logging in or signing up astro101 2000oct CoolDude26 Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 74 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: November 15, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Far-IR/Submillimeter Astronomy: Far-IR/Submillimeter Astronomy Astronomy 101 Dr. C. Darren Dowell, Caltech Submillimeter Observatory 11 October 2000 http://www.submm.caltech.edu/~cdd/classOutline: Outline Kirchhoff’s Law Far-infrared/submillimeter emission Atmospheric constraints, observatories Detectors Observing strategies Bolometers A submillimeter cameraKirchhoff’s Law: Kirchhoff’s Law Absorptivity = emissivity Example 1: A 99% reflective mirror absorbs 1% of radiation incident on it. This means it must also emit with a spectrum given by: F(n) = B(n) × 1% Example 2: Spacecraft radiators (directed toward cold outer space) are coated with black (absorptive) paint to cool efficiently.Where is the far-IR/submillimeter?: Where is the far-IR/submillimeter? A useful definition: Far-IR: l = 30 mm to 300 mm, which is unobservable from the ground Submillimeter: l = 300 mm to 1 mm, partially available from high, dry mountains In frequency units, 31011 Hz to 11013 Hz Compare: Visual wavelengths at l 0.5 mm 61016 Hz Commercial FM radio at l 3 m 1108 HzSources of far-IR/submillimeter emission: Sources of far-IR/submillimeter emission Continuum Blackbody emission from solar system objects and stars ‘Graybody’ emission from dusty nebulae Free-free (bremsstrahlung) emission from ionized gas Synchrotron emission from relativistic electrons spiraling around magnetic fields Line Rotational transitions of molecules Electronic transitions in atoms (large prinicipal quantum number ‘n’, fine structure)Vela/Puppis Nebula seen by IRAS: Vela/Puppis Nebula seen by IRASDust in the Interstellar Medium: Dust in the Interstellar Medium Dust grains are made of silicate and graphite material, coated with ices in cold regions. There is a grain size distribution (more small grains, fewer large grains); an average size of 0.1 mm gives the best fit in simple models. Dust is intermixed with H2 in molecular clouds, with M(dust)/M(H2) 0.01. The majority of dust emission is from nebulae with ongoing star formation, where the dust is heated by nearby stars.Emission from a single dust grain: Emission from a single dust grain F(n) = A Q(n) B(n,T) / D2 F(n) = flux density (measured intensity) A = geometrical cross section = pr2 Q(n) = emissivity (modification to cross section) B(n,T) = Planck function D = distance from observer to dust grain AQ(n) = emission cross section = absorption cross section (by Kirchhoff’s Law) Q(n) 1 at ultraviolet wavelengths. Q(n) falls as l-2 at submillimeter wavelengths. Nebulae which are visually opaque are usually transparent in the far-IR/submillimeter.Comparison of optical/IR with far-IR/submillimeter: Comparison of optical/IR with far-IR/submillimeterThe Milky Way – An Edge-On Spiral Galaxy: The Milky Way – An Edge-On Spiral GalaxyThe Andromeda Galaxy (M 31): The Andromeda Galaxy (M 31)Continuum spectra of various objects: Continuum spectra of various objectsFar-IR/submillimeter emission lines: Far-IR/submillimeter emission lines Spectral lines are responsible for 5 to 50% of total far-IR/submillimeter emission from nebulae. Larger fraction for longer wavelengths; smaller fraction for shorter wavelengths. Largest fraction for environments where young stars are evaporating gas off dust grains.Submm. lines in the Orion Nebula: Submm. lines in the Orion NebulaRotational transitions: Rotational transitions Start with classical mechanics: I = m1m2R2/(m1+m2) J = Iw E = Iw2/2 Add