Energy & Planetary Science: Overview of Power, Energy Types & Formation, Study notes of Astronomy

An introduction to the concepts of power, units of energy, types of energy, and planetary formation. Topics covered include the conversion of matter to energy, the different states of matter, and the detection of extrasolar planets. The document also discusses the physics of collapsing clouds and the formation of planets in the solar system.

Typology: Study notes

2019/2020

Uploaded on 11/25/2020

koofers-user-hg4-1
koofers-user-hg4-1 🇺🇸

10 documents

1 / 4

Toggle sidebar

This page cannot be seen from the preview

Don't miss anything!

bg1
1
ASTR1030, Accelerated Solar System
Astronomy
Midterm 2 Study Sheet
I. PHYSICS
1. Energy and Power
Energy is defined as the ability to do work.
Power is the rate of energy use, e. g. the amount of energy
used in a period of time.
2. Units
1 calorie is the amount of energy it takes to raise one gram
of water by 1oC.
1 joule (~1/4 of a calorie) is the standard MKS unit
favored by science.
1 Watt is a joule/s.
3. Types of Energy:
Kinetic Energy is the energy from motion.
Potential Energy is stored energy that can be converted
(gravitational, chemical, electrical).
Radiative Energy is energy carried by light.
Thermal Energy is a type kinetic energy called heat.
4. Heat Versus Temperature:
Temperature is the measure of the average kinetic energy
of a particle within a object.
Thermal Energy, or heat, is the total kinetic energy in an
object.
5. Mass is Energy:
Matter contains a tremendous amount of energy.
This matter to energy conversion can explain the energy
output of the sun and other stars.
Converting matter to energy on Earth in a controlled fash-
ion, however, is very difficult.
6. Basic Physics: States of Matter
Solid: At low enough temperature (below 0 oC for water),
individual molecules have very little kinetic energy. They
can thus bond tightly to their neighbors to form a solid.
Liquid: As the kinetic energy of the molecules increases
(they move faster), they can break the bonds to the nearest
neighbor, yet still remain tightly packed (incompressible).
Gas: At even higher temperatures (above 100 oC for
water), the molecules no longer stay together (evapora-
tion). All bonding between molecules is gone.
Plasma: At extremely high temperatures (greater than
~5000 oC), the molecules dissociate and ionize. The mate-
rial is now freely moving electrons and ions.
II. KEPLER’S LAWS
(See Midterm 1 Study Sheet)
III. NEWTON’S LAWS: MOTION & GRAVITY
(See Midterm 1 Study Sheet)
IV. NEWTON’S FORM OF KEPLER’S 3RD LAW
(See Midterm 1 Study Sheet)
V. LIGHT
1. Light is a wave and particle.
Wave:
Po we r En er gy
Ti me
-------------------=
E mc2
=
fλ× c=
Photons:
2. Types of light:
Radio Waves are the same as light - the lowest frequency
(longest wavelength) part of the spectrum. We (humans)
cannot sense radio waves.
Infrared Radiation has frequencies less than that of visible
light (longer wavelengths). We cannot see infrared radia-
tion, but we can feel intense infrared radiation as heat.
Visible Light is a small portion of the spectrum from 700
nm (red) to 400 nm (violet). Remember, 1 nm = 1x10-9 m.
We (humans) see light.
Ultraviolet Radiation has frequencies greater than that of
visible light (shorter wavelengths). We cannot sense ultra-
violet radiation, but after exposure, we can feel it’s effects
(sunburn).
X rays have frequencies greater than that of ultraviolet
(shorter wavelengths). We cannot sense X rays. Many
materials are transparent to X rays (i. e., they look like
glass or water to someone with X-ray vision), so X rays
are very useful to “look” inside or through an object.
Gamma Rays have frequencies greater than that of X rays.
Individual gamma ray photons have a lot of energy and
can damage a cell if they strike it - making them danger-
ous to humans.
3. Interaction with Matter. There are 4 basic ways
in which light can interact with matter:
Emission: Every substance has a distinct emission pattern
or finger print.
Important Point: We can tell what a star is made of by ana-
lyzing the emission spectrum.
Absorption: Every substance has a distinct absorption pat-
tern or finger print. Important Point: We can tell what a
gas is made of by analyzing the absorption spectrum.
Transmission
Reflection
4. Wien’s law
The peak in the spectrum is proportional to the tempera-
ture.
Important Point: One can determine a star’s surface temper-
ature by measuring the wavelength of the peak emission.
5. Stefan-Boltzmann Law
The total amount of energy is proportional to the tempera-
ture to the forth power times the size of the object.
The surface area of a star is:
Ehc
λ
------ h 6.626 10 34
×J s= =
λpe ak
2.9 106
×
T
----------------------- Kn m
o
( )=
P
A
--- σT4σ5.7 10 8
×W
m2K4
--------------
= =
A4πR2
=
pf3
pf4

