Potential rates of ammonium oxidation, nitrite oxidation, nitrate reduction and denitrification in the young barley rhizosphere

Potential activities (enzyme contents) of ammonium (NH 4 +) oxidizing, nitrite (NO 2 −) oxidizing, nitrate (NO 3 −) reducing and denitrifying bacteria were measured in bulk and rhizosphere soil obtained from young barley plants in the field. The activities as well as pools of inorganic N (NH 4 +, NO...

Full description

Saved in:
Bibliographic Details
Published inSoil biology & biochemistry Vol. 28; no. 1; pp. 47 - 54
Main Authors Højberg, Ole, Binnerup, Svend Jørgen, Sørensen, Jan
Format Journal Article
LanguageEnglish
Published Oxford Elsevier Ltd 1996
New York, NY Elsevier Science
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Potential activities (enzyme contents) of ammonium (NH 4 +) oxidizing, nitrite (NO 2 −) oxidizing, nitrate (NO 3 −) reducing and denitrifying bacteria were measured in bulk and rhizosphere soil obtained from young barley plants in the field. The activities as well as pools of inorganic N (NH 4 +, NO 2 − and NO 3 −) were followed for 3 weeks in the beginning of the growth season (May–June). During the 3 weeks two separate periods of rain gave dramatic changes in soil water content. A rainfall in the beginning of the sampling period, resulting in a short-term wetting of the soil, stimulated the potential nitrification in the rhizosphere. On the other hand, potential denitrification only responded positively to the second, longer wetting of the soil. The potential activities were not affected by changes in the pools of inorganic N. As judged from the potential activities (enzyme contents), both groups of nitrifiers, NO 3 − reducer, and denitrifiers seemed most abundant in the rhizosphere, where the activities were from 1.5 to 2.5 times higher than in the bulk soil. NH 4 + oxidizers and NO 2 − oxidizers showed a distinct and similar trend throughout the sampling period, which was also the case for NO 3 − reducers and denitrifiers. The results indicate that potential activities (enzyme contents) in the four bacterial groups were less dependent on their inorganic N substrates in the bulk and rhizosphere soils, but showed distinct and different responses to duration of soil wetting after rainfall.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0038-0717
1879-3428
DOI:10.1016/0038-0717(95)00119-0