Title: Chapter 7 Our Planetary System
1Chapter 7Our Planetary System
Earth, as viewed by the Voyager spacecraft
27.1 Studying the Solar System
- Our goals for learning
- What does the solar system look like?
- What can we learn by comparing the planets to one
another? - What are the major features of the Sun and
planets?
3What does the solar system look like?
1. What is in it?
4- Eight major planets with nearly circular orbits
- Pluto (dwarf planet) is smaller than the major
planets and has a more elliptical orbit
5What Counts as a Planet?
- 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.
6History of Planet Count
- The number of objects counted as planets in the
solar system has varied over the centuries - As low as 6 and has high as 13
7What does the solar system look like?
2. How far apart . are things? Planets are
very tiny compared to distances between them.
8What can we learn by comparing the planets to one
another?
9Comparative Planetology
- We can learn more about a world like our Earth by
studying in context with other worlds in the
solar system. - Stay focused on processes common to multiple
worlds instead of individual facts specific to a
particular world.
10- Comparing the planets reveals patterns among them
- Those patterns provide insights that help us
understand our own planet
11What are the major features of the Sun and
planets?
Sun and planets to scale
12(No Transcript)
13Density and Composition
Density mass _ volume
g/cm3
- Measure a planets volume
- Measure a planets spin gt calculate mass
- Result is a worlds bulk density.
14Density and Composition
- Common materials
- Iron 7.9 g/cm3
- Basalt 3.3 g/cm3
- (rock)
- Carbon and hydrogen ices 0.4-1.5 g/cm3
- (volatiles)
- H and He ltlt0.01 g/cm3
15Density and Composition
- Earth 5.5 g/cm3 composition- iron, rock
- Saturn 0.7 g/cm3 composition- some rock,
volatiles and lots HHe - Callisto 1.9 g/cm3 Titan 2 g/cm3 composition
-rock and ice
16Thought Question
- Planet Mars has a bulk density of 3.9 g/cm3 What
materials is it made of ? - Iron 7.9 g/cm3
- Basalt 3.3 g/cm3
- Volatiles 1-1.5 g/cm3
- H and He ltlt0.01 g/cm3
17Thought Question
- Planet Mars has a bulk density of 3.9 g/cm3 What
materials is it made of ? - Iron 7.9 g/cm3
- Basalt 3.3 g/cm3
- Volatiles 1-1.5 g/cm3
- H and He ltlt0.01 g/cm3
18What have we learned?
- What does the solar system look like?
- Planets orbit Sun in the same direction and in
nearly the same plane. - What can we learn by comparing the planets to one
another? - Comparative planetology looks for patterns among
the planets. - Those patterns give us insight into the general
processes that govern planets - Studying other worlds in this way tells us about
our own Earth
19What have we learned?
- How can we tell what planets are made of?
- The bulk density of the planets reflect the type
of materials the planets are composed of. - There are 4 main common types of material
- Most planets are made of a mixture of these
materials that are not necessarily represented on
the surface.
20What features of the solar system provide clues
to how it formed?
21- All large bodies in the solar system orbit in the
same direction and in nearly the same plane
22Motion of Large Bodies
- Most also rotate in the direction of orbit.
23Sun
- Over 99.9 of solar systems mass
- Made mostly of H/He gas (plasma)
- Converts 4 million tons of mass into energy each
second
24Two Main Planet Types
- Terrestrial planets (rocky worlds)
- Jovian planets
- (gas giant worlds)
25The 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.
26There 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
center.
27gas giant worlds are far from the Sun
Rocky worlds are close to the Sun.
28Jupiter largest gas giant world
gas giant worlds are much larger than rocky
worlds
Earth largest rocky world
29Rocky worlds have no rings and no, or few, moons.
Gas Giant worlds have rings and many moons.
30Swarms of Smaller Bodies
- Many rocky asteroids and icy comets populate the
solar system
31Notable Exceptions
- Several exceptions to the normal patterns need to
be explained
32What have we learned?
- What features of the solar system provide clues
to how it formed? - Motions of large bodies All in same direction
and plane - Two main planet types Terrestrial and jovian
- Swarms of small bodies Asteroids and comets
- Notable exceptions Rotation of Uranus, Earths
large moon, etc.