1984
DOI: 10.1016/0004-6981(84)90009-x
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A literature survey on tracer experiments for atmospheric dispersion modelling studies

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Cited by 7 publications
(3 citation statements)
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“…An important step was the introduction of a fluorescent-particle tracer (Nickola, 1977), which allowed a sudden increase in the range of dispersion studied, from the few hundred metres allowed by the pitch smoke studies. Other early tracer substances include sulphur dioxide (Barad, 1958;Cramer et al, 1958;Haugen, 1959), uranine dye, zinc and cadmium sulphides (Haugen and Fuquay, 1963;Fuquay et al, 1964;Nickola, 1977), krypton-85 (Nickola, 1977;Heffter et al, 1984), rhodamine B (Nickola, 1977), spores and metal oxides (Vanderborght and Kretzschmar, 1984). A more comprehensive anthology and description of these early experiments are available elsewhere (Islitzer and Slade, 1968;Draxler, 1984).…”
Section: Introductionmentioning
confidence: 99%
“…An important step was the introduction of a fluorescent-particle tracer (Nickola, 1977), which allowed a sudden increase in the range of dispersion studied, from the few hundred metres allowed by the pitch smoke studies. Other early tracer substances include sulphur dioxide (Barad, 1958;Cramer et al, 1958;Haugen, 1959), uranine dye, zinc and cadmium sulphides (Haugen and Fuquay, 1963;Fuquay et al, 1964;Nickola, 1977), krypton-85 (Nickola, 1977;Heffter et al, 1984), rhodamine B (Nickola, 1977), spores and metal oxides (Vanderborght and Kretzschmar, 1984). A more comprehensive anthology and description of these early experiments are available elsewhere (Islitzer and Slade, 1968;Draxler, 1984).…”
Section: Introductionmentioning
confidence: 99%
“…The ATC observed were then compared with ATC modeled using a normal distribution plume equation determined by Briggs [5] for rural and urban environments, and by Doury [6] for the rural environment. These parametrizations were widely shared and used by the scientific community [7][8][9][10][11][12][13], and were established using field data, and are based on a discreet description of the atmospheric boundary layer. The parametrizations applied by Briggs depend on the Pasquill-Turner atmospheric classes [14] and the distance from the source, while Doury parametrizations depend on two stability conditions (normal diffusion and weak diffusion) and plume transfer time.…”
Section: Introductionmentioning
confidence: 99%
“…It has a variety of applications in engineering and electronics. SFa was formerly used extensively as a tracer for atmospheric dispersion studies, but for long range experiments it is now being superseded by perfiuorocarbons having lower backgrounds [Vanderborght and Kretzschmar, 1984]. Perfiuorodecalin is a dense liquid (specific gravity 1.9) which is immiscible with water, and has a very low solubility, < 10 -7 mol L -•.…”
Section: Introductionmentioning
confidence: 99%