Sources 1/2
- Model 634 Deuterium source (side on,
Sources 1/2 Model 634 Deuterium source (side on, MgF2 window, 30 W) - - PowerPoint PPT Presentation
Sources 1/2 Model 634 Deuterium source (side on, MgF2 window, 30 W) for vacuum ultraviolet and UV range 115 to 300nm Sources 2/2 Model 621 universal chimney-type lamp housing with forced air cooling, safety interlock, 150 W Xenon Arc
Xe lamp (250-600 nm) D2 lamp (115-250 nm)
Vacuum manual filter wheel with 5-posn, 25mm DIA:
Exit slit
28mm(1–1/8 Inch) Diameter, 11–stage, Bialkali Photocathode, Head–On Type, Low Dark Current, High Stability,Low Profile (R6094)
GENERAL
Parameter Description/Value Unit Spectral Response 300 to 650 nm Wavelength of Maximum Response 420 nm Photocathode MateriaI Bialkali Structure Number of Stages Minimum Effective Area 25 mm dia. Window MateriaI Borosilicate glass Dynode Base Suitable Socket Box and Line 11 14–pin glass base E678–14C (supplied)
PHOTOMULTlPLlER TUBES
R6094, R6095
TPMHB0223EA
200 800 600 400 0.01 0.1 1 10 100 CATHODE RADIANT SENSITIVITY (mA / W) QUANTUM EFFICIENCY (%) WAVELENGTH (nm) QUANTUM EFFICIENCY CATHODE RADIANT SENSITIVITY
Sodium salicylate is the most popular scintillator we use today. Sodium salicylate has excellent fluorescent efficiency, nearly constant response in the 30 to 300nm spectral region, is easy to prepare, and does not affect vacuum pressure. Stability of fluorescence efficiency is excellent over time in vacuum systems with clean dry vacuum pumps. We have systems in the field using it for more than twenty years with continued good
Emission Wavelength: 420nm Decay Time: 7-12 nanoseconds Characteristic: Crystalline layer of approximately 1-2mg/cm2 Fluorescence Efficiency: ~60% for incident wavelengths 40 to 300nm
spectra, obtained before and after the sample spectrum.
min
Lyot, 1929
“per mille” or “per thousand” symbol
1971, Dollfus & Bowell
14
128
Bo
eo 120 160
LBO
Angle of vision in degrees A-Mixture of ashes, of 0.13 albedo
B -Average curve for the Moon
Figure 51. Lunar Ground and Volcanic Ashes area is 0.13. This number represents fairly well the average albedo
definition employed in the present work (1). The curve B of Fig. 51 is the average of the curvesfor the first quarter and the last quarter
similarity between the curves A and B is remarkable, considering the great dif- ferences that the curves
materials show. On the
hand, the volcanic ashes scatter back in the direction of the source, even for very high angles
ized light which is smaller than that of all the other substances studied. This proportion never 'exceeds the ratio of 1/1000. I have shown (French page
46) however,
that the Moon shows this effect
very faintly. Finally, the lunar ground, when
illuminated, scatters much more light in the direction close to the Sun than in the opposite direction. The
same is true of an
area covered with dull powders and especially with volcanic ashes. All these similarities lead us to conclude that the Moon must be almost completely covered with powders having a constitution similar to that of the Earth's volcanic ashes. These powders could also be in the form of a very
(1)
The value of this quantity is poorly known. Zollner gave the value
Annuaire du Bureau des Longitudes gives the value
and Stewart gives for the most probable average value for the brightness of the full Moon a value
for the albedo).
Accessible with LASP TREX lab Roughly: 10 – 100deg (exact range TBD)
VPF-100)
cable (Lakeshore 325)
1970, Coyne & Pellicori
Coyne GV, Pellicori SF (1970) Wavelength dependence of polarization. xx. the integrated disk of the moon. Astron J. 75:54-60. doi:10.1086/110940
200 300 400 500 wavelength (nm) 0.00 0.05 0.10 0.15 0.20 0.25 polarization WUPPE (not full disk) [8] SOLSTICE Coyne & Pellicori [7] waning waxing
Fox et al, 1998, WUPPE, MNRAS 298 Coyne & Pellicori, 1970, Astron. J. 75 60° phase
21