Anaerobic ammonium oxidation in agricultural soils-synthesis and prospective
Denitrification is considered as the dominant nitrogen (N) removing pathway, however, anaerobic oxidation of ammonium (anammox) also plays a significant part in N loss in agricultural ecosystems. Large N inputs into agricultural soils may stimulate the growth of anammox bacteria, resulting in high a...
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Published in | Environmental pollution (1987) Vol. 244; pp. 127 - 134 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
England
Elsevier Ltd
01.01.2019
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Abstract | Denitrification is considered as the dominant nitrogen (N) removing pathway, however, anaerobic oxidation of ammonium (anammox) also plays a significant part in N loss in agricultural ecosystems. Large N inputs into agricultural soils may stimulate the growth of anammox bacteria, resulting in high activity and diversity of anammox bacteria and subsequent more N loss. In some specific niches, like oxic-anoxic interface, three processes, nitrification, anammox and denitrification couple with each other, and significant anammox reaction could be observed. Soil parameters like pH, dissolved oxygen, salinity, oxidation-reduction potential (ORP), and substrate concentrations impact the anammox process. Here we summarize the current knowledge on anammox activity and contribution to N loss, abundance and diversity of anammox bacteria, factors affecting anammox, and the relationship between anammox and other N loss pathways in agricultural soils. We propose that more investigations are required for (1) the role of anammox to N loss with different agricultural management strategies; (2) microscale research on the coupling of nitrification-anammox-denitrification, that might be a very complex process but ideal model for further studies responsible for N cycling in terrestrial ecosystems; and (3) new methods to estimate differential contributions of anammox, codenitrification and denitrification in total N loss in agricultural ecosystems. New research will provide much needed information to quantify the contribution of anammox in N loss from soils at landscape, ecosystem and global scales.
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•About 5–10% of the applied fertilizers was lost by anammox in agricultural soils.•Terrestrial soils possess a high diversity and abundance of anammox bacteria.•The oxic/anoxic interfaces in the agricultural soil are hotspots for anammox.•The redox gradient area is the main coupling nitrification-anammox-denitrification.•Anammox, codenitrification and denitrification need further estimation. |
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AbstractList | Denitrification is considered as the dominant nitrogen (N) removing pathway, however, anaerobic oxidation of ammonium (anammox) also plays a significant part in N loss in agricultural ecosystems. Large N inputs into agricultural soils may stimulate the growth of anammox bacteria, resulting in high activity and diversity of anammox bacteria and subsequent more N loss. In some specific niches, like oxic-anoxic interface, three processes, nitrification, anammox and denitrification couple with each other, and significant anammox reaction could be observed. Soil parameters like pH, dissolved oxygen, salinity, oxidation-reduction potential (ORP), and substrate concentrations impact the anammox process. Here we summarize the current knowledge on anammox activity and contribution to N loss, abundance and diversity of anammox bacteria, factors affecting anammox, and the relationship between anammox and other N loss pathways in agricultural soils. We propose that more investigations are required for (1) the role of anammox to N loss with different agricultural management strategies; (2) microscale research on the coupling of nitrification-anammox-denitrification, that might be a very complex process but ideal model for further studies responsible for N cycling in terrestrial ecosystems; and (3) new methods to estimate differential contributions of anammox, codenitrification and denitrification in total N loss in agricultural ecosystems. New research will provide much needed information to quantify the contribution of anammox in N loss from soils at landscape, ecosystem and global scales. Denitrification is considered as the dominant nitrogen (N) removing pathway, however, anaerobic oxidation of ammonium (anammox) also plays a significant part in N loss in agricultural ecosystems. Large N inputs into agricultural soils may stimulate the growth of anammox bacteria, resulting in high activity and diversity of anammox bacteria and subsequent more N loss. In some specific niches, like oxic-anoxic interface, three processes, nitrification, anammox and denitrification couple with each other, and significant anammox reaction could be observed. Soil parameters like pH, dissolved oxygen, salinity, oxidation-reduction potential (ORP), and substrate concentrations impact the anammox process. Here we summarize the current knowledge on anammox activity and contribution to N loss, abundance and diversity of anammox bacteria, factors affecting anammox, and the relationship between anammox and other N loss pathways in agricultural soils. We propose that more investigations are required for (1) the role of anammox to N loss with different agricultural management strategies; (2) microscale research on the coupling of nitrification-anammox-denitrification, that might be a very complex process but ideal model for further studies responsible for N cycling in terrestrial ecosystems; and (3) new methods to estimate differential contributions of anammox, codenitrification and denitrification in total N loss in agricultural ecosystems. New research will provide much needed information to quantify the contribution of anammox in N loss from soils at landscape, ecosystem and global scales. [Display omitted] •About 5–10% of the applied fertilizers was lost by anammox in agricultural soils.•Terrestrial soils possess a high diversity and abundance of anammox bacteria.•The oxic/anoxic interfaces in the agricultural soil are hotspots for anammox.•The redox gradient area is the main coupling nitrification-anammox-denitrification.•Anammox, codenitrification and denitrification need further estimation. |
Author | Zhu, Yong-Guan Zhu, Gui-Bing Nie, San'an Singh, Brajesh |
Author_xml | – sequence: 1 givenname: San'an surname: Nie fullname: Nie, San'an organization: College of Life Sciences, Fujian Agriculture and Forest University, Fuzhou, 350002, China – sequence: 2 givenname: Gui-Bing surname: Zhu fullname: Zhu, Gui-Bing organization: Key Laboratory of Drinking Water Science and Technology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China – sequence: 3 givenname: Brajesh surname: Singh fullname: Singh, Brajesh organization: Hawkesbury Institute for the Environment, Western Sydney University, Locked Bag 1797, Penrith South, NSW, 2751, Australia – sequence: 4 givenname: Yong-Guan surname: Zhu fullname: Zhu, Yong-Guan email: ygzhu@iue.ac.cn organization: Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China |
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Keywords | Rhizosphere Anammox N loss Agricultural soils Oxic/anoxic interface |
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SubjectTerms | Agricultural soils Agriculture Ammonium Compounds - chemistry Anaerobiosis Anammox Denitrification N loss Oxic/anoxic interface Oxidation-Reduction Rhizosphere Soil Microbiology |
Title | Anaerobic ammonium oxidation in agricultural soils-synthesis and prospective |
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