Our local neighbourhood - The Solar System
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Transcript of Our local neighbourhood - The Solar System
Our local neighbourhood - The Solar System
Dr Nicola LoaringSALT/SAAO
Concept: The Scale of our Solar
SystemIf the Sun were a grapefruit (10cm)Earth, grain of sand 1mm, 15 m away Jupiter, marble 1.5cm, 80 m awayPluto, tiny grain of sand 0.2mm, 700 m away
And the NEXT CLOSEST sun (or star) would be in ... Nairobi !
DEMO
Concept: Two types of Planet
Terrestrial planets:Rocky with molten cores
Jovian planets: Mainly gas and liquid with rocky cores
The rocky worlds are the 4 inner planets plus our Moon
They have a solid rock surface with an iron core and a weak or no atmosphere.
Rocky Planets
There are 4 gas giant planets in our solar system.
These planets have NO solid surfaces – just gas and clouds that get denser as you move to their centre.
Gas Giants
Rocky worlds
are close to the Sun
Gas giant worlds are far from the Sun
Relative distribution of the two types of Planets
Wikipedia
Jupiter – largest gas giant world
Earth – largest rocky world
Gas giant worldsare much larger than rocky worlds
Relative sizes
NASA/JPL
Activity opportunity: Powers of 10
Body RadiusSurface
AreaVolume
Earth 1 1 1
Jupiter 10x [101]100x [102]
1000x [103]
Sun 100x 10,000x1,000,00
0x
Rocky worlds have no rings and no, or few, moons.Gas Giant worlds have
rings and many moons.
(From left to right: Enceladus and shadow, Dione and shadow. Titan and Mimas are off the limb to the right).
Relative numbers of rings and moons
www.hubblesite.org
Why are there two types of planet?
Solar System Formation
All orbits are in the same direction and in the same plane.
Suggests a common origin.
Solar system formed when a cloud of gas and dust in space was disturbed. Gas and dust drawn together, forming a solar nebula.
The cloud began to spin as it collapsed and therefore flattened.
As the disk got thinner particles formed clumps, planetisimals eventually forming planets or moons.
As the cloud continued to fall in, the centre eventually got so hot that it became a star, the Sun. Solar wind then blew away excess material.
Why are there 2 types of planet?
Inside the frost line: Too hot for hydrogen compounds to form ices.Outside the frost line: Cold enough for ices to form.
Inner parts of disk are hotter than outer parts. Only materials that solidify at high temperatures can condense to form solid particles. Rock can be solid at much higher temperatures than ice.
Density and Composition
Earth 5.5 g/cm3 composition- iron, rock
Saturn 0.7 g/cm3 composition- some rock, volatiles and lots H & He
Callisto 1.9 g/cm3, Titan 2 g/cm3 composition -rock and ice
DEMO
Asteroids and Comets
Leftovers from the accretion process
Rocky asteroids inside frost line
Icy comets outside frost line
The inner rocky Planets- MercuryHas the largest temperature
extreme in the solar system from -183C to 430C.
Second densest planet after the Earth, so must have a large iron core.
Has a very thin atmosphere consisting of atoms blasted off its surface from the solar wind. Atmosphere is constantly being replenished. Heavily cratered surface because its atmosphere is so thin. DEMO
Mission Launch Year
Mariner 10 1973
Messenger 2004 (to orbit 2011)
BepiColombo 2013 (to arrive 2019)
The inner rocky Planets -Venus
Venus is a similar size to the Earth.It atmosphere is mainly Carbon dioxide and Nitrogen.Its very hot there due to the ‘Green house effect’ a whopping 462C.
Recent Missions Launch Year
Galileo 1989 (flyby 1990)
Magellan1989 (in orbit 1990-
1994)
Cassini1997 (flyby 1998,
1999)
Venus Express 2005 (arrive 2006)
Messenger2004 (flyby 2006,
2007)
Planet C 2010
Our home the Earth
Earth is at a distance of 150 million kilometres from the Sun. Sunlight takes 8 minutes to reach us.
Our atmosphere is composed of 78 percent nitrogen, 21 percent oxygen and 1 percent other constituents.
71% of the Earth’s surface is covered by water!
Earth is the only planet in the solar system known to harbour life.
Picture taken by Apollo 17 astronauts
The Moon
Heavily cratered.
