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Measurement of thermal and net radiation

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Lg Ground Thermal. Loe Emitted Outgoing Thermal. Infrared Thermometer (IRT) ... If IRT sensor surface (generally blackened thermopile) has e close to 1, then ... – PowerPoint PPT presentation

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Title: Measurement of thermal and net radiation


1
Measurement of thermal and net radiation
Sd - Solar Diffuse
Sb - Solar Beam
La Sky Thermal
Loe Emitted Outgoing Thermal
Sr - Solar Reflected
Lg Ground Thermal
2
Infrared Thermometer (IRT)
  • Useful for non-contact measurement of surface T
  • IRTs measure F (radiant flux density)
  • If IRT sensor surface (generally blackened
    thermopile) has e close to 1, then

3
Infrared Thermometer (IRT)
Ideally.
4
IRT absorption spectrum
  • Most IRTs have filters that only pass 8-13 µm
    radiation
  • Why?

Atmospheric Emittance (clear sky)
5
Measuring T with IRTs
  • IRTs measure radiant flux density (F, W/m2)
  • If radiating surface is not a black body, F is
    made up of emitted component and reflected
    component
  • Only emitted component affected by T

Total Fseen by IRT Femitted by surface F
emitted by surroundings and reflected
(error)
6
Errors in IRT from reflected radiation
From previous slide
What happens if Ti Ts?
7
Errors in IRT from reflected radiation
From previous slide
What happens if es 1 ?
8
Magnitude of error when e?1 and Ts ? Ti
  • Generally less than 1 C under clear skies
  • Much less under cloudy skies or indoors
  • Correction not needed except in extreme
    situations
  • Well create one of those situations in lab

9
Determining emissivity of a surface
Solving our favorite equation for es
So if you can measure TT, Ts, and Ti, you can
calculate es
10
Pyrgeometers
  • Measure only thermal radiation
  • Dome is specially designed to reflect solar and
    transmit thermal radiation
  • Hemispherical view (unlike IRT)

11
Measurement of Total Radiation
  • Total radiation solar thermal
  • Now we need both wavelengths to reach sensing
    surface
  • Still need protection from convection..
  • Can we still use a glass dome?
  • Can we use black and white sensor?

12
Total radiometer
solar in
thermal in
thermal emitted
conduction to base
If you assume as al e 1
C Calibration constant V mV output Need to
know Tb!
13
Measurement of Net Radiation
  • Rn total incoming total outgoing total
    radiation absorbed by surface
  • Two ways to measure
  • Summation of radiation components measured
    independently
  • Net radiometers

14
Component Summation
  • Most accurate method
  • Expensive several thousand for each sensor

15
Net Radiometers
  • Less Expensive, Less accurate
  • Measure temperature difference between upward and
    downward facing surface

16
Net Radiometers
Rn Sd Ld Su - Lu
Only need to measure mV output to get Rn! (all
emissivity, absorptivity, and Tbase terms cancel
out)
17
Calibration of total and net radiometers
  • Short wave calibration
  • Use a known standard (Eppley or Kipp pyranometer)
  • Shade simultaneously on a clear day
  • Long wave altered only slightly
  • Direct short wave altered equally
  • From standard pyranometer you know ?Sb
  • From radiometer you know ? mV
  • Radiation incident on opposite side must remain
    constant

Calibration ?Sb/ ? mV
18
Calibration of total and net radiometers
  • Long wave calibration
  • Alter long wave radiation with a long wave
    emitter (radiator)
  • Need to know
  • ? radiator temperature
  • Emissivity of radiator
  • Plate view factor
  • Radiation incident on opposite side must remain
    constant

19
Calibrating the radiometer for todays lab
?Tradiator measure with IRT or
thermocouple Emissivity radiator painted with
optical black paint, e 0.98 View Factor (F)

d distance between source and sensor L length
of the radiator edges
calibration ? F/?mV
20
Todays Lab (contd.)
  • Use IRT to measure longwave energy budget for a
    person
  • Pay attention to view factors
  • Look at thermal emissivities of different surfaces
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