Radiometer
From Wikipedia, the free encyclopedia
A radiometer is a device used to measure the radiant flux or power in electromagnetic radiation. Although the term is perhaps most generally applied to a device which measures infrared radiation, it can also be applied to detectors operating any wavelength in the electromagnetic spectrum; a spectrum-measuring radiometer is also called a spectroradiometer.
Whenever describing a radiometer, the most important characteristics are:
- spectral range (what wavelengths)
- spectral sensitivity (what sensitivity versus wavelength)
- field of view (180 degrees or limited to a certain narrow field)
- directional response (typically cosine response or uni-directional response)
Radiometers can use all kinds of detectors; some are " thermal" that is absorbing energy and converting that to a signal, some sense photons (photodiode) having a constant response per quantum (light particle). In a common application, the radiation detector within a radiometer is a bolometer which absorbs the radiation falling on it and, as a result, rises in temperature. This rise can then be measured by a thermometer of some type. This temperature rise can be related to the power in the incident radiation.
An early detector of infrared and visible radiation (light) was the Crookes radiometer. A more sensitive device, employing a different principle, is the Nichols radiometer.
A Microwave radiometer operates in the Microwave region of the electromagnetic spectrum.
The term radiometer is occasionally used as shorthand for a Crookes radiometer, a device in which a rotor with dark and light vanes in a partial vacuum spins when exposed to light.
[edit] See also
- Pyranometer (instrument)
- Photometry (optics) Main article - explains technical terms and units
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