Research Progress on Hydroxylamine, An Intermediate in the Nitrogen Cycle
Received date: 2023-03-16
Revised date: 2023-05-12
Online published: 2023-07-19
Supported by
the National Natural Science Foundation of China “Source and flux of N2O in the euphotic zone of the Northwestern Pacific”(92058204);Creative Research Groups of the National Natural Science Foundation of China “Nitrogen cycle under global change”(41721005)
Hydroxylamine (NH2OH) is one of the most active trace forms of nitrogen in oceans, and it is the key intermediate product of many nitrogen cycle processes, such as ammonia oxidation, dissimilatory nitrate reduction to ammonium and anaerobic ammonia oxidation. Therefore, it is an important component of the marine nitrogen cycle network framework. Concurrently, NH2OH is an important precursor of the greenhouse gas nitrous oxide (N2O), closely related to the production and release of marine N2O. Accordingly, a systematic understanding of the source and sink, spatiotemporal variations, and regulatory mechanisms of NH2OH in the ocean is essential to understand the oceanic nitrogen cycle and climate effects. However, the nanomolar concentration of NH2OH in the ocean and its complex and active migration and transformation processes render the oceanographic community’s understanding of NH2OH unclear. Current research on marine NH2OH is systematically reviewed, focusing on the potential source and sink processes of NH2OH, the determination methods of NH2OH, the possible contribution of NH2OH to marine N2O, and the distribution characteristics and potential impact factors of NH2OH in the ocean. Finally, the problems and difficulties in determining NH2OH and the possible mechanisms affecting its distribution are summarized, and suggestions and prospects for future research on marine NH2OH are discussed.
Key words： Marine nitrogen cycle; Hydroxylamine; Nitrous oxide
Senwei TONG , Jinyu YANG , Xianhui WAN , Qingqing NIU , Shuh-Ji KAO . Research Progress on Hydroxylamine, An Intermediate in the Nitrogen Cycle[J]. Advances in Earth Science, 2023 , 38(7) : 688 -702 . DOI: 10.11867/j.issn.1001-8166.2023.033
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