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Copyright © 2010 Pearson Education, Inc. Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

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Page 1: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.Copyright © 2010 Pearson Education, Inc.

Chapter 4The Solar

System

Page 2: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

EXAM 1

• Average 71• Median 72

Page 3: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Tough Questions

• Copernicus’ Heliocentric theory explains that…

• Venus retrogrades when she overtakes us at an inferior conjunction

• The sun lies at one focus of an ellipse• Mars will retrograde when it reaches a certain

position on its epicycle• All planets lie between the Sun and Earth

Page 4: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

If a new wave arrives on shore every two seconds, then its frequency is 2 Hz.

• False• It would be ½ Hz or 1 per 2 seconds• 2 Hz would be 2 per second

Page 5: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Doubling the temperature of a black body will double the total energy it radiates.

• False

F = s T4

If you were to double T then F would be 16x bigger.

Page 6: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

What is the light gathering power of an 8 inch telescope compared to a 4 inch telescope?

• 4x better

Light gathering depends on the area.

Area = pr2

4 is twice as big as 8 so area is 4 times

Page 7: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

The opacity of the atmosphere is partially corrected via adaptive optics.

• False

Adaptive optics can correct for atmospheric turbulence but not opacity such as clouds or smog.

Page 8: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Example Questions

• Of those examples I gave in class that appeared on the exam 68% got them correct.

Page 9: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Chapter 4The Solar System

Page 10: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Units of Chapter 4

An Inventory of the Solar System

Interplanetary Matter

The Formation of the Solar System

Planets Beyond the Solar System

Page 11: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Early astronomers knew Moon, stars, Mercury, Venus, Mars, Jupiter, Saturn, comets, and meteors.

Now known: Solar system has 166 moons, one star, eight planets (added Uranus and Neptune), asteroids, comets, meteoroids, dwarf planets, and Kuiper Belt objects.

An Inventory of the Solar System

Page 12: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

An Inventory of the Solar System

Page 13: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

• Distance from Sun known by Kepler’s laws.

• Orbital period can be observed.

• Radius known from angular size.

• Masses known from Newton’s laws.

• Rotation period known from observations.

• Density can be calculated knowing radius and mass.

An Inventory of the Solar System

Page 14: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

All orbits but Mercury’s are close to the same plane.

An Inventory of the Solar System

Page 15: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

An Inventory of the Solar System

Page 16: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 1

Which of the following are terrestrial planets?

a) only Earth

b) Earth, Moon, and Venus

c) Mercury, Venus, Earth, and Mars

d) Mercury, Venus, Earth, Moon, Mars, and Pluto

e) Mercury, Venus, Earth, Moon, Mars, and Ceres

Page 17: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 1

Which of the following are terrestrial planets?

a) only Earth

b) Earth, Moon, and Venus

c) Mercury, Venus, Earth, and Mars

d) Mercury, Venus, Earth, Moon, Mars, and Pluto

e) Mercury, Venus, Earth, Moon, Mars, and Ceres

Terrestrial planets are “Earth-like.”

Page 18: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Terrestrial planets:

Mercury, Venus, Earth, Mars

Jovian planets:

Jupiter, Saturn, Uranus, Neptune

An Inventory of the Solar System

Page 19: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Mass and Density

• Mass: how much “stuff” something has.• Density: how much “stuff” something has

in a certain size (volume)

Page 20: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 2

The major difference(s) between the terrestrial and jovian planets involve(s)

a) mass.

b) density.

c) rotation speed.

d) density and rotation speed.

e) mass and density.

Page 21: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 2

The major difference(s) between the terrestrial and jovian planets involve(s)

a) mass.

b) density.

c) rotation speed.

d) density and rotation speed.

e) mass and density.

Jovian planets are more massive, but less dense, than

terrestrial planets.

Page 22: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Differences between the terrestrial planets:

• Atmospheres and surface conditions are very dissimilar.

• Only Earth has oxygen in atmosphere and liquid water on surface. **Goldilocks**

• Earth and Mars rotate at about the same rate; Venus and Mercury are much slower, and Venus rotates in the opposite direction.

• Earth and Mars have moons; Mercury and Venus don’t.

• Earth and Mercury have magnetic fields; Venus and Mars don’t.

An Inventory of the Solar System

Page 23: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 3

Which of the following defines density?

a) mass times surface gravity

b) mass divided by volume

c) size divided by weight

d) mass times surface area

e) weight divided by size

Page 24: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 3

Which of the following defines density?

a) mass times surface gravity

b) mass divided by volume

c) size divided by weight

d) mass times surface area

e) weight divided by size

Density can be thought of as

MATTER

SPACE gm/cm3

Lots of matter in a small space = HIGH density.