Partial preview of the text

Download Energy & Planetary Science: Overview of Power, Energy Types & Formation and more Study notes Astronomy in PDF only on Docsity!

ASTR1030, Accelerated Solar System

Astronomy

Midterm 2 Study Sheet

I. PHYSICS

1. Energy and Power

  • Energy is defined as the ability to do work.
  • Power is the rate of energy use, e. g. the amount of energy used in a period of time.

2. Units

  • 1 calorie is the amount of energy it takes to raise one gram of water by 1oC.
  • 1 joule (~1/4 of a calorie) is the standard MKS unit favored by science.
  • 1 Watt is a joule/s.

3. Types of Energy:

  • Kinetic Energy is the energy from motion.
  • Potential Energy is stored energy that can be converted (gravitational, chemical, electrical).
  • Radiative Energy is energy carried by light.
  • Thermal Energy is a type kinetic energy called heat.

4. Heat Versus Temperature:

  • Temperature is the measure of the average kinetic energy of a particle within a object.
  • Thermal Energy, or heat, is the total kinetic energy in an object.

5. Mass is Energy:

  • Matter contains a tremendous amount of energy.
  • This matter to energy conversion can explain the energy output of the sun and other stars.
  • Converting matter to energy on Earth in a controlled fash- ion, however, is very difficult.

6. Basic Physics: States of Matter

  • Solid : At low enough temperature (below 0 oC for water), individual molecules have very little kinetic energy. They can thus bond tightly to their neighbors to form a solid.
  • Liquid : As the kinetic energy of the molecules increases (they move faster), they can break the bonds to the nearest neighbor, yet still remain tightly packed (incompressible).
  • Gas : At even higher temperatures (above 100 oC for water), the molecules no longer stay together (evapora- tion). All bonding between molecules is gone.
  • Plasma : At extremely high temperatures (greater than ~5000 oC), the molecules dissociate and ionize. The mate- rial is now freely moving electrons and ions.

II. KEPLER’S LAWS

(See Midterm 1 Study Sheet)

III. NEWTON’S LAWS: MOTION & GRAVITY

(See Midterm 1 Study Sheet)

IV. NEWTON’S FORM OF KEPLER’S 3RD LAW

(See Midterm 1 Study Sheet)

V. LIGHT

1. Light is a wave and particle.

  • Wave :

Power Energy Time

= -------------------

E mc 2 =

f × λ = c

  • Photons :

2. Types of light:

  • Radio Waves are the same as light - the lowest frequency (longest wavelength) part of the spectrum. We (humans) cannot sense radio waves.
  • Infrared Radiation has frequencies less than that of visible light (longer wavelengths). We cannot see infrared radia- tion, but we can feel intense infrared radiation as heat.
  • Visible Light is a small portion of the spectrum from 700 nm (red) to 400 nm (violet). Remember, 1 nm = 1x10-9^ m. We (humans) see light.
  • Ultraviolet Radiation has frequencies greater than that of visible light (shorter wavelengths). We cannot sense ultra- violet radiation, but after exposure, we can feel it’s effects (sunburn).
  • X rays have frequencies greater than that of ultraviolet (shorter wavelengths). We cannot sense X rays. Many materials are transparent to X rays (i. e., they look like glass or water to someone with X-ray vision), so X rays are very useful to “look” inside or through an object.
  • Gamma Rays have frequencies greater than that of X rays. Individual gamma ray photons have a lot of energy and can damage a cell if they strike it - making them danger- ous to humans.

