By Murray J McEwan
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Extra resources for Chemistry of the atmosphere
The difference is that in the rotating sector technique one follows the amplitude of the output signal as a function of modulation frequency, rather than the phase. In most applications the 'amplitude' which is measured is given by the relative yield of some chemical product , but measurements of the intensity of emitted light as a function of modulation frequency have also been used.
D. , J. geophys. Res . , 65, 370 ( 1960). Ditchburn, R. W. and Young, P. , J. atmos. terr. Phys. 24, 1 27 (1962). Hasson , V. and Nicholls, R. , J. , B, 4, 1 789 (1971). Hudson, R. , Rev . Geophys. , 9, 305 ( 1 971). Watanabe, K . , Inn, E . C. Y . , J. chem. , 21, 1026 (1 953). Wayne, R . , Ann. N. Y. Acad. , 171, 199 ( 1970). Cairns , R. B. and Samson, J. A. , Phys. Rev . , 139, Al403 (1965). Huffman, R. , Paulsen , D. , Larrabee, J . C. and Cairns, R . , J. geophys. , 76, 1028 ( 197 1). 12 Lofthus, A .
The small sampling leak L leads, via the mass spectrometer ion source S, to a diffusion pump D. In later versions of the apparatus jet J is replaced by a small sphere with six 0. 1 mm holes, and the jet is moved by an external magnet operating on an iron slug. Fig. 5 LABOR A TOR Y STUDIES 45 mixed with a large excess of argon or helium, through a microwave dis charge, and then observed the ensuing reaction of the atoms with 0 3 • The progress of the reaction was followed by monitoring the decrease in the 0 3 concentration, as indicated by the height of the peak at mass 48 , as a function of reaction time .
Chemistry of the atmosphere by Murray J McEwan