Lecture 5

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University of Virginia *

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1210

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Astronomy

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Oct 30, 2023

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Announcements HW 2 due Wednesday @ 11:59 PM Telescope lab sign ups available Learning from Light Types of Spectra in Astronomy Continuous spectra (emitted by sufficiently dense objects) Continuous spectrum with dark lines (absorption spectrum) Bright line spectra Bohr Model of the Atom Toy model of an atom Electrons orbit the nucleus at discrete energy levels Orbits are given by numbers, n, based on their energy level To change orbits, an electron must change energy Higher energy states correspond to higher n levels It’s like rungs on a ladder Absorption To go from a lower level to a higher level, the electron must increase in energy It can do this by absorbing a photon that has exactly the amount of energy needed to go from the lower level to the upper level Emission To go from a higher level to a lower level, the electron must give up energy (emit a photon) The emitted photon has exactly the difference between the two levels Ionization It is possible to give the electron though energy to completely escape from the aton. The atom is then said to be ionized. The amount of energy required to ionize an atom is called the ionization energy
The ionization energy can be provided by photons or by collisions The resulting atom is left with a net positive charge Energy Level Transitions The only allowed changed in energy are those corresponding to a transition between energy levels The energy stored in an electron is measured in “eV” or electron volts Chemical Fingerprints Each type of atom has a unique spectral fingerprint. The correspond to its allowed electron levels Observing the fingerprints in a spectrum tells us which kinds of atoms are present What is temperature? Temperature is a direct measurement of the internal motions of atoms and molecules in an object The higher an object’s temperature, the faster its particles are moving The temperature of an object species the average thermal energy (or heat) of the particles it contains Measuring Temperature Scientists often use the Kelvin scale: A change in temperature of 1 K is the same as a change of 1 o C 0k (absolute zero) is the point at which all molecular motion ceases 0k = 273 o C = -459 o F Absolute zero is the lowest possible temperature For comparison, the temperature of the atmosphere of the earth is about 300K Thermal Radiation Nearly all large or dense objects emit thermal radiation, including stars, planets, and people An object’s thermal radiation spectrum depends on only one property: its temperature Properties of Thermal Radiation Hotter objects emit more light at all frequencies per unit area Hotter objects emit photons with a higher average energy Wien’s Law The higher the temperature, the shorter the wavelength of peak radiation: Lambda max = 2.9E 6 /T Lambda max is the wavelength of the peak, in nm, and T is the temperature in Kelvin Speed of a Distant Object
The Doppler Shift can tell you about the relative motion of distant objects because photons behave as waves
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