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Blackbody Radiation & Atomic Spectra. “Light” – From gamma-rays to radio waves The vast majority of information we have about astronomical objects comes.

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Presentation on theme: "Blackbody Radiation & Atomic Spectra. “Light” – From gamma-rays to radio waves The vast majority of information we have about astronomical objects comes."— Presentation transcript:

1 Blackbody Radiation & Atomic Spectra

2 “Light” – From gamma-rays to radio waves The vast majority of information we have about astronomical objects comes from light they either emit or reflect Here, “light” stands for all sorts of electromagnetic radiation A type of wave, electromagnetic in origin Understanding the properties of light allows us to use it to determine the –temperature –chemical composition –(radial) velocity of distant objects

3 Waves Light is a type of wave Other common examples: ocean waves, sound A disturbance in a medium (water, air, etc.) that propagates Typically the medium itself does not move much

4 Wave Characteristics Wave frequency: how often a crest washes over you Wave speed = wavelength ( )  frequency (f)

5 Electromagnetic Waves Medium = electric and magnetic field Speed = 3  10 5 km/sec

6 Electromagnetic Spectrum Energy: low  medium  high

7 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= h f, where h is a constant)

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

9 Three Things Light Tells Us Temperature –from black body spectrum Chemical composition –from spectral lines Radial velocity –from Doppler shift

10 Temperature Scales FahrenheitCentigradeKelvin Absolute zero  459 ºF  273 ºC 0 K Ice melts32 ºF0 ºC273 K Human body temperature 98.6 ºF37 ºC310 K Water boils212 ºF100 ºC373 K

11 Black Body Spectrum Objects emit radiation of all frequencies, but with different intensities Higher Temp. Lower Temp. I peak f peak <f peak <f peak

12 Cool, invisible galactic gas (60 K, f peak in low radio frequencies) Dim, young star (600K, f peak in infrared) The Sun’s surface (6000K, f peak in visible) Hot stars in Omega Centauri (60,000K, f peak in ultraviolet) The higher the temperature of an object, the higher its I peak and f peak 14

13 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

14 Example: Wien’s Law Sun T=6000K, Earth t=300K (or you!) The Sun is brightest in the visible wave lengths (500nm). At which wave lengths is the Earth (or you) brightest? Wien: peak wave length is proportional to temperature itself  Scales linearly! Factor f=T/t=20, so f 1 =20 1 =20, so peak wavelength is 20x500nm=10,000 nm = 10 um Infrared radiation!

15 Energy & Power Units Energy has units Joule (J) Rate of energy expended per unit time is called power, and has units Watt (W) Example: a 100 W = 100 J/s light bulb emits 100 J of energy every second Nutritional Value: energy your body gets out of food, measured in Calories = 1000 cal = 4200 J Luminosity is the same as power radiated

16 Stefan’s Law A point on the Blackbody curve tells us how much energy is radiated per frequency interval Question: How much energy is radiated in total, i.e. how much energy does the body lose per unit time interval? Stefan(-Boltzmann)’s law: total energy radiated by a body at temperature T per second: P = A σ T 4 σ = 5.67 x 10 -8 W/(m 2 K 4 )

17 Example: Stefan-Boltzmann Law Sun T=6000K, Earth t=300K (or you!) How much more energy does the Sun radiate per time per unit area? Stefan: Power radiated is proportional to the temperature (in Kelvin!) to the fourth power Scales like the fourth power! Factor f=T/t=20, so f 4 =20 4 =2 4 x10 4 =16x10 4  160,000 x

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

19 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

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

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

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

23 Kirchhoff’s Laws 1.A luminous solid or liquid (or a sufficiently dense gas) emits light of all wavelengths: the black body spectrum 2.Light of a low density hot gas consists of a series of discrete bright emission lines: the positive “fingerprints” of its chemical elements! 3.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.

24 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!

25 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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