Titlebook: Denitrification in the Nitrogen Cycle; Han L. Golterman Book 1985 Springer Science+Business Media New York 1985 biology.ecology.ecosystem.

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Marine Denitrificationoering, 1967; Ryther and Dunstan, 1971; Walsh and Dugdale, 1971; McCarthy, 1977; Eppley et al., 1979). For this reason its biogeochemical cycle has, for many years, been extensively studied by marine scientists. The majority of the nitrogen required for plant growth in the marine environment is supp

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Denitrification by Methanotrophic / Methylotrophic Bacterial Associations in Aquatic Environments in both natural and technical aquatic environments. Hypotheses concerning the particular questions of denitrification by such bacterial associations in the presence of oxygen and with methane as the sole supplied carbon substrate are proposed. Experimental results that seek to further elucidate den

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Genetics of Denitrification in , and ,ted so far in not being able to grow with N.O as sole oxidant severely limit its utility for investigations on the later steps of the denitrification pathway. . grows well on exogenous N.O as sole oxidant, but its use in physiological genetic studies required the development of procedures for geneti

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Denitrification Loss from Managed Grasslandsink for atmospheric N.O. Only 1.6% of the fertilizer applied was lost as N.O, this gas comprising 21% of the total denitrification loss. Up to 55% of the annual denitrification loss occured following application of N in late winter/early spring. This loss was eliminated by applying N in an ammonium

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https://doi.org/10.1007/978-1-4615-4489-0sink for atmospheric N.O. Only 1.6% of the fertilizer applied was lost as N.O, this gas comprising 21% of the total denitrification loss. Up to 55% of the annual denitrification loss occured following application of N in late winter/early spring. This loss was eliminated by applying N in an ammonium