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氮同位素效应可用于诊断废水厌氧氨氧化系统中的 N 转化。

Nitrogen isotope effects can be used to diagnose N transformations in wastewater anammox systems.

机构信息

Aquatic and Isotope Biogeochemistry, Department of Environmental Sciences, University of Basel, Basel, 4056, Switzerland.

Eawag, Swiss Federal Institute for Aquatic Science and Technology, Dübendorf, 8600, Switzerland.

出版信息

Sci Rep. 2021 Apr 12;11(1):7850. doi: 10.1038/s41598-021-87184-0.

Abstract

Anaerobic ammonium oxidation (anammox) plays an important role in aquatic systems as a sink of bioavailable nitrogen (N), and in engineered processes by removing ammonium from wastewater. The isotope effects anammox imparts in the N isotope signatures (N/N) of ammonium, nitrite, and nitrate can be used to estimate its role in environmental settings, to describe physiological and ecological variations in the anammox process, and possibly to optimize anammox-based wastewater treatment. We measured the stable N-isotope composition of ammonium, nitrite, and nitrate in wastewater cultivations of anammox bacteria. We find that the N isotope enrichment factor ε for the reduction of nitrite to N is consistent across all experimental conditions (13.5‰ ± 3.7‰), suggesting it reflects the composition of the anammox bacteria community. Values of ε for the oxidation of nitrite to nitrate (inverse isotope effect, - 16 to - 43‰) and for the reduction of ammonium to N (normal isotope effect, 19-32‰) are more variable, and likely controlled by experimental conditions. We argue that the variations in the isotope effects can be tied to the metabolism and physiology of anammox bacteria, and that the broad range of isotope effects observed for anammox introduces complications for analyzing N-isotope mass balances in natural systems.

摘要

厌氧氨氧化(anammox)作为生物可利用氮(N)的汇,在水生系统中起着重要作用,并在工程化过程中通过从废水中去除氨来发挥作用。anammox 在铵、亚硝酸盐和硝酸盐的 N 同位素特征(N/N)中赋予的同位素效应可用于估计其在环境中的作用,描述 anammox 过程中的生理和生态变化,并可能优化基于 anammox 的废水处理。我们测量了厌氧氨氧化细菌废水培养物中铵、亚硝酸盐和硝酸盐的稳定 N 同位素组成。我们发现,在所有实验条件下,亚硝酸盐还原为 N 的 N 同位素富集因子 ε 都是一致的(13.5‰±3.7‰),这表明它反映了厌氧氨氧化细菌群落的组成。亚硝酸盐氧化为硝酸盐的 ε 值(反同位素效应,-16 至-43‰)和铵还原为 N 的 ε 值(正常同位素效应,19-32‰)的变化更大,可能受实验条件的控制。我们认为,同位素效应的变化可以与厌氧氨氧化细菌的新陈代谢和生理学联系起来,并且观察到的厌氧氨氧化的同位素效应范围很广,这给分析自然系统中的 N 同位素质量平衡带来了复杂性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c10a/8041819/a0de66c16948/41598_2021_87184_Fig1_HTML.jpg

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