Affection 发表于 2025-3-30 08:29:13
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https://doi.org/10.1007/978-3-658-14176-9ir pollution modeling.. The SRI model exists in several forms : The simpler form (EURMAP-1) can be used to obtain long-term averages ; the more complicated form (EURMAP-2 ) is used for short-term pollution episodes.沉思的鱼 发表于 2025-3-30 20:06:28
Nato Challenges of Modern Societyhttp://image.papertrans.cn/a/image/151786.jpg随意 发表于 2025-3-31 00:01:42
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https://doi.org/10.1007/978-3-658-08052-5An air pollution transport model is developed. It will be applied in an area which covers the Netherlands and (parts of) the surrounding countries (500 × 500 km.). Transport is described by变白 发表于 2025-3-31 05:15:08
Air Pollutant Reactions in Major Plumes Transported over the North SeaA study is being made of pollutant transport and transformation within a large number of major industrial and urban plumes. The North Sea to the west of The Netherlands was selected as the sampling area for the field experiments conducted during 1979 – 1981.exacerbate 发表于 2025-3-31 12:47:50
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Chemical Transformation in Plumesnitudes of the resultant pollutant concentrations depend on the chemical composition of a plume and of the ambient air entrained in a plume, the elevation and temperature of a plume, and the meteorological conditions (including solar intensity) experienced by a plume. It is postulated that these traoccurrence 发表于 2025-3-31 18:56:00
A Comparison between Chemically Reacting Plume Models and Windtunnel Experimentsfrom NO to NO. has been determined..Based on the results from these experiments and existing field studies, a critical review of chemically reacting plume models has been carried out..It is shown that in principle these models should take into account the effect of inhomogeneous mixing and the corre高贵领导 发表于 2025-3-31 23:57:07
Solutions to the Equation for Surface Depletion of a Gaussian Plume = v. C(x,y,z.), at a given point in computed as the deposition velocity v. times the pollutant concentration, C(x,y,z.), at a particular reference height z. ; however, in Horst’s model C(x,y,z) is the concentration due to the initial, unabsorbed plume minus the sum of concentration deficits due to