Evidence for water.
Mission Launch Year
Apollo manned missions 1968 - 1972
Lunar Prospector 1998
SMART-1 2003
SELENE (JAXA) 2007
Chandrayaan-1 2008
LRO 2009
LCROSS 2009
The inner rocky Planets - Mars
Mars is 1/10th the mass of Earth
Average temp is –63C
Rock are made of silicates (like sand) and also a dash of iron oxides to give it that reddish colour (Mars is rusty!)
Surface is dry now, but scientists believe there were once rivers, lake and maybe oceans of water
Water exists in “permafrost” a few metres below the surface (Mars Express / Mars Odyssey). Maybe even liquid water down there! (MGS).
No landers have detected water in soil, but have found evidence of past water.
Mars
Mars has the highest (extinct) volcano in the Solar System: Olympus Mons at 24 km high 2.7 times Everest!
Recent Missions Launch Year
Viking 1 1975 (landed 1976)
Viking 2 1975 (landed 1976)
Mars Global Surveyor 1996 (arrived 1997)
Mars Pathfinder 1996 (arrived 1997)
Mars Express 2003 (still active)
Spirit / Opportunity 2003 (still active)
Phoenix 2007 (till 2008)
ExoMars 2016?
Mars Sample Return Mission 2020?
The gas giants -JupiterLargest planet in the solar system – its diameter is 11x the Earth’s diameter.
Jupiter takes about 12 years to orbit the sun and rotates in about 10 hours.
Jupiter is a ball of dense hydrogen, helium, water, nitrogen and other gases over a rocky core. ~90% H, ~10% He.
Above core is the main bulk of the planet which is liquid metallic hydrogen. (Huge pressure). Ionized protons and electrons in liquid form.
Powerful winds, jet streams, lightning and huge hurricane-like storms like the Great Red Spot.
This storm has been raging for over 300 years and is twice the size of Earth!
Mission Launch
Pioneer 11 1974 (arrived 1979)
Voyager 1 1977 (arrived 1980)
Voyager 2 1977 (arrived 1981)
Galileo1989 (arrived 1990, still
operational)
This image shows, from left to right, the outer portion of the C ring and inner portion of the B ring. The B ring begins a little more than halfway across the image. The general pattern is from "dirty" particles indicated by red to cleaner ice particles shown in turquoise in the outer parts of the rings.
Cassini and Saturn
95 times the Earth’s mass.
Saturn, famous for its rings. These are made up of trillions of icy particles.
1015 tons of material in the rings, enough for a small moon!
No more than 50 million years old (MUCH younger than the planet) - continually replenished
Mission Launch Date
Pioneer 11 1973 (flyby 1979)
Voyager 1 1977 (encounter 1980)
Voyager 2 1977 (encounter 1981)
Cassini-Huygens1997 (orbiting 2004, Titan descent 2005 - orbiter still
operational)
Titan's surface in2004-2005!
Titan
Liquid ethane/methane on surfaceLots of hydrocarbons
Uranus Primarily composed of rock and ices with only 15% H (much less than Jupiter and Saturn).
No rocky core like Jupiter and Saturn, but material is more evenly distributed.
No liquid metallic hydrogen envelope.
Atmosphere of 83% H, 15% He, 2% methane.
Mission Launch Date
Voyager 21977 (encounter 1985-
1986)
NeptuneComposed of ices and rock with about 15% H and a little He
Atmosphere mainly H and He with a little methane which gives it its blue colour as methane absorbs red light
Small solid core, the size of the Earth
No distinct layers like Uranus (unlike Saturn and Jupiter)
Neptune has the fastest winds in the solar system reaching 2000 km/hr
Mission Launch Date
Voyager 2 1977 (flyby 1989)
The IAU definition of a planet (2006): is in orbit around the Sun, has sufficient mass so that it is nearly round has "cleared the neighborhood" around its orbit.
What Counts as a Planet?
Mission Launch
New Horizons 2006 (to arrive 2015)
The IAU currently recognises five dwarf planets—Ceres, Pluto, Haumea, Makemake, and Eris.
Ceres is in the asteroid belt others in the Kuiper belt.
Many Kuiper Belt objects, exist in what is believed to be a vast shell of icy and rocky objects that live at the very edge of our solar system.
Dwarf Planets