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Electromagnetic Spectrum

Electromagnetic Spectrum. Energy: low  medium  high. Electromagnetic Radiation: Quick Facts. There are different types of EM radiation, visible light is just one of them EM waves can travel in vacuum, no medium needed

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Electromagnetic Spectrum

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  1. Electromagnetic Spectrum Energy: low  medium  high

  2. Electromagnetic Radiation: Quick Facts • There are different types of EM radiation, visible light is just one of them • EM waves can travel in vacuum, no medium needed • The speed of EM radiation “c” is the same for all types and very high ( light travels to the moon in 1 sec.) • The higher the frequency, the smaller the wavelength (f = c) • The higher the frequency, the higher the energy of EM radiation (E= hf, where h is a constant)

  3. Visible Light • Color of light determined by its wavelength • White light is a mixture of all colors • Can separate individual colors with a prism

  4. Three Things Light Tells Us • Temperature • from black bodyspectrum • Chemical composition • from spectral lines • Radial velocity • from Doppler shift

  5. Temperature Scales

  6. Black Body Spectrum • Objects emit radiation of all frequencies, but with different intensities Ipeak Higher Temp. Ipeak Ipeak Lower Temp. fpeak<fpeak <fpeak

  7. Cool, invisible galactic gas (60 K, fpeak in low radio frequencies) Dim, young star (600K, fpeak in infrared) The Sun’s surface (6000K, fpeak in visible) Hot stars in Omega Centauri (60,000K, fpeak in ultraviolet) The higher the temperature of an object, the higher its Ipeak and fpeak

  8. Wien’s Law • The peak of the intensity curve will move with temperature, this is Wien’s law: Temperature* wavelength = constant = 0.0029 K*m So: the higher the temperature T, the smaller the wavelength, i.e. the higher the energy of the electromagnetic wave

  9. Example • Peak wavelength of the Sun is 500nm, so T = (0.0029 K*m)/(5 x 10-7 m) = 5800 K • Instructor temperature: roughly 100 F = 37C = 310 K, so wavelength = (0.0029K*m)/310 K = 9.35 * 10-6 m = 9350 nm  infrared radiation

  10. Measuring Temperatures • Find maximal intensity  Temperature (Wien’s law) Identify spectral lines of ionized elements  Temperature

  11. Color of a radiating blackbody as a function of temperature • Think of heating an iron bar in the fire: red glowing to white to bluish glowing

  12. Kirchhoff’s Laws: Dark Lines Cool gas absorbs light at specific frequencies  “the negative fingerprints of the elements”

  13. Kirchhoff’s Laws: Bright lines Heated Gas emits light at specific frequencies  “the positive fingerprints of the elements”

  14. Kirchhoff’s Laws • A luminous solid or liquid (or a sufficiently dense gas) emits light of all wavelengths: the black body spectrum • Light of a low density hot gas consists of a series of discrete bright emission lines: the positive “fingerprints” of its chemical elements! • A cool, thin gas absorbs certain wavelengths from a continuous spectrum dark absorption ( “Fraunhofer”) lines in continuous spectrum: negative “fingerprints” of its chemical elements, precisely at the same wavelengths as emission lines.

  15. Spectral Lines – Fingerprints of the Elements • Can use this to identify elements on distant objects! • Different elements yield different emission spectra

  16. Spectral Lines Origin of discrete spectral lines: atomic structure of matter Atoms are made up of electrons and nuclei Nuclei themselves are made up of protons and neutrons Electrons orbit the nuclei, as planets orbit the sun Only certain orbits allowed Quantum jumps!

  17. The energy of the electron depends on orbit When an electron jumps from one orbital to another, it emits (emission line) or absorbs (absorption line) a photon of a certain energy The frequency of emitted or absorbed photon is related to its energy E = h f (h is called Planck’s constant, f is frequency)

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