Titlebook: Reactive Halogen Compounds in the Atmosphere; P. Fabian,Onkar N. Singh Book 1999 Springer-Verlag Berlin Heidelberg 1999 Air Pollution.CFC.

現(xiàn)實(shí)

Reactive Chlorine Compounds in the Atmosphere,oceans, rain, or by deposition. Chlorine-containing gases may be classified according to their lifetimes in the troposphere, which is often a reflection of their chemical reactivities. If the lifetime is less than about one year, the gases are considered to be “reactive”; if it is between 1-10 years

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Reactive Fluorine Compounds,ironment is expected to grow rapidly in the future. Their environmental fate and impact should thus be carefully assessed. Compounds of fluorine are covered by this chapter if they do not contain other halogens and exhibit at least some economic or environmental relevance. Here, these substances are

profligate

Iodine Compounds in the Atmosphere, CH.I, several other organic iodine compounds of biological origin, such as CH.I., CH.ClI and C.H.I have been detected in ocean water. Due to their low solubility the water can become super-saturated with iodocarbons causing a flux from the aqueous to the gas phase. Anthropogenic sources of iodine i

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Production, Sales and Emissions of Halocarbons from Industrial Sources, Chapter, data are presented on the production, sales and emission of chlorofluorocarbons, halons, hydrochlorofluorocarbons, hydrofluorocarbons, and the following chlorinated solvents: methyl chloroform, methylene chloride, tetrachlorethene and trichloroethene. Data available from the United Nations

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1867-979X ogen compounds and their interactions. It provides a review on the present knowledge of their properties, applications, sources, sinks as well as international regulations.978-3-662-14745-0978-3-540-69690-2Series ISSN 1867-979X Series E-ISSN 1616-864X

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1867-979X tesScientific evidence clearly shows that chlorine and bromine compounds, such as CFCs, released into the atmosphere are responsible for continuous and progressive global ozone losses superimposed by dramatic seasonal ozone depletions first observed over Antarctica, now occurring over Arctic regions