3. Interaction with Matter. There are 4 basic ways

in which light can interact with matter:

  • Emission : Every substance has a distinct emission pattern or finger print. Important Point : We can tell what a star is made of by ana- lyzing the emission spectrum.
  • Absorption : Every substance has a distinct absorption pat- tern or finger print. Important Point: We can tell what a gas is made of by analyzing the absorption spectrum. _- Transmission
  • Reflection_

4. Wien’s law

  • The peak in the spectrum is proportional to the tempera- ture.

Important Point : One can determine a star’s surface temper- ature by measuring the wavelength of the peak emission.

5. Stefan-Boltzmann Law

  • The total amount of energy is proportional to the tempera- ture to the forth power times the size of the object.
  • The surface area of a star is:

E hc λ

------ h 6.626 10

  • 34 = = × Js

λ (^) peak 2.9 10

6 × T

----------------------- Knm

o = ( )

P A

--- σ T 4 σ 5.7 10

  • 8 × W m 2 K

= = ------------- 4 -

A 4 π R 2 =

6. Doppler Shift.

Important Point : We can tell if a star is moving toward or away by analyzing the light spectrum.

  • Objects speed (positive toward us) (
  • The change in wavelength is:

7. Detecting Extrasolar Planets

  • Most extrasolar planets are found by detecting small motions (Doppler shifts) that they induce on the host star.
  • Another way of detecting extrasolar planets is by detect- ing small drops in brightness due to a planetary transit.

VI. TELESCOPES

1. Types of Telescopes

  • Refracting
  • Reflecting

2. Angular Resolution

  • Small angel formula:
  • Arcmin, arcsec: arcmin = 1/60o; arcsec = 1/60 arcmin = 1/ 3600 o
  • Diffraction Limit:

v c ∆λ λ o

= -------

∆λ =λ shifted – λ rest

Refracting Telescope

Camera or Eye

Reflecting Telescope

α s 2 π d α =^ ----------^ ×^360 ° s

d

α 2.5 10 5 × λ dt


  = ^ ^ arcsec

3. Light Gathering

  • Area of pupil: ~10-5^ m^2
  • A 6” telescope has a light-gathering area of:

4. Uses

  • Imaging
  • Spectroscopy
  • Timing

5. Radio Telescopes

  • Radio telescopes can have a long baseline (as large as the Earth) and, in spite of the long wavelengths, achieve excellent angular resolution.

6. Difficulties

  • Light Pollution
  • Atmospheric turbulence.
  • The atmosphere is opaque to IR, UV, X-Ray, and Gamma Rays!

7. Space Telescopes

  • Space telescopes can “see” in IR, UV, X-Ray, and γ-Ray.
  • Space Telescopes do not suffer from atmospheric turbu- lence.

VII. SOLAR SYSTEM FORMATION: THE 4

CHALLENGES.

1. 1. Patterns of Motion

  • All planets orbit in the same direction - counter clockwise.
  • All planets lie in the same plane.
  • Almost all planets have nearly circular orbits.
  • Almost all planets rotate counter clockwise.
  • Almost all moons orbit their planet counterclockwise.
  • The sun rotates counterclockwise.

2. Types of planets.

3. Asteroids and Comets

4. Exceptions

  • Not all planets have the same rotation: Venus, Uranus, an Pluto.
  • Mercury and Pluto inclined orbits.
  • Earth has a large moon.
  • Some moons of the Giant planets orbit clockwise.

5. 5. Two more challenges:

  • Hubble’s pictures of planetary nebulae.
  • Recent findings of extra-solar planets.

Terrestrial Planets Giant Planets Smaller. Larger. Rocky (high density). Gaseous (low density) Solid Surface. No solid surface Close to the sun. Far from the sun. Warmer Cooler Few or no moons or rings. Rings and many moons.

Asteroids Comets Mostly lie between Jupiter and Mars.

Mostly in the Oort cloud, as far away as 50,000 AU. Trojan asteroids are in Jupiter’s orbit.