quantum mechanics: J = {N(N+1)}1/2h/2p quantized n = DE/h, with DN = 1 most likely Then: E = h2N(N+1)/8p2I n = h(N+1)/4p2I {state N+1 state N} m1 m2 R C O wRotational transitions of Carbon Monoxide: Rotational transitions of Carbon Monoxide CO molecule: m1 = 12 amu = 2.0 × 10-26 kg m2 = 16 amu = 2.7 × 10-26 kg R = 1.1 Å = 1.1 × 10-10 m Plug in: I = m1m2R2/(m1+m2) = 1.4 × 10-46 kg m2 n = h(N+1)/4p2I = 121 GHz (N+1) Actually: n = 115.271 GHz, 230.538 GHz, 345.796 GHz, … 12 amu 16 amu 1.1 Å C OAtmospheric constraints: Atmospheric constraints Water vapor is the primary enemy of far-IR/submillimeter astronomy. Range l = 30 – 300 mm is unavailable from the ground. Other options: Airplanes (40,000 ft.) – KAO, SOFIA Balloons (120,000 ft.) Satellites – IRAS, ISO, SIRTF 300 mm – 1 mm range is partially available from high, dry mountains (> 10,000 ft.) – Mauna Kea (CSO, JCMT, SMA); South Pole; Chile (ALMA) l > 1 mm – available from lower elevationsSlide19: Mauna Kea, Hawaii (13,000 ft.) 1000 mm 300 mm‘Submillimeter Valley’, Mauna Kea: ‘Submillimeter Valley’, Mauna KeaCaltech Submm. Observatory – 10 m: Caltech Submm. Observatory – 10 mKuiper Airborne Observatory (1974-1995) – 0.9 m: Kuiper Airborne Observatory (1974-1995) – 0.9 mA telescope in an airplane (!): A telescope in an airplane (!)On the Kuiper Airborne Observatory: On the Kuiper Airborne ObservatoryStratospheric Observatory for Infrared Astronomy (2002) – 2.5 m: Stratospheric Observatory for Infrared Astronomy (2002) – 2.5 mSpace Infrared Telescope Facility (2002) – 0.85 m: Space Infrared Telescope Facility (2002) – 0.85 mAngular resolution in the far-IR/submillimeter: Angular resolution in the far-IR/submillimeter Diffraction for a single telescope: q 1.2 l / D Typical submillimeter telescope: D = 10 m, l = 800 mm q = 20” Interferometry can solve angular resolution problem: q 1.2 l / B, where B is the separation of two telescopes SMA: 1” ALMA (2007): 0.1” There are slow atmospheric ‘seeing’ (wavefront distortion) effects, but they can be corrected with sky monitors.Far-IR/submillimeter detectors: Far-IR/submillimeter detectors ‘Incoherent’ – light as a particle Photoconductors – 1 photon raises 1 electron from valence band to conduction band; works only for l < 200 mm Bolometers – photons raise the temperature of an absorber, which is measured by a thermistor ‘Coherent’ – light as a wave Heterodyne mixers – measure ‘beat frequency’ of cosmic radiation against a local oscillatorHeterodyne mixers: Heterodyne mixers Basic idea: Illuminate mixer element with radiation from the sky, and also radiation from a transmitter (‘local oscillator’). Beat frequencies get produced: Vsky = V1 sin (w1t – f1) VLO = V0 sin (w0t – f0) Voutput = (Vsky + VLO)2 = C sin [(w1-w0)t – f] + high frequency terms which get filtered out See Smith, p. 106, for exercise. Example: Line of interest at 345 GHz, LO at 344 GHz line appears at (345 – 344) = 1 GHz, a frequency which spectrometers can deal with.Difficulty of infrared/submillimeter astronomy from the ground: Difficulty of infrared/submillimeter astronomy from the ground Infrared astronomy from the ground has been likened to “observing in the day, with the telescope on fire”. Why? The atmosphere emits, and the telescope itself emits. Atmospheric emission is ~106 times brighter than the faintest source which can be detected in 1 hour. Telescope emission can be minimized with a good design.Optical telescope: Optical telescopeSubmillimeter telescope: Submillimeter telescopeObserving strategies: Observing strategies The terrestrial atmosphere absorbs heavily in the far-IR/submillimeter, so it must also emit. (Kirchhoff’s