2002
DOI: 10.1007/s00253-002-1059-8
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Oxygen-limited autotrophic nitrification/denitrification by ammonia oxidisers enables upward motion towards more favourable conditions

Abstract: The hypothesis is formulated that in case of oxygen limitation in the sediment, nitrifiers switch from nitrification to oxygen-limited autotrophic nitrification-denitrification (OLAND) in order to survive and maintain activity. During OLAND, ammonium is oxidised using nitrite as e-acceptor to form dinitrogen gas. As an additional advantage they benefit from the gaseous N(2) formed as a means of transport. In this way, the nitrifiers can move out of the sediment and rise through the water column towards more fa… Show more

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Cited by 32 publications
(2 citation statements)
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“…High concentrations of NO 2 − were detected in A and C soil horizon. In the first horizon, the rate of nitritation is faster than nitratation, resulting in the accumulation of NO 2 − [23,24]. NO 3 − increases with depth and, together with NO 2 − , represents the dominant species of N in the deepest soil horizon (Figure 3).…”
Section: Nitrogen Species Distribution Within the Soil Zonementioning
confidence: 99%
See 1 more Smart Citation
“…High concentrations of NO 2 − were detected in A and C soil horizon. In the first horizon, the rate of nitritation is faster than nitratation, resulting in the accumulation of NO 2 − [23,24]. NO 3 − increases with depth and, together with NO 2 − , represents the dominant species of N in the deepest soil horizon (Figure 3).…”
Section: Nitrogen Species Distribution Within the Soil Zonementioning
confidence: 99%
“…When the rate of nitritation is faster than nitratation, NO 2 − accumulates. When nitratation takes place more rapidly, only a small amount of NO 2 − is produced [23,24]. The presence of NH 4…”
Section: Introductionmentioning
confidence: 99%