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Titlebook: Denitrification in Soil and Sediment; Niels Peter Revsbech,Jan S?rensen Book 1990 Springer Science+Business Media New York 1990 biochemist

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發(fā)表于 2025-3-21 17:38:44 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Denitrification in Soil and Sediment
編輯Niels Peter Revsbech,Jan S?rensen
視頻videohttp://file.papertrans.cn/266/265538/265538.mp4
叢書名稱F.E.M.S. Symposium Series
圖書封面Titlebook: Denitrification in Soil and Sediment;  Niels Peter Revsbech,Jan S?rensen Book 1990 Springer Science+Business Media New York 1990 biochemist
描述The formation of atmospheric nitrogen gas by denitrifying bacteria may represent a significant nutrient sink in natural ecosystems. The rate of denitrification has often been difficult to measure in situ, however, and new methodologies should stimulate research on distribution of activity in space and time. The load of fertilizer nitrogen in modem agriculture has led to increasing nutrient reservoirs in recipient subsoils, aquifers, inland waters and coastal seas. By its conversion of nitrate to atmospheric nitrogen, bacterial denitrification is the only biological process to potentially reduce the impact of increasing nutrient loadings by fertilizer nitrogen in the environment. As part of a scientific program set up by the Danish Ministry of Environment to study environment cycling of nitrogen, phosphorous and organic matter (NPO program) in the light of agricultural, domestic and industrial activities, a symposium on DENITRIFICATION IN SOIL AND SEDIMENT was held at the University of Aarhus, Denmark from 6-9 June 19i9. On the basis of lectures given at the symposium, this book contains a number of invited contributions on the regulation of denitrification activity (control of enzy
出版日期Book 1990
關(guān)鍵詞biochemistry; biofilm; cyclin; development; ecosystem; environment; enzymes; metabolism; nitrogen; nutrient c
版次1
doihttps://doi.org/10.1007/978-1-4757-9969-9
isbn_softcover978-1-4757-9971-2
isbn_ebook978-1-4757-9969-9
copyrightSpringer Science+Business Media New York 1990
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Distributed Systems for System Architectsogical groups of microorganisms thus creating more reduced conditions (Kaplan, 1979). In the absence of 0. many aerobic and facultatively anaerobic bacteria are able to carry out NO. respiration using NO. as terminal electron acceptor (Payne, 1973; Herbert, 1982). In NO. respiration the end-product(
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https://doi.org/10.1007/978-0-387-35570-279), but the highest resolution by such an approach is still rather on a centimeter than on a millimeter scale while denitrifying microenvironments such as biofilms often have dimensions of less than 1 mm. The recent introduction of a microsensor for simultaneous detection of O. and N.O has now made
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Bio-Inorganic Aspects of Denitrification: Structures and Reactions of NxOy Compounds and Their Intertion of reduced (-3) valency nitrogen species may play an important role in the biological formation of carcinogenic nitrosamines (Zehnder, 1988). Model studies suggest the hypothesis that the formation of these carcinogenic compounds may involve metal centres capable of catalysing both oxidation of
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Physiological and Ecological Aspects of Aerobic Denitrification, a Link with Heterotrophic Nitrifica denitrification by some of them is inhibited by relatively low amounts of oxygen (e.g. . X; Melberg et al., 1980) while others continue to denitrify even at air saturation (e.g. .). It is not unlikely that, as with electron donors, the environmental conditions and nutrient supplies determine whethe
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