Law) Transmission = 60% emissivity = 40% T (atmosphere) = 270 K lpeak 2900 mm / T 10 mm significant emission on the Rayleigh-Jeans side of the spectrum. The atmospheric emission changes as ‘cells’ of water vapor drift by. Constant sky subtraction is necessary.One sky subtraction approach – chopping mirror: One sky subtraction approach – chopping mirror A mirror wobbles back and forth, causing the detector to view two different parts of the sky. (Smith, p. 128)Another sky subtraction approach – differential radiometer: Another sky subtraction approach – differential radiometer One pixel is ‘source + sky’, and two pixels are ‘sky’. This is similar to using edge pixels on a CCD to subtract the sky, but with a much worse sky and fewer pixels.Bolometer – diagram of 1 ‘pixel’: Bolometer – diagram of 1 ‘pixel’ Radiation is intercepted, absorber heats, and temperature change is measured by thermistor. weak thermal link wires cold bath at fixed temperature absorber thermistor radiationActual bolometers: Actual bolometersA closer look…: A closer look…An even closer look…: An even closer look… leg = thermal link, wire on top absorber: 1 mm square doped silicon thermistor (invisible)What is a thermistor?: What is a thermistor? A thermistor is a resistor whose resistance varies with temperature. Thermistors can be made out of semiconductors. When the temperature increases, more electrons enter the conduction band, and therefore the resistance goes down.Typical thermistor behavior: Typical thermistor behaviorIV curves – a useful method for analyzing detector performance: IV curves – a useful method for analyzing detector performance An applied current is necessary to measure a resistance.IV curve for a bolometer: IV curve for a bolometer linear region turnover, due to self-heatingNow add radiation…: Now add radiation… operating currentLimits to bolometer performance: Limits to bolometer performance The kinetic energy of the electrons and atoms in a bolometer limit its performance: Johnson noise – random voltage from fluctuations in the motion of electrons Phonon noise – random bolometer temperature from fluctuations of energy flowing down the thermal link The colder, the better. NEP: Smallest power which is detected in a 1 second integration; units W Hz-1/2 = W s1/2 State of the art: Bolometers at 0.3 K: NEP = 10-16 W s1/2 Bolometers at 0.1 K: NEP = 10-17 W s1/2A Lightbulb on the Moon?: A Lightbulb on the Moon? How much power can be collected by a 10 meter telescope from a 100 watt lightbulb at the distance of the Moon? P = 100 watts (pr2/4pd2) r = 5 m, d = 4 x 108 m Therefore, P = 4 x 10-15 watts In principle, one could easily detect the light bulb with a bolometer at 0.3 K. Detecting the light bulb might be more difficult than our simple calculation would indicate. Why?Bolometers – impartial detectors of radiation: Bolometers – impartial detectors of radiation Bolometers can detect radiation over a very broad range of the electromagnetic spectrum, from X rays to radio wavelengths Wavelength is contrained to passband of interest by choice of absorber and by choice of filters in front of detector. The bolometer is the superior broadband (Dl/l > 0.01) detector from l = 200 mm – 1 mm.SHARC II – a camera using bolometers: SHARC II – a camera using bolometers SHARC II – Submillimeter High Angular Resolution Camera, 2nd generation For the Caltech Submillimeter Observatory Observing at l = 350 mm Goal: 12 × 32 = 384 bolometers – the most submillimeter pixels in the world, by a factor of 3 Bolometers cooled to 0.3 K Started in 1997; first tests with 16 pixels in September 2000; finish in 2001(?)Goal: 2-dimension bolometer