Astro 500 A500/L-15 1

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Astro 500 A500/L-15 1

Lecture Outline Spectroscopy from a 3D Perspective ü Basics of spectroscopy and spectrographs ü Fundamental challenges of sampling the data cube Approaches and example of available instruments Ø I: Grating-dispersed spectrographs Ø II: Fabry-Perot interferometry Ø III: Spatial heterodyne spectroscopy a lot of material A500/L-15 2

Approaches Examples of available instruments ü Grating-dispersed spectrographs ü basic spectrograph design ü dispersive elements Ø Long-slit spectrographs o General Observing Considerations Ø Double spectrographs + ADC s Ø Multi-objects spectrographs: slitlets vs fibers Ø Echelle spectrographs Ø 3D spectroscopy: coupling formats and methods o Fiber o Fiber+lenslet o Slicer o Lenslet o Filtered multi-slit Ø summary of considerations Ø sky subtraction A500/L-15 3

Grating-dispersed spectrographs dispersive elements - recap Implications for resolution, band-pass, efficiency, in instrument design Ø transmission vs reflection: o VPH transmission gratings preferred because of higher throughput, large size, customization, and resulting compact spectrograph geometry (minimize vignetting, maximize throughput). Novel, efficient modes possible: grism, double-gratings, notch gratings. o requires articulating camera - not always possible or practical. o VPH grisms an improvement if no articulation. Ø For the highest resolutions, high density VPH gratings may compete with echelles; double VPH gratings certainly will. Ø Echelle gratings get best combination of high dispersion and large anamorphic factors: better at packing spectral resolution elements on the detector, at the cost of less-compact (lossy) geometry and/or the need for larger optics. o white pupil designs ameliorate some of these problems. o No free lunch! A500/L-15 4

Grating-dispersed spectrographs basic spectrograph design Grating equation m λ = σ ( sin β + sin α ) (reflection) σ is groove separation (nm) Angular dispersion γ = dβ/dλ = m / σ cos β = (sin β + sin α) / λ cos β Linear dispersion dl/dλ = f 2 γ A500/L-15 5

Long-slit Spectra Geometry In the camera focal plane there is the dispersion direction perpendicular to the slit and the spatial direction along the slit. A500/L-15 6

in telescope focal plane Length set by decker seeing disk A500/L-15 7

General Spectrometer Observing Considerations On-chip binning S/N Order-blocking Atmospheric dispersion Resolution and slit-width A500/L-15 8

On-chip Binning On-chip binning: line# I You are going to sum over these lines in the extraction anyway. On-chip binning will reduce RN x #pixels stellar spectrum night-sky line spectral direction For LRIS-B, 0.15 arcsec/pixel in the spatial direction spatial direction A500/L-15 9

S/N for Spectral Observations On-chip binning: spatial direction I stellar spectrum line# S spectral pixel = lines R object t night-sky line spectral direction [ ] lines N spectral pixel = (R object t) + (R sky t) + RN 2 1 2 A500/L-15 10

Binning In the spectral direction, binning can reduce spectral resolution. If the FWHM of arc-lamp lines 5 pixels, you can start to think about binning. But Often you are interested in accurate line centers and higher moments of the spectral line profiles in which case, well sampled features are a good idea. A500/L-15 11

S/N for Spectral Observations Often sum counts again in the spectral direction to determine S/N resolution element. Note! Assumes sky noise is at the shot noise limit. Imperfectly modeled and subtracted sky lines are worse than this. For spectra the S/N usually varies considerably with wavelength: Ø Absorption, emission, continuum Ø Sky lines Ø System efficiency with wavelength A500/L-15 12

Orders and blocking filters m=1 m=2 m=3 400nm 200nm 133.3nm 800nm 400nm 266.6nm For order n, at λ n there is also order m light with wavelength λ m =(n/m)λ n A500/L-15 13

