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Electromagnetic Radiation |
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Transmission of energy through space without physical connection through varying electric and magnetic fields
Ex. Light |
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Transmits energy without the physical transport of material |
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Water wave
Water just moves up and down
Wave travels and can transmit energy |
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Number of wave crests that pass a given point per second |
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Time between passage of successive crests
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Distance between successive crests |
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Speed at which crests move |
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The small range of the electromagnetic spectrum that human eyes percieve as light. Radiation outside this range is invisible to human eyes
(Different wavelengths of light) |
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Oscillating electric and magnetic fields. Changing electric field creates magnetic field, and vice versa. Created by accelerating charged particles. |
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No limit on wavelengths; different ranges have different names
(Radio waves, infrared, visible light, ultraviolet, X-rays, gamma rays) |
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Water boils: 212 F; 100 C; 373 K
Water freezes: 32 F; 0 C; 273 K
All thermal motion stops:
-459 F; -273 C; 0 K |
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Radiation emitted by an object depending only on its temperature
Tells the temperature of an object by being measured |
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1. Peak wavelength is inversely proportional to temperature (frequency is directly proportional to temperature)
2. Total energy emitted is proportional to fourth power of temperature |
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If one is moving toward a source of radiation, the wavelengths seem shorter; if moving away, they seem longer
Can change perceived frequency of radiation
Depends on relative speed of source and observer |
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Splits light into component colors |
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Single frequencies emitted by particular atoms |
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can be used to identify elements |
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If a continuous spectrum passes through a cool gas, atoms of the gas will absorb the same frequencies they emit
Can also be used to identify elements. |
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1. Luminous solid, liquid, or dense gas produces continuous spectrum
2. Low-density hot has produces emission spectrum
3. Continuous spectrum incident on cool, then gas produces absorption spectrum |
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Existence of spectral lines required new model of atom, so that only certain amounts of energy could be emitted or absorbed.
Bohr model had certain allowed orbits for electron |
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Correspond to energy differences between allowed levels
Modern model has electrol cloud rather than orbit |
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When light shines on metal, electrons can be emitted
Frequency must be higher than minimum, charachteristic of material
Increased frequency: more energetic electrons
Increased intensity: more electrons, same energy
Can only be understood if light behaves like particles |
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Absorption can boost an electron to the second (or higher) excited state |
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Two ways to decay:
1. Directly to ground state
2. Cascade one orbital at a time |
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Created when atoms absorb photons of right energy for excitation |
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Much more complicated spectra, many more possible states |
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Can be used to identify atoms |
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Can vibrate and rotate, besides having energy levels |
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Produce visible and ultraviolet lines |
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Much more complex than atomic spectra, even for hydrogen |
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Information that can be gleaned from spectral lines: |
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Chemical composition
Temperature
Radial velocity |
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Line broadening can be due to a variety of causes |
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The Doppler Shift may cause thermal broadening of spectral lines
Rotation will also cause broadening of spectral lines through the Doppler Effect |
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emitted by solid, liquid and dense gas |
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Hot gas has charachteristic emission spectrum
Spectra can be explained using atomic models, with electrons occupying specific orbitals
Emission and absorption lines result form transitions between orbitals |
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Molecules can also emit and absorb radiation when making transitions between vibrational or rotational states |
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Refraction/Refracting lens |
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The bending of a beam of light as it passes from one transparent medium into another. ex. glass
Uses a lens to gather and concentrate a beam of light |
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Uses a curved mirror to focus the incoming light |
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Modern telescopes are all reflectors: |
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Light traveling through lens is refracted differently depending on wavelength
Some light traveling through lens is abosorbed
Large lens can be very heavy, and can only be supported at edge
A lens needs to optically acceptable surfaces, mirror needs only one |
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Light-gathering power: Improves detail
Brightness proportional to square of radius of mirror |
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When better, can distinguish objects that are closer together |
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Proportional to wavelength and inversely proportional to telescope size-bigger is better |
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Charge-coupled devices are electronic devices, which can be quickly read out and reset |
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by computers can sharpen images |
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Atmospheric blurring is due to air movements |
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Solutions:
Put telescopes on mountaintops, especially in deserts
Put telescopes in space |
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Control mirrors based on temperature and orientation |
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Track atmospheric changes with laser; adjust mirrors in real time |
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Similar to optical reflecting telescopes
Prime focus
Less sensitive to imperfections (due to longer wavelength); can be made very large
Largest: Arecibo |
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Longer wavelength means poor angular resolution |
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Advantages of radio astronomy:
Can observe 24 hours a day
Clouds, rain, and snow don't interfere
Observations at an entirely different frequency; get totally different information |
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Combines information from several widely spread radio telescopes as if it came from a single dish
Resolution with be that of dish whose diameter= largest separation between dishes
Involves combining signals from two receivers; teh amount of interference depends on the direction of the signal
Can get radio images whose resolution is close to optical
Can also be done with visible light but is much more difficult due to shorter wavelengths |
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can produce an image where visible radiation is blocked; generally can use optical telescope mirrors and lenses
these telescopes can also be in space |
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Set of 66 radiotelecopes located in Chile |
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Must be done in space, as the atmosphere absorbs almost all uv rays |
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X rays and gamma rays will not reflect off mirrors as other wavelengths do;
X rays will reflect at a very shallow angle and can therefore be focused
Gamma rays cannot be focused at all; images are therefore coarse |
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Early astronomers knew Moon, stars, Mercury, Venus, Mars, Jupiter, Saturn, comets and meteors |
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Now known: The solor system has 169 moons, one star, eight planets, eight asteroids, more than 100 Kuiper belt objects, and many smaller asteroids, comets, and meteoroids
More than 800 extrasolar planets have been found |
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1. Orbital Period
2. Radius
3. Masses
4. Rotation Period
5. Density |
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1. can be observed
2. known from angular size
3. Newton's laws
4. from observations
5. can be calculated knowing radius and mass |
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All orbits but Mercury's are close to the same plane
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Because the planet's orbits are close to being in plane, it is possible for them to appear in a straight line as viewed from Earth |
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Mercury, Venus, Earth, Mars
Small and rocky
Close to the Sun
rotate slowly
Weak magnetic fields
Few moons
No rings |
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Jupiter, Saturn, Uranus, Neptune
Large and gaseous
Far from the Sun
Rotate quickly
Strong magnetic fields
Many moons
Rings |
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Differences among the terrestrial planets |
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All have atmospheres; but they are very different; surface conditions vary as well]
Only Earth has oxygen in its atmosphere and liquid water on its surface
Earth and Mars spin at about the same rate; Mercury is much slower, Venus is slow and retrograde
Only Earth and Mars have moons
Only Earth and Mercury have magnetic fields |
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Gravitational slingshots can change direction of spacecraft and also accelerate it |
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Asteroids and meteoroids have rocky composition; asteroids are bigger
Comets are icy with some rocky parts
Pluto, once classified as one of the planets, is the closest large Kuiper belt object to the sun |
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Find out the Doppler Shift for lightwave when the recession velocity between the object and the source is 27 km/s |
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27 km/s
_______________________= 0.009%
300,000 km/s |
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20 km/s
__________________=0.007%
300,000 km/s |
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Find out how much energy is emitted by a single light particle for a frequency 3000 per second |
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E=(6.63 x 10^-34) x 3000=
1.989 x 10^-30 J |
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