array: Goal: 2-dimension bolometer arrayCross section of SHARC II: Cross section of SHARC IIUseful cryogens for far-IR cameras: Useful cryogens for far-IR cameras Liquid cryogens are used at their boiling point temperature, since they are colder than their surroundings. Water as a ‘cryogen’ would provide a temperature of 373 K. Liquid nitrogen (N2) – 77 K Liquid helium (4He) at 1 atmosphere – 4.2 K Liquid 4He at 10-3 atmosphere – 1.5 K Liquid 3He at 10-3 atmosphere – 0.3 KAssembling the camera: Assembling the cameraAssembling the camera: Assembling the cameraNo Multi-Layer Insulation: No Multi-Layer Insulation P = net power flow = sAT14 – sAT04 = sA[T14 – T04] P T1 > T0 e = 1 = a T0 e = 1 = a sAT14 sAT04With one shield layer: With one shield layer Equilibrium of shield: sAT14a + sAT04a = 2sAT24e T24 = T14/2 + T04/2 P = sAT24e + sAT04(1-a) – sAT04 = sA(e/2) [T14 – T04] P T1 e = 1 = a T0 e = 1 = a sAT14 T2 e = a 1 sAT14a sAT14(1-a) sAT24e sAT24e sAT04(1-a) sAT04 sAT04aPutting it on the telescope: Putting it on the telescopeOn the telescope: On the telescopeInaugural image – Orion Nebula core: Inaugural image – Orion Nebula coreKey points – far-IR/submm. astronomy: Key points – far-IR/submm. astronomy Most of the far-IR/submillimeter emission from the universe comes from dust. Line emission is mostly from rotational transitions of simple molecules. The far-IR/submillimeter is particularly useful for studying the formation of stars, from nearby nebulae to high-redshift galaxies. The water in the Earth’s atmosphere absorbs most of far-IR/submillimeter radiation from space – the main motivation for airborne and spaceborne observatories. Far-IR/submm detectors include photoconductors, bolometers, and heterodyne mixers. Bolometers detect a small temperature rise from absorbed radiation. You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
astro101 2000oct CoolDude26 Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 74 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: November 15, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Far-IR/Submillimeter Astronomy: Far-IR/Submillimeter Astronomy Astronomy 101 Dr. C. Darren Dowell, Caltech Submillimeter Observatory 11 October 2000 http://www.submm.caltech.edu/~cdd/classOutline: Outline Kirchhoff’s Law Far-infrared/submillimeter emission Atmospheric constraints, observatories Detectors Observing strategies Bolometers A submillimeter cameraKirchhoff’s Law: Kirchhoff’s Law Absorptivity = emissivity Example 1: A 99% reflective mirror absorbs 1% of radiation incident on it. This means it must also emit with a spectrum given by: F(n) = B(n) × 1% Example 2: Spacecraft radiators (directed toward cold outer space) are coated with black (absorptive) paint to cool efficiently.Where is the far-IR/submillimeter?: Where is the far-IR/submillimeter? A useful definition: Far-IR: l = 30 mm to 300 mm, which is unobservable from the ground Submillimeter: l = 300 mm to 1 mm, partially available from high, dry mountains In frequency units, 31011 Hz to 11013 Hz Compare: Visual wavelengths at l 0.5 mm 61016 Hz Commercial FM radio at l 3 m 1108 HzSources of far-IR/submillimeter emission: Sources of far-IR/submillimeter emission Continuum Blackbody emission from solar system objects and stars ‘Graybody’ emission from dusty nebulae Free-free (bremsstrahlung) emission from ionized gas Synchrotron emission from relativistic electrons spiraling around magnetic fields Line Rotational transitions of molecules Electronic transitions in atoms (large prinicipal quantum number ‘n’, fine structure)Vela/Puppis Nebula seen by IRAS: Vela/Puppis Nebula seen by IRASDust in the