actinometer

Actinometers are instruments used to measure the heating power of radiation. They are used in meteorology to measure solar radiation as pyrheliometers.

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 (e.g. potassium ferrioxalate) 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.

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^{[1] [2][3]}. Uranyl oxalate has been used historically but is very toxic and cumbersome to analyze.

Recent investigations into nitrate photolysis^[4][5] 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 scavengers proved a viable method of measuring production of hydroxyl radical.

References

1. ^ Calvert, Jack G; James N Pitts (1966). Photochemistry. New York: Wiley and Sons. 
2. ^ Taylor, H. A. (1971). Analytical methods techniques for actinometry in Analytical photochemistry and photochemical analyis. New York: Marcel Dekker Inc. 
3. ^ Rabek, J. F. (1982). Experimental methods in Photochemistry and Photophysics. Chicester: Wiley and Sons. 
4. ^ 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. doi:10.1016/S1352-2310(00)00281-8. 
5. ^ 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. doi:10.1021/jp0349132.