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

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Measuring Denitrification in Soils Using 15N TechniquesN2 (Balderston et al., 1976; Yoshinari and Knowles, 1976). The C.H. inhibition method made the study of denitrification accessible to many more scientists, as shown by the explosive increase in the number of articles about denitrification published since the introduction of the C.H. blockage techniq
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Combined Use of the Acetylene Inhibition Technique and Microsensors for Quantification of Denitrific79), 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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Book 1990trial 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
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Bio-Inorganic Aspects of Denitrification: Structures and Reactions of NxOy Compounds and Their Interl., 1987; Cole and Ferguson, 1988; Zehnder, 1988). Nitrogen is an essential constituent of many biomolecules which are important for life, e.g. amino acids, proteins, or DNA. In the process of nitrogen fixation dinitrogen is reduced to ammonia. This reaction is catalyzed by nitrogenase, a complex mu
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Physiology, Biochemistry and Genetics of Nitrate Dissimilation to Ammoniaial NO. reduction. In fact, the rapid, dissimilatory reduction to NH. by fermentative bacteria was documented many years ago (see, for example, Woods, 1938). As the limited literature on NO. dissimilation to NH. published before 1988 has recently been reviewed extensively (Cole, 1988; 1989), this ar
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Role of Environmental Factors in Regulating Nitrate Respiration in Intertidal Sedimentse case of respiratory metabolism, or indirectly as a consequence of fermentation. Oxidants used in respiratory metabolism include O., NO. and NO., manganese and ferric oxides, SO. and CO.. Organic matter decomposition within sediments results in the depletion of these oxidants. As a consequence micr
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