Interstellar Medium: Dust in the Interstellar Medium Dust grains are made of silicate and graphite material, coated with ices in cold regions. There is a grain size distribution (more small grains, fewer large grains); an average size of 0.1 mm gives the best fit in simple models. Dust is intermixed with H2 in molecular clouds, with M(dust)/M(H2) 0.01. The majority of dust emission is from nebulae with ongoing star formation, where the dust is heated by nearby stars.Emission from a single dust grain: Emission from a single dust grain F(n) = A Q(n) B(n,T) / D2 F(n) = flux density (measured intensity) A = geometrical cross section = pr2 Q(n) = emissivity (modification to cross section) B(n,T) = Planck function D = distance from observer to dust grain AQ(n) = emission cross section = absorption cross section (by Kirchhoff’s Law) Q(n) 1 at ultraviolet wavelengths. Q(n) falls as l-2 at submillimeter wavelengths. Nebulae which are visually opaque are usually transparent in the far-IR/submillimeter.Comparison of optical/IR with far-IR/submillimeter: Comparison of optical/IR with far-IR/submillimeterThe Milky Way – An Edge-On Spiral Galaxy: The Milky Way – An Edge-On Spiral GalaxyThe Andromeda Galaxy (M 31): The Andromeda Galaxy (M 31)Continuum spectra of various objects: Continuum spectra of various objectsFar-IR/submillimeter emission lines: Far-IR/submillimeter emission lines Spectral lines are responsible for 5 to 50% of total far-IR/submillimeter emission from nebulae. Larger fraction for longer wavelengths; smaller fraction for shorter wavelengths. Largest fraction for environments where young stars are evaporating gas off dust grains.Submm. lines in the Orion Nebula: Submm. lines in the Orion NebulaRotational transitions: Rotational transitions Start with classical mechanics: I = m1m2R2/(m1+m2) J = Iw E = Iw2/2 Add quantum mechanics: J = {N(N+1)}1/2h/2p quantized n = DE/h, with DN = 1 most likely Then: E = h2N(N+1)/8p2I n = h(N+1)/4p2I {state N+1 state N} m1 m2 R C O wRotational transitions of Carbon Monoxide: Rotational transitions of Carbon Monoxide CO molecule: m1 = 12 amu = 2.0 × 10-26 kg m2 = 16 amu = 2.7 × 10-26 kg R = 1.1 Å = 1.1 × 10-10 m Plug in: I = m1m2R2/(m1+m2) = 1.4 × 10-46 kg m2 n = h(N+1)/4p2I = 121 GHz (N+1) Actually: n = 115.271 GHz, 230.538 GHz, 345.796 GHz, … 12 amu 16 amu 1.1 Å C OAtmospheric constraints: Atmospheric constraints Water vapor is the primary enemy of far-IR/submillimeter astronomy. Range l = 30 – 300 mm is unavailable from the ground. Other options: Airplanes (40,000 ft.) – KAO, SOFIA Balloons (120,000 ft.) Satellites – IRAS, ISO, SIRTF 300 mm – 1 mm range is partially available from high, dry mountains (> 10,000 ft.) – Mauna Kea (CSO, JCMT, SMA); South Pole; Chile (ALMA) l > 1 mm – available from lower elevationsSlide19: Mauna Kea, Hawaii (13,000 ft.) 1000 mm 300 mm‘Submillimeter Valley’, Mauna Kea: ‘Submillimeter Valley’, Mauna KeaCaltech Submm. Observatory – 10 m: Caltech Submm. Observatory – 10 mKuiper Airborne Observatory (1974-1995) – 0.9 m: Kuiper Airborne Observatory (1974-1995) – 0.9 mA telescope in an airplane (!): A telescope in an airplane (!)On the Kuiper Airborne Observatory: On the Kuiper Airborne ObservatoryStratospheric Observatory for Infrared Astronomy (2002) – 2.5 m: Stratospheric Observatory for Infrared Astronomy (2002) – 2.5 mSpace Infrared Telescope Facility (2002) – 0.85 m: Space Infrared Telescope Facility (2002) – 0.85 mAngular resolution in the far-IR/submillimeter: Angular resolution in the far-IR/submillimeter Diffraction for a single telescope: q 1.2 l / D Typical submillimeter telescope: D = 10 m, l = 800 mm q = 20” Interferometry