Environmental hazard assessment of chemicals and products. Part VI. Abiotic degradation in the troposphere.
The atmosphere constitutes an important sink for many volatile and semivolatile organic compounds (Part II). Even non-volatile compounds may enter the troposphere due to incomplete burning of fuel and industrial, agricultural and traffic-related processes. Depending on vapour pressure, temperature and content of aerosol particles, chemicals prefer the free gas phase, the surface of the particles, or both compartments. Polar compounds (low Henry-coefficient) may dissolve in cloud- and fog droplets. Clearly, the prefered compartment influences the dominant abiotic degradation path. In this paper, a survey is given about the distribution and degradation pathways of chemicals in the troposphere. In the free gas phase of the troposphere, the reaction with OH-radicals is the dominant degradation path. In addition, the reactions with ozone and nitrate-radicals, and direct photochemical reactions also play a role in abiotic degradation.
Klöpffer
W
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C.A.U. GmbH, Dreieich/Frankfurt am Main, Germany.
D000336:Aerosols; D000393:Air Pollutants / Q000032:analysis / Q000378:metabolism*; D006838:Hydrocarbons / Q000737:chemistry / Q000378:metabolism*; D007220:Industrial Waste; D009589:Nitrogen Oxides / Q000737:chemistry / Q000378:metabolism; D010126:Ozone / Q000737:chemistry / Q000378:metabolism; D010316:Particle Size; D010777:Photochemistry; D017382:Reactive Oxygen Species / Q000737:chemistry / Q000378:metabolism*; D018570:Risk Assessment; D014835:Volatilization
D000336:Aerosols; D000393:Air Pollutants; D006838:Hydrocarbons; D007220:Industrial Waste; D009589:Nitrogen Oxides; D017382:Reactive Oxygen Species; C031701:nitrogen trioxide; D010126:Ozone