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Virtanen, Artturi I. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
The origin of nitrogen oxides in the atmosphere is discussed. Evidently only a small proportion of the nitrate- and nitrite-nitrogen found in the precipitation is formed through electric discharges from molecular nitrogen, photochemical nitrogen fixation being probably of greater importance. Formation of nitrate nitrogen through atmospheric oxidation of nitrous oxide (N2O) evaporating from the soil is also considered likely. Determination of nitrogen compounds at different altitudes is indispensable for gaining information of the N2-fixation in the atmosphere and, in general, of the origin of nitrogen oxides and their decomposition. International co-operation is needed for this as well as for the quantitative determination of the nitrogen compounds removed from the soil by leaching and brought by waters into the seas.DOI: 10.1111/j.2153-3490.1952.tb01016.x
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    • ANGSTROMA,., and HOGBERGL,., 1952; On the content of nitrogen (NH,-N, and NO,-N) in atmospheric Precipitation. Trllrrs 4, pp. 31-42.
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    • FINNELLH, . H., and HOUGHTONH,. W., 1932: Nitrogen content of rain water. Panhandle Bull. 34, pp. 3-8.
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    • RUSSELE,. J. and RICHARDSE,. H., 1919: The amount and composition of rain falling at Rothanisted. J . Agr. Sci. 9, pp. 309-337.
    • SCHARREKR.,, and FAST,H., 1952: Untersuchungen uber die dem Boden durch die Niederschlige zugefiihrten Pflanzennahrstoffe. Z . I'j7anzenern;ihr. Ditrigirng 11. Bodenkunde 55 (IOO), pp. 97-106.
    • VIRTANENA,. I., 1952: Attnospharischer Stickstoff als Aufrechterhalter des Lebens. Angeui. Clirrnie (in press).
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