can solve angular resolution problem: q 1.2 l / B, where B is the separation of two telescopes SMA: 1” ALMA (2007): 0.1” There are slow atmospheric ‘seeing’ (wavefront distortion) effects, but they can be corrected with sky monitors.Far-IR/submillimeter detectors: Far-IR/submillimeter detectors ‘Incoherent’ – light as a particle Photoconductors – 1 photon raises 1 electron from valence band to conduction band; works only for l < 200 mm Bolometers – photons raise the temperature of an absorber, which is measured by a thermistor ‘Coherent’ – light as a wave Heterodyne mixers – measure ‘beat frequency’ of cosmic radiation against a local oscillatorHeterodyne mixers: Heterodyne mixers Basic idea: Illuminate mixer element with radiation from the sky, and also radiation from a transmitter (‘local oscillator’). Beat frequencies get produced: Vsky = V1 sin (w1t – f1) VLO = V0 sin (w0t – f0) Voutput = (Vsky + VLO)2 = C sin [(w1-w0)t – f] + high frequency terms which get filtered out See Smith, p. 106, for exercise. Example: Line of interest at 345 GHz, LO at 344 GHz line appears at (345 – 344) = 1 GHz, a frequency which spectrometers can deal with.Difficulty of infrared/submillimeter astronomy from the ground: Difficulty of infrared/submillimeter astronomy from the ground Infrared astronomy from the ground has been likened to “observing in the day, with the telescope on fire”. Why? The atmosphere emits, and the telescope itself emits. Atmospheric emission is ~106 times brighter than the faintest source which can be detected in 1 hour. Telescope emission can be minimized with a good design.Optical telescope: Optical telescopeSubmillimeter telescope: Submillimeter telescopeObserving strategies: Observing strategies The terrestrial atmosphere absorbs heavily in the far-IR/submillimeter, so it must also emit. (Kirchhoff’s Law) Transmission = 60% emissivity = 40% T (atmosphere) = 270 K lpeak 2900 mm / T 10 mm significant emission on the Rayleigh-Jeans side of the spectrum. The atmospheric emission changes as ‘cells’ of water vapor drift by. Constant sky subtraction is necessary.One sky subtraction approach – chopping mirror: One sky subtraction approach – chopping mirror A mirror wobbles back and forth, causing the detector to view two different parts of the sky. (Smith, p. 128)Another sky subtraction approach – differential radiometer: Another sky subtraction approach – differential radiometer One pixel is ‘source + sky’, and two pixels are ‘sky’. This is similar to using edge pixels on a CCD to subtract the sky, but with a much worse sky and fewer pixels.Bolometer – diagram of 1 ‘pixel’: Bolometer – diagram of 1 ‘pixel’ Radiation is intercepted, absorber heats, and temperature change is measured by thermistor. weak thermal link wires cold bath at fixed temperature absorber thermistor radiationActual bolometers: Actual bolometersA closer look…: A closer look…An even closer look…: An even closer look… leg = thermal link, wire on top absorber: 1 mm square doped silicon thermistor (invisible)What is a thermistor?: What is a thermistor? A thermistor is a resistor whose resistance varies with temperature. Thermistors can be made out of semiconductors. When the temperature increases, more electrons enter the conduction band, and therefore the resistance goes down.Typical thermistor behavior: Typical thermistor behaviorIV curves – a useful method for analyzing detector performance: IV curves – a useful method for analyzing detector performance An applied current is necessary to measure a resistance.IV curve for a bolometer: IV curve for a bolometer linear region turnover, due to self-heatingNow add radiation…: