Titlebook: Chemistry of Multiphase Atmospheric Systems; Wolfgang Jaeschke Conference proceedings 1986 Springer-Verlag Berlin Heidelberg 1986 Systems.

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Ambient Radical Concentrations in the Presence of Airborne Liquid Waterto oxidize NO and CO to NO. and CO.. The NO. produced is measured by luminol chemiluminescence, based on the gas-surface reaction of NO. with a pH 12, 3 mM aqueous luminol solution. NO. produced from sources other than the chain reaction is measured by substitution of N. for CO one-half of the time.

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Photochemistry of the Atmospheric Aqueous Phaseent box model. Both scavenging of ambient acidic aerosols and gases as well as aqueous-phase chemical reactions within droplets are found to be important sources of acidity to cloud water and can lead to pH levels in cloudwater in the remote marine atmosphere well below 5.6. The major sources of aci

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0258-1256 ge in the field of atmospheric chemistry. In general the chemistry of atmospheric trace constituents is governed by the oxygen content of the atmosphere. Upon entering the atmosphere in a more or less reduced state, trace substances are oxidized via various pathways and the generated products are of

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,States of?the?Electromagnetic Field I,es. Vertical and meridional distributions of C. to C. hydrocarbons are presented which underline their importance at the midlatitudes of the northern hemisphere. An attempt is made to quantify the global emissions of individual light nonmethane hydrocarbons, and the various sources of C. – C. hydrocarbons are briefly discussed.

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Multiphase Atmospheric Chemistry applicable in the three phases of Multiphase Atmospheric Systems (MAS) are briefly discussed. In a final part some experiments and theoretical considerations with respect to the removal of SO. in MAS are discribed. The investigations were performed in a dynamic flow reactor, where multiphase systems relevant to the atmosphere could be simulated.