Modeling NOx reduction competition to identify thresholds of inorganic nitrogen retention and loss in aquatic ecosystems
编号:773 访问权限:仅限参会人 更新:2024-12-30 19:46:34 浏览:204次 口头报告

报告开始:2025年01月14日 11:25(Asia/Shanghai)

报告时间:15min

所在会场:[S3] Session 3-The Nitrogen Cycle Towards a Sustainable Ocean: From Microbes to Global Biogeochemistry [S3-1] The Nitrogen Cycle Towards a Sustainable Ocean: From Microbes to Global Biogeochemistry

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摘要
Eutrophication and the disturbances which promote eutrophying condition may create environments favorable to the retention of nutrients, such as nitrogen (N), thus creating a positive feedback loop. This positive feedback loop is driven by 1) anoxia (due to oxygen consumption by bacteria) and 2) the increased availability of electron donors to heterotrophic microbial communities. The resulting alterations to the biogeochemical landscape dictate the degree to which bioavailable N is retained in an ecosystem, as NH4, rather than converted to N2O or N2. To develop a framework for understanding the threshold at which competing microbial metabolisms will drive a net loss versus a net gain of inorganic N and provide a clear mechanism to explain the aforementioned positive feedback loop, we have used redox-constrained parameters (which may be more broadly applicable than species or location-specific parameters) to develop a microbial population model that mechanistically resolves the competition of dissimilatory nitrate reduction to ammonium (DNRA), an inorganic N retention pathway, versus denitrification and anaerobic ammonium oxidation (anammox), inorganic N loss pathways. These metabolisms compete for electron acceptors (NO2) under varying electron donor (organic matter, OM) loading intensities. Our model demonstrates how we can understand the known response of DNRA and denitrification to varying OM and nitrite supply rate ratios from the underlying energetics, enabling a trait-based model. Therefore, our framework aids in improving our understanding of N cycling in environments where microbial community dynamics are largely unknown. In our model, net loss (i.e., N2 production from denitrification) does not balance net production (i.e., NH4 production from DNRA) when denitrification and DNRA communities reach coexistence or even when the DNRA functional group becomes the most abundant biomass. Instead, positive inorganic N production occurs when DNRA is able to reduce ~45% of available NO2.
 
关键词
DNRA, denitrification, anammox, nitrite, organic matter
报告人
Jemma Fadum
Postdoctor Carnegie Science

稿件作者
Jemma Fadum Carnegie Science
Emily Zakem Carnegie Science
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重要日期
  • 会议日期

    01月13日

    2025

    01月17日

    2025

  • 09月27日 2024

    初稿截稿日期

  • 01月17日 2025

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
承办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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