Now add radiation… operating currentLimits to bolometer performance: Limits to bolometer performance The kinetic energy of the electrons and atoms in a bolometer limit its performance: Johnson noise – random voltage from fluctuations in the motion of electrons Phonon noise – random bolometer temperature from fluctuations of energy flowing down the thermal link The colder, the better. NEP: Smallest power which is detected in a 1 second integration; units W Hz-1/2 = W s1/2 State of the art: Bolometers at 0.3 K: NEP = 10-16 W s1/2 Bolometers at 0.1 K: NEP = 10-17 W s1/2A Lightbulb on the Moon?: A Lightbulb on the Moon? How much power can be collected by a 10 meter telescope from a 100 watt lightbulb at the distance of the Moon? P = 100 watts (pr2/4pd2) r = 5 m, d = 4 x 108 m Therefore, P = 4 x 10-15 watts In principle, one could easily detect the light bulb with a bolometer at 0.3 K. Detecting the light bulb might be more difficult than our simple calculation would indicate. Why?Bolometers – impartial detectors of radiation: Bolometers – impartial detectors of radiation Bolometers can detect radiation over a very broad range of the electromagnetic spectrum, from X rays to radio wavelengths Wavelength is contrained to passband of interest by choice of absorber and by choice of filters in front of detector. The bolometer is the superior broadband (Dl/l > 0.01) detector from l = 200 mm – 1 mm.SHARC II – a camera using bolometers: SHARC II – a camera using bolometers SHARC II – Submillimeter High Angular Resolution Camera, 2nd generation For the Caltech Submillimeter Observatory Observing at l = 350 mm Goal: 12 × 32 = 384 bolometers – the most submillimeter pixels in the world, by a factor of 3 Bolometers cooled to 0.3 K Started in 1997; first tests with 16 pixels in September 2000; finish in 2001(?)Goal: 2-dimension bolometer array: Goal: 2-dimension bolometer arrayCross section of SHARC II: Cross section of SHARC IIUseful cryogens for far-IR cameras: Useful cryogens for far-IR cameras Liquid cryogens are used at their boiling point temperature, since they are colder than their surroundings. Water as a ‘cryogen’ would provide a temperature of 373 K. Liquid nitrogen (N2) – 77 K Liquid helium (4He) at 1 atmosphere – 4.2 K Liquid 4He at 10-3 atmosphere – 1.5 K Liquid 3He at 10-3 atmosphere – 0.3 KAssembling the camera: Assembling the cameraAssembling the camera: Assembling the cameraNo Multi-Layer Insulation: No Multi-Layer Insulation P = net power flow = sAT14 – sAT04 = sA[T14 – T04] P T1 > T0 e = 1 = a T0 e = 1 = a sAT14 sAT04With one shield layer: With one shield layer Equilibrium of shield: sAT14a + sAT04a = 2sAT24e T24 = T14/2 + T04/2 P = sAT24e + sAT04(1-a) – sAT04 = sA(e/2) [T14 – T04] P T1 e = 1 = a T0 e = 1 = a sAT14 T2 e = a 1 sAT14a sAT14(1-a) sAT24e sAT24e sAT04(1-a) sAT04 sAT04aPutting it on the telescope: Putting it on the telescopeOn the telescope: On the telescopeInaugural image – Orion Nebula core: Inaugural image – Orion Nebula coreKey points – far-IR/submm. astronomy: Key points – far-IR/submm. astronomy Most of the far-IR/submillimeter emission from the universe comes from dust. Line emission is mostly from rotational transitions of simple molecules. The far-IR/submillimeter is particularly useful for studying the formation of stars, from nearby nebulae to high-redshift galaxies. The water in the Earth’s atmosphere absorbs most of far-IR/submillimeter radiation from space – the main motivation for airborne and spaceborne observatories. Far-IR/submm detectors include photoconductors, bolometers, and heterodyne mixers. Bolometers detect a small temperature rise from absorbed radiation.