Analysis of Nitrification in Agricultural Soil and Improvement of Nitrogen Circulation with Autotrophic Ammonia-Oxidizing Bacteria

Accumulations of inorganic nitrogen (NH 4 + , NO 2 − , and NO 3 − ) were analyzed to evaluate the nitrogen circulation activity in 76 agricultural soils. Accumulation of NH 4 + was observed, and the reaction of NH 4 +  → NO 2 − appeared to be slower than that of NO 2 −  → NO 3 − in agricultural soil...

Full description

Saved in:
Bibliographic Details
Published inApplied biochemistry and biotechnology Vol. 169; no. 3; pp. 795 - 809
Main Authors Matsuno, Toshihide, Horii, Sachie, Sato, Takanobu, Matsumiya, Yoshiki, Kubo, Motoki
Format Journal Article
LanguageEnglish
Published New York Springer-Verlag 01.02.2013
Springer
Springer Nature B.V
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Accumulations of inorganic nitrogen (NH 4 + , NO 2 − , and NO 3 − ) were analyzed to evaluate the nitrogen circulation activity in 76 agricultural soils. Accumulation of NH 4 + was observed, and the reaction of NH 4 +  → NO 2 − appeared to be slower than that of NO 2 −  → NO 3 − in agricultural soil. Two autotrophic and five heterotrophic ammonia-oxidizing bacteria (AOB) were isolated and identified from the soils, and the ammonia-oxidizing activities of the autotrophic AOB were 1.0 × 10 3 –1.0 × 10 6 times higher than those of heterotrophic AOB. The relationship between AOB number, soil bacterial number, and ammonia-oxidizing activity was investigated with 30 agricultural soils. The ratio of autotrophic AOB number was 0.00032–0.26 % of the total soil bacterial number. The soil samples rich in autotrophic AOB (>1.0 × 10 4 cells/g soil) had a high nitrogen circulation activity, and additionally, the nitrogen circulation in the agricultural soil was improved by controlling the autotrophic AOBs.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0273-2289
1559-0291
DOI:10.1007/s12010-012-0029-6