Wetlands, carbon monoxide

Zuo Y, Jones RD (1997) Photochemistry of Natural Dissolved Organic Matter in Lake and Wetland Waters-Production of Carbon Monoxide, Wat. Res. 31, No. 4 850-858. [Pg.144]

Zuo Y. and Jones R. D. (1997) Photochemistry of natural dissolved organic matter in lake and wetland waters— production of carbon monoxide. Water Res. 31, 850-858. [Pg.2571]

Rich J. J. and King G. M. (1999) Carbon monoxide consumption and production by wetland peats. FEMS Microbiol. Ecol. 28, 215-224. [Pg.4279]

In the troposphere, the production of ozone results from the day-time oxidation of methane, nonmethane hydrocarbons, and carbon monoxide in the presence of nitrogen oxides. Under natural conditions, methane, produced in oxygen-deficient environments, is released primarily by wetlands, lakes, and rivers. Nonmethane hydrocarbons, such as isoprene and terpenes, are emitted by various types of trees. Nitric oxide is released by soils as a result of microbial activity and is produced in the atmosphere by lightning in thunderstorm systems. [Pg.32]

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