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Heterogeneous Catalysis in the Troposphere

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Abstract The sections in this article are Introduction The Atmosphere as a Global Catalytic and Photocatalytic Reactor Thermal Heterogeneous Catalytic Processes over Ice Particles, and Liquid and Solid Aerosols Hydrolytic Reactions Redox Reactions Acid‐Catalyzed Reactions of Organic Compounds over Aerosols Heterogeneous Photocatalytic Reactions in the Troposphere Role of Heterogeneous Photocatalytic Processes in the Global Chemistry of the Atmosphere Experimental Data on Photocatalytic Reactions of Atmospheric Components Photocatalytic Reactions of the Main Atmospheric Components over Semiconductor Oxides Photocatalytic Reactions of Trace Components of the Atmosphere over Semiconductor Oxides Photocatalysis over Compounds with Wide Band Gaps Photocatalysis by Dissolved Transition Metal Ions Photogenerated Catalysis Destructive Photoadsorption by Alkaline Earth Oxides Role of Thermal Absorption and Adsorption in Tropospheric Catalysis and Photocatalysis Conclusions
Title: Heterogeneous Catalysis in the Troposphere
Description:
Abstract The sections in this article are Introduction The Atmosphere as a Global Catalytic and Photocatalytic Reactor Thermal Heterogeneous Catalytic Processes over Ice Particles, and Liquid and Solid Aerosols Hydrolytic Reactions Redox Reactions Acid‐Catalyzed Reactions of Organic Compounds over Aerosols Heterogeneous Photocatalytic Reactions in the Troposphere Role of Heterogeneous Photocatalytic Processes in the Global Chemistry of the Atmosphere Experimental Data on Photocatalytic Reactions of Atmospheric Components Photocatalytic Reactions of the Main Atmospheric Components over Semiconductor Oxides Photocatalytic Reactions of Trace Components of the Atmosphere over Semiconductor Oxides Photocatalysis over Compounds with Wide Band Gaps Photocatalysis by Dissolved Transition Metal Ions Photogenerated Catalysis Destructive Photoadsorption by Alkaline Earth Oxides Role of Thermal Absorption and Adsorption in Tropospheric Catalysis and Photocatalysis Conclusions.

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