Simultaneous effects of increasing levels of glucose and oxygen partial pressures on denitrification and dissimilatory nitrate reduction to ammonium in repacked soil cores

被引:124
作者
Fazzolari, E [1 ]
Nicolardot, B [1 ]
Germon, JC [1 ]
机构
[1] INRA, CMSE, Lab microbiol Sols, F-21034 Dijon, France
关键词
denitrification; dissimilatory nitrate reduction to ammonium (DNRA); oxygen; carbon; glucose; regulation; repacked soil core;
D O I
10.1016/S1164-5563(99)80006-5
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Dissimilatory nitrate reduction to ammonium (DNRA) and its importance in comparison to denitrification were studied in soil samples artificially repacked to control water potential and porosity, and incubated for 72 h. Labelled nitrate (100 mg N.kg(-1) dry soil, 21.8 % N-15 in excess) and increasing levels of glucose-C (250, 500 and 1000 mg glucose-C.kg(-1) dry soil) were initially added to the soil samples to obtain increasing glucose-C/nitrate-N ratios of 2.5, 5 and 10, which were then subjected to different O-2 partial pressures (0, 0.5, 1.0 and 2.0 % (v/v)). The results confirmed the good reproducibility of the experimental conditions using this method. Denitrification, rather than DNRA, was the dominant process in all the treatments developed during this experiment: N2O production in the presence of acetylene varied from 4.9 (glucose-C/nitrate-N = 2.5; 2 % O-2) to 103.6 % (glucoseC/nitrate-N = 2.5; 0 % O-2) of the original nitrate whereas DNRA varied from 1.8 (glucose-C/nitrate-N = 2.5; 2.0 % O-2) to 24.6 % (glucose-C/nitrate-N = 10; 1.0 % O-2) of the original nitrate. This work demonstrated that under these conditions, DNRA activity was less sensitive than denitrification to an inhibitory effect by O-2 and reinforced the idea that carbon is the main driving factor regulating nitrate distribution between denitrification and DNRA. (C) Elsevier, Paris.
引用
收藏
页码:47 / 52
页数:6
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