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Published byHarold Woods Modified over 9 years ago
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Measuring the Universe
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Electromagnetic Radiation
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Common frequency bands
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Electromagnetic Radiation Electromagnetic waves have two basic properties Specific wavelength Wave properties Wavelength, frequency Exhibit interference, diffraction, and polarization Specific energy Particle properties Energy in quantum units = photons Single photons can be detected by sensitive instruments
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Electromagnetic Radiation Energy of electromagnetic radiation is inherent in its frequency/band Intensity of EM radiation is measured in the number of photons Total transmitted or received energy is the photon energy (frequency) times intensity
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Electromagnetic Radiation EM equivalent Energy-Intensity curve
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Electromagnetic Radiation Low-energy photons have little interaction with material High-energy photons interact with everything Sensors are designed for interaction with EM waves/photons at specific frequencies/wavelengths
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Electromagnetic Radiation Radio frequencies Sensors: Metal wire antenna elements Interaction: Photons interact with ionosphere (mostly electrons) Observations: Radio frequencies are primarily used to examine planetary atmospheres
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Electromagnetic Radiation Microwave Sensors: Metal wire antenna elements Interaction: Microwave band photons interact with most materials Observations: Microwave frequencies are used for almost all planetary, stellar, and universe observations Versatile interaction with material Simple technology Extremely useful for detecting hydrogen The most abundant material in the universe Microwave band used for most communications
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Electromagnetic Radiation Infrared Sensors: Solid materials sensitive in the IR band Mostly crystals CCD imaging commonly used Interaction: IR photons interact with most materials Far IR has different character than near IR Observations: IR frequencies are used for many planetary, stellar, and universe observations Planetary observations common (warm) Useful for measure large red-shifted objects formed in the early universe Difficult to observe through the atmosphere
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Electromagnetic Radiation Visible Sensors: Films, solid materials sensitive in visible band Semiconductors commonly used for imaging CCD imaging usually most sensitive Interaction: Visible photons interact with almost all materials Different visible bands interact differently with most materials Observations: Visible band is the most commonly used for planets, stars, and universe Useful since our eyes are sensitive only to that band Some interference from the atmosphere
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Electromagnetic Radiation Ultraviolet Sensors: Solid materials Crystals commonly used for spectra and imaging CCD imaging available Interaction: UV photons interact with all materials Near UV – least energetic Extreme UV – highest energy Observations: UV used for planetary atmospheres and planetary/moon surface composition, stars, and galaxies UV technology difficult Completely absorbed by the atmosphere Telescopes must be placed on satellites
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Electromagnetic Radiation X-ray Sensors: Solid materials Mostly crystals Spectra and imaging CCD imaging available Interaction: X-ray photons interact strongly with all materials Soft X-ray – lower energies Hard X-rays – higher energies Observations: X-ray used to study stars, supernova, black holes, and galaxies X-ray technology difficult Completely absorbed by the atmosphere Telescopes must be placed on satellites
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Electromagnetic Radiation γ-ray Sensors: Solid materials Mostly crystals Spectra and imaging CCD imaging available Interaction: γ-ray photons interact very strongly with all materials Observations: γ -ray used to study some stars, supernova, black holes, and galaxies γ -ray technology difficult Completely absorbed by the atmosphere Telescopes must be placed on satellites
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Electromagnetic Radiation Common frequency bands
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