DOC PREVIEW
UA PTYS 206 - Lecture Notes

This preview shows page 1-2-22-23 out of 23 pages.

Save
View full document
View full document
Premium Document
Do you want full access? Go Premium and unlock all 23 pages.
Access to all documents
Download any document
Ad free experience
View full document
Premium Document
Do you want full access? Go Premium and unlock all 23 pages.
Access to all documents
Download any document
Ad free experience
View full document
Premium Document
Do you want full access? Go Premium and unlock all 23 pages.
Access to all documents
Download any document
Ad free experience
View full document
Premium Document
Do you want full access? Go Premium and unlock all 23 pages.
Access to all documents
Download any document
Ad free experience
Premium Document
Do you want full access? Go Premium and unlock all 23 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

Electromagnetic Radiation andScientific InstrumentsPTYS 206-2April 1, 2008Announcements• Deep Impact 6 PM Wednesday Night– Pizza, no beer• Watch at home if you can’t watch here. It willbe discussed in class on Thursday• New homework posted todayThe Cassini SpacecraftScientific InstrumentsRadiation• Cameras• Spectrometers(UV, Vis, IR)• Radar• Radio• Laser altimetersFields and Particles• Mass spectrometers• Magnetometers(measures magneticfields)• Langmuir probes(measures electricalcurrents)• Energetic particledetectorsCCD Cameras, from Astronomers to youThe array of CCDs used onthe Sloan Digital Sky SurveyClose-up of a CCD chipSomething bought in WalmartHow CCDs WorkHow It Works: The Charged-Coupled Device, or CCD by Courtney Peterson, Journalof Young InvestigatorsThe image area is divided up into anarray of very small (10µm x 10µm)individual detectors called pixels.Filters Separate light intowavelengthsThe set of filters used on theHubble Space Telescope CameraOptical (Interference)FiltersCassini CameraImaging Science Subsystem (ISS)Narrow Angle Camera (NAC)Actual Photo - basicallya 10 cm focal lengthtelescopeMechanical DiagramRemember the ElectromagneticSpectrumTwo Kinds of LightAll warm bodies emit radiation.We can characterize the radiation from objects asreflected or emitted.Reflected radiation is light that is produced by aanother object (usually the Sun) that then bounces offthe object being studied.Emitted radiation is produced by the object itself, as aconsequence of its temperature. Usually, UV and visible light are reflected radiationand IR light is emitted radiation.Spectrum:1 a band of colors, as seen in a rainbow, produced byseparation of the components of light by their differentdegrees of refraction according to wavelength.•the entire range of wavelengths of electromagnetic radiation.•An image or distribution of components of anyelectromagnetic radiation arranged in a progressive seriesaccording to wavelength.•A similar image or distribution of components of sound,particles, etc., arranged according to such characteristics asfrequency, charge, and energy.2 used to classify something, or suggest that it can beclassified, in terms of its position on a scale between twoextreme or opposite points : the left or the right of the politicalspectrum. a wide range : self-help books are covering a broader andbroader spectrum.The First Spectrometer was a PrismSpectrometersBreaks light into the contributions from variouswavelengths. This is what scientists call a spectrum.Stefan-Boltzmann Law! P ="#T4All objects emit electro-magnetic radiation. Thepower radiated by anobject at temperature T isproportional to the temp-erature to the 4th power.P is the power radiatedσ= 5.67×10-8 W m-2 K-4 isthe Stefan-Boltzmannconstantε is the emissivity, usuallyequal to ~1.Wein’s Law: λ= 0.003/TThe temperature of an objectdetermines the spectrum of itsemitted radiation.High temperatures imply shortwavelengths; lowtemperatures imply longwavelengths.The wavelength at whichmost of the radiation isemitted is inverselyproportional to thetemperature.Wein’s Lawλ = 0.003/Tλ is the wavelength in metersT is the temperature in KelvinsThe lava from this volcano glowsbecause it is hot.Spectrum of Thermal RadiationThe peak of the curve isdetermined by Wein’s law.The area underthe curve isdetermined by theStefan-Boltzmannlaw.The spectrum of radiationfrom warm bodies has acharacteristic shape.Spectrum Variations with TemperatureThe Sun emits visible light.The Spectrum of the Sun.The Sun’s surfacetemperature is 6000K.Thus it emits radiation ata wavelength ofλ= 0.003/6000 metersλ= 5×10-6 metersThis is in the middle ofthe visible spectrumEarth emits IR radiationEarth’s temperature is300K, and thus radiatesat a peak wavelength ofλ = 0.003 / 300 meters,λ = 10x10-6 meters.This is in the infraredregion of the spectrum.Spectra Identify MaterialsEmission featuresAbsorption featuresSpectral Features from TitanAt ultraviolet wavelengthswe see emissionscharacteristic of nitrogenand hydrogenAt visible and near infraredwavelengths we see absorptionfeatures due to methane.Methane = CH4 = swamp gasReflected LightEmitted LightThermal Emissions from Titanidentify numerous


View Full Document

UA PTYS 206 - Lecture Notes

Documents in this Course
Titan

Titan

40 pages

Planets

Planets

18 pages

Comets

Comets

34 pages

Exam 1

Exam 1

8 pages

Mercury

Mercury

33 pages

Craters

Craters

32 pages

Earth

Earth

42 pages

Mars

Mars

36 pages

Venus

Venus

36 pages

The Sun

The Sun

37 pages

The Moon

The Moon

35 pages

The Moon

The Moon

35 pages

Load more
Download Lecture Notes
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view Lecture Notes and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view Lecture Notes 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?