2022
DOI: 10.1016/j.soilbio.2022.108611
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Heterotrophic nitrification – An eternal mystery in the nitrogen cycle

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Cited by 87 publications
(41 citation statements)
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“…Moreover, we found soil properties, especially the SOM were the major factor that influenced bacterial community (Tables 1, 2 and 4). That may be because SOM was an important nutrient resource for soil microorganisms [50], especially the heterotrophic microorganisms are sensitive to SOM dynamics [51,52]. As well, in the present study, we found the key biomarkers of gullies such as the Rhizobiales, were positively correlated with SOM (Figure 3).…”
Section: Nvr Influenced the Microbial Community In Gullies By The Acc...supporting
confidence: 75%
“…Moreover, we found soil properties, especially the SOM were the major factor that influenced bacterial community (Tables 1, 2 and 4). That may be because SOM was an important nutrient resource for soil microorganisms [50], especially the heterotrophic microorganisms are sensitive to SOM dynamics [51,52]. As well, in the present study, we found the key biomarkers of gullies such as the Rhizobiales, were positively correlated with SOM (Figure 3).…”
Section: Nvr Influenced the Microbial Community In Gullies By The Acc...supporting
confidence: 75%
“…Microbial oxidation of NH 4 + to NO 3 – via nitrite (NO 2 – ) is termed as nitrification ( Barth et al, 2019 ) during which autotrophic nitrifiers can gain their energy for their routine activities ( Figure 4 ). Meanwhile, some heterotrophic nitrifiers can process the conversion of inorganic and organic N to NO 3 – or NO 2 – with no acquired energy, and this process is termed as heterotrophic nitrification ( Martikainen, 2022 ). Here, the discussion is only about autotrophic nitrification due to its large contribution to the N cycle relative to heterotrophic nitrification.…”
Section: Pathways Of N Cycle In Rice-based Systemsmentioning
confidence: 99%
“…Biological oxidation of NH 4 + ions to NO 3 – via NO 2 – stipulates the translocation of N through the negatively charged soil particles, and hence, this oxidative conversion determines the actual N fate in the soil. Generally, nitrification in rice soil is mediated in two ways, as described in the previous section of N pathways, autotrophic nitrification during which the autotrophic nitrifiers acquire their required energy for their metabolic processes ( Jung et al, 2011 ), and heterotrophic nitrification during which heterotrophic nitrifies convert the inorganic N (NH 4 + ) and organic N to NO 3 – via intermediate NO 2 – without acquiring any of their required energy ( Zhang et al, 2012 ; Hayatsu et al, 2021 ; Martikainen, 2022 ). The most likely form of N to translocate from soil solution to plant roots via mass flow is NO 3 – rather than NH 4 + , and if not readily taken up by the plant, it will cause leach down during flooding or be lost via denitrification during dry soil conditions.…”
Section: Toward Eco-efficient N Managementmentioning
confidence: 99%
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