Little matter in a large space = LOW density.

Page 25: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 4

Compared with terrestrial planets, jovian planets share all of the following characteristics EXCEPT

a) low density.

b) large size.

c) many moons.

d) ring systems.

e) slower rotation.

Page 26: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 4

Jovian planets share all of the following characteristics EXCEPT

a) low density.

b) large size.

c) many moons.

d) ring systems.

e) Slow rotation.

Page 27: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

The inner solar system, showing the asteroid belt, Earth-crossing asteroids, and Trojan asteroids

Page 28: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

a) beyond the orbit of Neptune.

b) between Earth and the Sun.

c) between Mars and Jupiter.

d) in the orbit of Jupiter, but 60 degrees ahead or behind it.

e) orbiting the jovian planets in captured, retrograde orbits.

Most asteroids are found

Question 5

Page 29: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

a) beyond the orbit of Neptune.

b) between Earth and the Sun.

c) between Mars and Jupiter.

d) in the orbit of Jupiter, but 60 degrees ahead or behind it.

e) orbiting the jovian planets in captured, retrograde orbits.

Question 5

Most asteroids are found

The Asteroid Belt is located between 2.1 and 3.3 A U

from the Sun.

Page 30: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 6

The asteroid belt is evidence of

a) a planet that once orbited the Sun but later was destroyed.

b) ancient material from the formation of the solar system.

c) a collision between Jupiter and one of its larger moons.

d) comets that were trapped by Jupiter’s gravitational field.

Page 31: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 6

The asteroid belt is evidence of

a) a planet that once orbited the Sun but later was destroyed.

b) ancient material from the formation of the solar system.

c) a collision between Jupiter and one of its larger moons.

d) comets that were trapped by Jupiter’s gravitational field.

Asteroids, meteoroids, and comets may have not changed at all since

the solar system formed.

Page 32: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

Large picture: The path of Icarus, an Earth-crossing asteroid

Inset: Ceres, the largest asteroid

Page 33: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Asteroids and meteoroids have rocky composition; asteroids are bigger.

(above) Asteroid Ida with its moon, Dactyl

(below) Asteroid Gaspra

(above) Asteroid Mathilde

Interplanetary Matter

Page 34: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

VESTA - July 2011: 10% of main asteroid belt mass~530 km in dia.

Page 35: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 7

Compared to asteroids, comets show all of these properties EXCEPT

a) their densities are higher.

b) their orbits tend to be more elliptical.

c) they tend to be made of ice.

d) they can look fuzzy, whereas asteroids appear as moving points of

light.

e) their average distances from the Sun are far greater.

Page 36: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 7

Compared to asteroids, comets show all of these properties EXCEPT

Comets have densities much lower than asteroids

or planets.

a) their densities are higher.

b) their orbits tend to be more elliptical.

c) they tend to be made of ice.

d) they can look fuzzy, whereas asteroids appear as moving points of

light.

e) their average distances from the Sun are far greater.

Page 37: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

What Killed the Dinosaurs?

The larger an impact is, the less often we expect it to occur.

The dinosaurs may have been killed by the impact of a large meteor or small asteroid.

Page 38: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

Deep Impact Tempel 1

Asteroid Eros

Page 39: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Comets are icy, with some rocky parts.

The basic components of a comet

Interplanetary Matter

Page 40: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

The solar wind means the ion tail always points away from the Sun.

The dust tail also tends to point away from the Sun, but the dust particles are more massive and lag somewhat, forming a curved tail.

Page 41: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

The internal structure of the cometary nucleus

Page 42: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

The size, shape, and orientation of cometary orbits depend on their location. Oort cloud comets rarely enter the inner solar system.

Page 43: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

What causes a meteor shower?

Question 8a) A comet and an asteroid collide.

b) Earth runs into a stray swarm of asteroids.

c) Earth runs into the debris of an old comet littering its orbit.

d) Meteorites are ejected from the Moon.

e) Debris from a supernova enters Earth’s atmosphere

Page 44: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

What causes a meteor shower?

Question 8

Meteor showers can generate a few shooting stars, to hundreds of thousands, seen in an hour.

a) A comet and an asteroid collide.

b) Earth runs into a stray swarm of asteroids.

c) Earth runs into the debris of an old comet littering its orbit.

d) Meteorites are ejected from the Moon.

e) Debris from a supernova enters Earth’s atmosphere

Page 45: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

Meteor showers are associated with comets – they are the debris left over when a comet breaks up.

