Titlebook: Gaseous Loss of Nitrogen from Plant-Soil Systems; J. R. Freney,J. R. Simpson Book 1983 Springer Science+Business Media Dordrecht 1983 evol

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Human carcinogenicity of inorganic arsenic,umerous laboratory studies have provided useful information on the factors affecting denitrification in soils but these findings cannot be used to predict the extent of denitrification in the field. In recent years, increased interest in the efficiency of nitrogen (N) use in agriculture and the impa

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The Physiology of Arsenic in Rice,direct field measurements have been made of the exchanges of nitrogenous gases between soils, plants and the atmosphere. Methods of three general kinds have been employed: those using diffusion theory to calculate gas transport in the soil profile; enclosure methods in which the flux density of the

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Arsenic Contamination in the Environmentase the efficiency of N added to the system through biological and industrial fixation. Of the many pathways of loss, those from plants have in the main been ignored, or were thought to be extremely low (Allison 1955, 1966). Recently, however, Wetselaar and Farquhar (1980) have reviewed data that su

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https://doi.org/10.1007/978-981-13-6721-2 land. A short review of this topic was included recently in an article published by Terman (1979). The purpose of the present review is to deal mainly with NH. volatilization losses from manures and sewage sludges as affected by climatic and soil factors. Information on NH. volatilization from othe

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Arsenic Health Risk Assessment,nd Stobbs 1981, Woodmansee .. 1981, Steele 1982a). The cycle involves inputs of N from the atmosphere via biological or industrial fixation, and also mineralization of organic N in the soil, plant absorption of mineral N, consumption of plant material by grazers, return of excreta, decay of ungrazed

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Arsenic in Latin America: Part I,lizer N production has increased from 3.6 × 10. t in 1970 to an estimated 18 × 10. t in 1982/83, of which 85% will be urea (Stangel 1979). Expanded use of N fertilizer is being combined with fertilizer-responsive rice varieties and increased areas under irrigation in an all-out effort to produce eno

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D. Kirk Nordstrom,Donald G. Archer passive role, acting only as a medium for transport, e.g. for ammonia (NH.) release and uptake, whereas in other cases one or more chemical transformations take place in the atmosphere before each cycling N atom returns to a terrestrial ecosystem.

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https://doi.org/10.1007/978-3-662-42360-8s, and plant leaves; N., N.O, and NO evolution during biological denitrification; N., N.O, NO, and NO. evolution during abiological denitrification (chemodenitrification); N.O evolution during nitrification; and NH. and NO. (N oxides) release through combustion. The physical and biological processes

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