into a disk

  • During Collapse of cloud: -Three temperature regions

    Inner Region:Inner Region:Inner Region:Inner Region: -temperature rises above 2000oC -all matter is vaporized -no solid matter, only free atoms

    � forms SUNSUNSUNSUN

    Midrange Region:Midrange Region:Midrange Region:Midrange Region: -temperature: 0oC to 2000oC -heavier elements can form solids -no light gases or ice (frozen gas)

    � forms Terrestrial PlanetsTerrestrial PlanetsTerrestrial PlanetsTerrestrial Planets

    Outer Region:Outer Region:Outer Region:Outer Region: -temperature less than 0oC -heavier elements can form solids -light gases and ice are present

    � forms Jovian PlanetsJovian PlanetsJovian PlanetsJovian Planets

    http://www.pas.rochester.edu/~joel/papers.html

    http://www.pas.rochester.edu/~joel/papers.html