Others lie in Kuiper belt near Pluto. Rocky (high density). Icy (moderate density)

A π r 2 π [ 3 in × 2.54 cmin × 1 m ⁄ 100 cm ] 2 10

  • 2 m 2 = = =

IX. RADIOACTIVE DATING

  • Certain elements are unstable and decay.
  • The decay process is characterized by a half-life , making it an ideal clock.
  • By comparing the remaining amount of the unstable ele- ment with the decay product , one can determine the age of a rock.

X. CHAOS

1. Definition

  • In a chaotic system, a small change in initial conditions can lead to very large changes in the final state.
  • In a non-chaotic system, the more accurately one knows the initial conditions, the more accurately one can predict the final state.

2. Predictability

  • Chaotic systems are inherently unpredictable in detail, but one can observe patterns.
  • Example: weather. One can not accurately predict in thirty days if it will rain. But, one can predict that it will be colder in January than in July. In other words, there are patterns in the weather even though the details are difficult to predict.

3. Chaos and Nebular Theory

  • Virtually every phase of the solar system formation is cha- otic. A small change in the initial rotation can dramati- cally change the collapse. A small change in the initial formation of planetesimals can lead to a completely dif- ferent set of planets.
  • Under the nebular theory, one can predict patterns (for example, giant planets versus terrestrial planets, all plan- ets orbiting in the same direction, etc.) but one cannot pre- dict a detailed final result.

XI. PLANETARY GEOLOGY

1. Basic Processes of Formation

  • Accretion: Collisions between planetesimals and a planet result with the planet increasing in size.
  • Differentiation: The heavy materials, metals, sink to the center forming the core.

2. Interiors of the Terrestrial Planets

2.1 By composition:

  • Core: Mostly metals.
  • Mantle: Rock
  • Crust: The scum that floats to the top.

2.2 By rigidity:

  • Lithosphere: The rigid outer section; the crust and part of the mantle.

3. Basic Processes of Heating of the Interior

  • Accretion: The kinetic energy of the impacts turn into

thermal energy.

  • Differentiation: As the heavy metals sink, the friction releases heat.
  • Radioactivity: Nuclear energy released from the “nuclear ash” of a burned out star (part of the solar nebula).

4. Cooling of the Interior

4.1 Basic Processes:

  • Convection: Hot material flows carrying thermal energy with it.
  • Conduction: Heat flows within a material. The material does not move.
  • Eruption: In my mind, a form of convection.
  • Radiation: Conduction and convection move heat to the surface. Ultimately, the energy escapes the planet by radi- ation, mostly in the infrared. Important Point : Conduction, convection, and eruption bring heat from the interior to the surface. The heat must ultimately leave the surface via radiation - mostly in the infrared. 4.2 Smaller planets cool faster.
  • The most important effect: surface area to volume ratio. (Remember potatoes and peas!)
  • Large planets tend to have larger cores and therefore more radioactive heating.
  • The initial accretion and differentiation energy was greater for the larger planets since the gravity was stron- ger and they accreted more mass.
  • Larger planets tend to have atmospheres which, with greenhouse gasses, can slow the radiative cooling.

5. Magnetic Fields

Terrestrial Planets Need:

  • A metal core.
  • Internal convection (rotation). Important point : A terrestrial planet without a metal core (Mars has a small core) or a planet that has cooled off (e.g. the Moon) is not expected to have a strong magnetic field

6. Shaping the Surface of Terrestrial Planets

6.1 Impact cratering

  • A typical crater is about 10 times wider than the impactor that created it.
  • Cratering can tell us how old a surface is. 6.2 Volcanism
  • Lava Plains: Low viscosity (runny).
  • Shield Volcanoes Medium viscosity.
  • Strotovolcanoes: High viscosity (goo). 6.3 Tectonics
  • Plates move due to internal convection and a thin (weak) lithosphere.
  • Tectonics causes long cracks (valleys or ridges) on plane- tary surfaces. 6.4 Erosion
  • Only planets with atmospheres have significant erosion.

7. The Planets

Mercury Venus Earth Moon Mars Cratering *** - - *** *** Volcanism ** *** ** ** ** Tectonics * ** *** - - Erosion - * *** - **