10/07/2019                                                     Actinometer - Wikipedia
Actinometer
  Actinometers are instruments used to measure the heating power
  of radiation. They are used in meteorology to measure solar radiation
  as pyranometers, pyrheliometers and net radiometers.
  An actinometer is a chemical system or physical device which
  determines the number of photons in a beam integrally or per unit
  time. This name is commonly applied to devices used in the
  ultraviolet and visible wavelength ranges. For example, solutions of
  iron(III) oxalate can be used as a chemical actinometer, while
  bolometers, thermopiles, and photodiodes are physical devices giving
  a reading that can be correlated to the number of photons detected.
     Contents
     History
     Chemical actinometry
        Choosing an actinometer                                                    Actinometer instrument designed by Jules
        Chemical actinometry in the visible range                                  Violle and used to estimate the
     References                                                                    temperature of the Sun's surface.
  History
  The actinometer was invented by John Herschel in 1825; he introduced the term actinometer, the first of many uses of
  the prefix actin for scientific instruments, effects, and processes.[1]
  The actinograph is a related device for estimating the actinic power of lighting for photography.
  Chemical actinometry
  Chemical actinometry involves measuring radiant flux via the yield from a chemical reaction. It requires a chemical
  with a known quantum yield and easily analyzed reaction products.
  Choosing an actinometer
  Potassium ferrioxalate is commonly used, as it is simple to use and sensitive over a wide range of relevant wavelengths
  (254 nm to 500 nm). Other actinometers include malachite green leucocyanides, vanadium(V)–iron(III) oxalate and
  monochloroacetic acid, however all of these undergo dark reactions, that is, they react in the absence of light. This is
  undesirable since it will have to be corrected for. Organic actinometers like butyrophenone or piperylene are analysed
  by gas chromatography. Other actinometers are more specific in terms of the range of wavelengths at which quantum
  yields have been determined. Reinecke’s salt K[Cr(NH3)2(NCS)4] reacts in the near-UV region although it is thermally
  unstable.[2] [3][4] Uranyl oxalate has been used historically but is very toxic and cumbersome to analyze.
  Recent investigations into nitrate photolysis[5][6] have used 2-nitrobenzaldehyde and benzoic acid as a radical
  scavenger for hydroxyl radicals produced in the photolysis of hydrogen peroxide and sodium nitrate. However, they
  originally used ferrioxalate actinometry to calibrate the quantum yields for the hydrogen peroxide photolysis. Radical
https://en.wikipedia.org/wiki/Actinometer                                                                                     1/2
10/07/2019                                                  Actinometer - Wikipedia
  scavengers proved a viable method of measuring production of hydroxyl radical.
  Chemical actinometry in the visible range
  Meso-diphenylhelianthrene can be used for chemical actinometry in the visible range (400–700 nm).[7] This chemical
  measures in the 475–610 nm range, but measurements in wider spectral ranges can be done with this chemical if the
  emission spectrum of the light source is known.
  References
     1. Science, American Association for the Advancement of (April 25, 1884). "Notes and News" (https://books.google.
        com/books?id=h6zq_tFWAvUC&pg=PA527&dq=herschel+actinometer#v=onepage&q=herschel%20actinometer&
        f=false). Science. 3 (64): 527. Bibcode:1884Sci.....3..524. (http://adsabs.harvard.edu/abs/1884Sci.....3..524.).
        doi:10.1126/science.ns-3.64.524 (https://doi.org/10.1126%2Fscience.ns-3.64.524).
     2. Calvert, Jack G; James N Pitts (1966). Photochemistry. New York: Wiley and Sons. ISBN 0-471-13091-5.
     3. Taylor, H. A. (1971). Analytical methods techniques for actinometry in Analytical photochemistry and
        photochemical analysis. New York: Marcel Dekker Inc.
     4. Rabek, J. F. (1982). Experimental methods in Photochemistry and Photophysics. Chicester: Wiley and Sons.
        ISBN 0-471-90029-X.
     5. Anastasio, Cort; McGregor K.G. (2001). "Chemistry of fog waters in California's Central Valley: 1. In situ
        photoformation of hydroxyl radical and singlet molecular oxygen". Atmospheric Environment. 35 (6): 1079–1089.
        Bibcode:2001AtmEn..35.1079A (http://adsabs.harvard.edu/abs/2001AtmEn..35.1079A). doi:10.1016/S1352-
        2310(00)00281-8 (https://doi.org/10.1016%2FS1352-2310%2800%2900281-8).
     6. Chu, L; Anastasio, C. (2003). "Quantum Yields of Hydroxyl Radical and Nitrogen Dioxide from the Photolysis of
        Nitrate on Ice". Physical Chemistry A. 107 (45): 9594–9602. Bibcode:2003JPCA..107.9594C (http://adsabs.harvar
        d.edu/abs/2003JPCA..107.9594C). doi:10.1021/jp0349132 (https://doi.org/10.1021%2Fjp0349132).
     7. Brauer H-D; Schmidt R; Gauglitz G; Hubig S (1983). "Chemical actinometry in the visible (475-610 nm) by meso-
        diphenylhlianthrene". Photochemistry and Photobiology. 37 (6): 595–598. doi:10.1111/j.1751-
        1097.1983.tb04526.x (https://doi.org/10.1111%2Fj.1751-1097.1983.tb04526.x).
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https://en.wikipedia.org/wiki/Actinometer                                                                                  2/2