For higher orders with λ<310nm it s not an issue as the atmosphere cuts out all the light (can still be an issue for calibration sources). But, if you are working in the red (>640nm) in 1 st order, you need to block the 2 nd order light. If you are working in a higher order, may need to block red light from lower orders. A500/L-15 14

KPNO 2.1m Goldcam blue blocking filters A500/L-15 15

Dichroics and Double Spectrometers Telescope focal plane Reflection gratings grisms dichroic A500/L-15 16

Spectral Resolution R=λ/Δλ For slit spectra, depends on slit width and grating choice. What is the effective slit-width of a circular fiber? What is the effective slit-width of a tilted slit? A500/L-15 17

LRIS (Keck Obs WWW page) Typical information provided: Grating Name Grooves Blaze Wave Dispersion Spectral coverage (l/mm) (Å) (Å/pix) (Å/2048 pix) 150/7500 150 7500 4.8 9830 300/5000 300 5000 2.55 5220 400/8500 400 8500 1.86 3810 600/5000 600 5000 1.28 2620 600/7500 600 7500 1.28 2620 600/10000 600 10000 1.28 2620 831/8200 831 8200 0.93 1900 900/5500 900 5500 0.85 1740 1200/7500 1200 7500 0.64 1310 What order? What else do you need to know in order to calculate resolution? A500/L-15 18

Spectral Resolution Examples: Ø V filter: 5500Å/1000Å = 5.5 Ø LRIS-R: 1 ~4 pixels FWHM o 150 l/mm grating: R ~ 6500/20 ~ 325 o 600 l/mm grating: R ~ 6500/5 ~ 1300 o 1200 l/mm grating: R ~ 6500/2.6 ~ 2600 A500/L-15 19

Spectrometer Throughput Spectrometer throughput ranges from a few percent to ~50%. The losses accumulate fast. Dispersing elements are usually a big hit, then the losses at multiple surfaces go like (transmission) n where n is the number of surfaces in the collimator and camera elements (n can be pretty big). 0.98 8 * 0.7 * 0.8 = 0.47 Camera/coll grating ccd with 8 surfaces (often more) What s missing? A500/L-15 20

Slit Losses Another throughput issue: slit losses can be very significant! Applies to fibers too. A500/L-15 21

Other Losses Lens absorption (particularly in blue/nuv) Beam over-fill or blockage (vignetting) Fiber losses (transmission and surfaces) Slicer losses (optical surfaces) Telescope losses (mirrors) ADC losses Atmospheric absorption Other??? A500/L-15 22

Atmospheric dispersion Differential Atmospheric Dispersion (Filippenko, 1982, PASP, 94 715) Dispersion in the atmosphere causes chromatic distortion of images that gets larger at blue wavelengths at fixed airmass and larger with airmass at fixed central wavelength. Δθ = 206265 [(n λ1 1) (n λ2 1) ] tan(zd) index of refraction @X=1.5, 1.3ʺ separation between 350nm and 550nm zenith distance A500/L-15 23

X=1 X=1.5 Two problems: 1) Preferentially lose red (or blue) light out of the slit. 2) If guiding on a particular wavelength of light, the object at other wavelengths will move out of the slit. A500/L-15 24

Two solutions: Ø Align slit along the parallactic angle A500/L-15 25

Build an ADC A500/L-15 26

Uncorrected A500/L-15 27

Corrected with ADC A500/L-15 28

Linear ADC LADC displaces focus: Must repoint telescope Tilted focal surface -- must refocus telescope for prism separation and rotator angle Possible changes in vignetting Displaced pupil at grating (barely OK) Must oversize/displace prisms to minimize clear aperture A500/L-15 29

A500/L-15 30

Risely and Amici style ADC s Maximum dispersion Zero dispersion Pairs rotate depending on ZD What s needed for SALT? A500/L-15 31

Factor of 3+ KPNO 4m rotating `Risley prisms. Central guider wavelength A500/L-15 32