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Published byLionel White Modified over 7 years ago
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The “Monitor to measure the Integral TRAnsmittance” (MITRA)
and the “Cryogenic Solar Absolute Radiometer” (CSAR) IPC-XII Seminar, Davos, 12 October 2015 Benjamin Walter, Wolfgang Finsterle, Andre Fehlmann, Rainer Winkler, Ricco Soder, Markus Suter, Werner Schmutz
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WRR SI MOTIVATION Direct Solar Irradiance measurements [W m-2]
traceable (Fehlmann et al. 2012) WRR internal stray light scale difference 0.34 % ± 0.09 % (k=1) Intercomparisons: SI
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WRR SI MOTIVATION Direct Solar Irradiance measurements [W m-2]
traceable WRR CSAR = LINK directly traceable SI Intercomparisons SI - cryogenic radiometers
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The MITRA Instrument Transmittance depends on solar spectrum which
changes with air mass and atmospheric conditions WSG World Standard Group CSAR = Cryogenic Solar Absolut Radiometer entrance window Monitoring of transmittance entrance window
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Operation method & target uncertainty:
window IPC-XI uncertainty ≈ 1 % Previous uncertainty > 1 % sensing Measuring temperature rise Δt at both cavities reference cavity Target uncertainty for the CSAR: 0.01% (= 100 ppm) spectrally integrated transmittance MITRA requirement: uncertainty of tint < 100 ppm
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Measurements in front of the sun
WSG tracker outdoor conditions HELIOSTAT Laboratory conditions
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Measurements in front of the sun
Laboratory: - instrument stability = 150 ppm = 0.015% - heliostat windows: wavelength dependent reflectivity Outdoor: - instrument stability = 900 ppm ≈ 0.1% - Measurement influenced by: wind / temperature variations Two questions: 1. How accurate is the absolute value? 2. How to reduce wind and temperature variation problems in outdoor measurements?
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How accurate is the absolute value? Periodical recalibration !
Temperature differences must be very accurate: no long term stability of parameters Δt measurement uncertainty < 0.1 mk no generally valid thermometer calibration possible Periodical recalibration !
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How accurate is the absolute value?
Measured offset to validated simulations of Fehlmann: ± 300 ppm (k = 1) Calculated offset: ppm Good agreement between measured and calculated offset to simulations Periodical recalibration ± ppm (k = 1) depending on measurement conditions 2. wind and heat accumulation problem for outdoor measurements
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WIND and HEAT ACCUMULATION:
10°C warmer relative to ambient air temperature
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WIND and HEAT ACCUMULATION: Thermally-stable environment
wind cannot enter the cavity covered by the window wind influences both cavities similarly Thermally-stable environment wind shelter
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Thermally-stable environment
No wind influences and Heat accumulation problems anymore electrical and thermal insulation Indirect cooling of MITRA - 6 Peltier elements - CPU fans - PID - controller Constant backplate temperature ≈ ± 0.1 K
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Thermally-stable environment
Measurement on the WSG sun tracking platform ≈ 0.6 K Calibration of thermometers < ± 1 mK
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Thermally-stable environment
Measurement on the WSG sun tracking platform ≈ 0.6 K ≈ ± 100 ppm
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Thermally-stable environment
Measurement on the WSG sun tracking platform ≈ 0.6 K ≈ ± 100 ppm uncertainty =115 ppm mean(tint) = ≈ ± 100 ppm
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Thermally-stable environment
Measurement on the WSG sun tracking platform ≈ ± 100 ppm uncertainty =165 ppm mean(tint) = ≈ ± 100 ppm
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Summary MITRA improvements:
≈ ± 150 ppm Thermally-stable environment (Peltier cooling system) Outdoor instrument stability ≈ 150 ppm (k = 1) Periodical recalibration of thermometers Absolute value uncertainty about ppm (k = 1) 3. Overall uncertainty: ppm (k = 1)
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Summary MITRA improvements:
≈ ± 150 ppm Promising results Future improvements to reach the 100 ppm goal: Three cavity design to monitor the temperature drift Liquid cooling of the instrument Larger heatsink to provide more stable conditions
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Cryogenic Solar Absolute Radiometer (CSAR)
Cryocooler (Helium) 20 K reference block quartz window 10 mm cavity View limiting aperture apertures
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Cryogenic Solar Absolute Radiometer
Measurement procedure: Cleaning the windows One day for cooling CSAR to 20K Cavity characterization Electrical measurements every min Sampling rate = 3 s MITRA Helium pipes
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Cryogenic Solar Absolute Radiometer
IPC-XII DAY: CSAR measures about % lower than WRR
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Cryogenic Solar Absolute Radiometer
( k = 2 ) IPC-XII Good agreement with previous findings of difference between the WRR and the SI scales. Detailed values and uncertainties will follow soon ...
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Thank you for your attention! SUMMARY
MITRA: Thermally-stable environment (Peltier system) a.) No wind influences / convection / heat accumulation b.) Strongly reduce temperature drift c.) Remaining drift can empirically be corrected for d.) Periodical recalibration of thermometers d.) MITRA uncertainty ≈ ppm (k = 1) CSAR: a.) Overal stable performance b.) Preliminary results are in good agreement with previous findings that the SI scale is about 0.2% - 0.3% lower than WRR Thank you for your attention!
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