Page 46: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System
Page 47: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

Page 48: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

The impact of a large meteor can create a significant crater.

The Barringer meteor crater in Arizona

Page 49: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Interplanetary Matter

The Manicouagan reservoir in Quebec

Page 50: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 9

Any theory of the origin of the solar system must explain all of these EXCEPT

a) the orbits of the planets are nearly circular, and in the same plane.

b) the direction that planets orbit the Sun is opposite to the Sun’s spin.

c) the terrestrial planets have higher density and lower mass.

d) comets do not necessarily orbit in the plane of the solar system.

Page 51: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 9

Any theory of the origin of the solar system must explain all of these EXCEPT

a) the orbits of the planets are nearly circular, and in the same plane.

b) the direction that planets orbit the Sun is opposite to the Sun’s spin.

c) the terrestrial planets have higher density and lower mass.

d) comets do not necessarily orbit in the plane of the solar system.

The planets do orbit in the same direction that the Sun spins.

Most also spin in that direction, and most also have large moons that orbit in that direction.

Page 52: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Condensation theory:

• Interstellar dust grains help cool cloud, and act as condensation nuclei.

The Formation of the Solar System

Page 53: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Nebular contraction:

• Cloud of gas and dust contracts due to gravity; conservation of angular momentum means it spins faster and faster as it contracts.

Formation of the Solar System

Page 54: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Conservation of angular momentum says that product of radius and rotation rate must be constant.

Therefore, as a dust cloud collapses, its rate of rotation will increase.

The Concept of Angular Momentum

Page 55: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Temperature in cloud determines where various materials condense out; this determines where rocky planets and gas giants form.

The Formation of the Solar System

Page 56: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 10

The condensation sequence theory explains why

a) our planet Earth has water and rain.

b) stars are more likely to form large planets orbiting very near.

c) terrestrial planets are different from jovian planets.

d) the Moon formed near the Earth.

e) Pluto has such a circular orbit.

Page 57: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 10

The condensation sequence theory explains why

a) our planet Earth has water and rain.

b) stars are more likely to form large planets orbiting very near.

c) terrestrial planets are different from jovian planets.

d) the Moon formed near to Earth.

e) Pluto has such a circular orbit.

The condensation sequence theory explains how the temperature of the early solar nebula controls which materials

are solid, and which are gaseous.

Page 58: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

The Formation of the Solar System

The star Beta Pictoris is surrounded by a disk of warm matter, which may indicate planetary formation.

Page 59: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

The Formation of the Solar System

These images show possible planetary systems in the process of formation.

Page 60: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Planets Beyond the Solar System

Many planets have been discovered in other solar systems; this is one that is visible.

Page 61: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 11

Astronomers have detected most extrasolar planets by observing

a) the “wobble” of their parent stars using spectroscopy.

b) starlight reflected by their surfaces.

c) eclipses when the planets block the light of their parent stars.

d) the planets’ changing phases as they orbit their stars.

Page 62: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 13

Astronomers have detected most extrasolar planets by observing

a) the “wobble” of their parent stars using spectroscopy.

b) starlight reflected by their surfaces.

c) eclipses when the planets block the light of their parent stars.

d) the planets’ changing phases as they orbit their stars.

Measurements of the periodic Doppler shift in the spectra of the

star 51 Pegasi indicate it has a planetary companion.

Page 63: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Planets Beyond the Solar System

Some planets are discovered through the “wobble” they create in their parent star’s orbit.

Page 64: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Others are discovered through the periodic dimming of the parent star’s luminosity.

Planets Beyond the Solar System

Page 65: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Copyright © 2010 Pearson Education, Inc.

Planets Beyond the Solar System

These are the orbits of many extra-solar planets discovered so far. Most have masses closer to that of Jupiter than that of Earth.

Page 66: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 12

Extrasolar planets the size of Earth have NOT been seen yet with current techniques because

a) small planets probably don’t exist.

b) the large planets nearby have swept them up.

c) Earth-like planets take time to form.

d) large planets orbiting near to their stars are more easily detected.

e) small planets can only be seen if they cross in front of their star.

Page 67: Copyright © 2010 Pearson Education, Inc. Chapter 4 The Solar System

Question 12

Extrasolar planets the size of Earth have NOT been seen yet with current techniques because

a) small planets probably don’t exist.

b) the large planets nearby have swept them up.

c) Earth-like planets take time to form.

d) large planets orbiting near to their stars are more easily detected.

e) small planets can only be seen if they cross in front of their star.

Looking for detectable “wobbles” in the spectra of stars finds massive

planets with small orbits.

Other techniques may be needed to see less massive Earth-like planets.