School of Geographic Sciences, East China Normal University, Shanghai 200241, China.
Key Laboratory of Geographic Information Science (Ministry of Education), East China Normal University, Shanghai 200241, China.
Environ Sci Technol. 2022 May 3;56(9):5939-5949. doi: 10.1021/acs.est.2c00692. Epub 2022 Apr 24.
Acidification of estuarine and coastal waters is anticipated to influence nitrogen (N) removal processes, which are critical pathways for eliminating excess N from these ecosystems. We found that denitrification rates decreased significantly under acidified conditions ( < 0.05), which reduced by 41-53% in estuarine and coastal sediments under an approximately 0.3 pH reduction of the overlying water. However, the N removal rates through the anaerobic ammonium oxidation (anammox) process were concomitantly promoted under the same acidification conditions (increased by 47-109%, < 0.05), whereas the total rates of N loss were significantly inhibited by aquatic acidification ( < 0.05), as denitrification remained the dominant N removal pathway. More importantly, the emission of nitrous oxide (NO) from estuarine and coastal sediments was greatly stimulated by aquatic acidification ( < 0.05). Molecular analyses further demonstrated that aquatic acidification also altered the functional microbial communities in estuarine and coastal sediments; and the abundance of denitrifiers was significantly reduced ( < 0.05), while the abundance of anammox bacteria remained relatively stable. Collectively, this study reveals the effects of acidification on N removal processes and the underlying mechanisms and suggests that the intensifying acidification in estuarine and coastal waters might reduce the N removal function of these ecosystems, exacerbate eutrophication, and accelerate global climate change.
预计河口和沿海水域的酸化会影响氮 (N) 去除过程,这些过程是从这些生态系统中去除过量氮的关键途径。我们发现,在酸化条件下,反硝化速率显著下降(<0.05),在表层水 pH 值降低约 0.3 的情况下,河口和沿海沉积物中的反硝化速率分别降低了 41-53%。然而,在相同的酸化条件下,通过厌氧氨氧化(anammox)过程的 N 去除率同时得到促进(增加了 47-109%,<0.05),而由于反硝化仍然是主要的 N 去除途径,因此水生酸化显著抑制了总 N 损失率(<0.05)。更重要的是,水生酸化极大地促进了河口和沿海沉积物中一氧化二氮(NO)的排放(<0.05)。分子分析进一步表明,水生酸化还改变了河口和沿海沉积物中的功能微生物群落;反硝化菌的丰度显著降低(<0.05),而 anammox 菌的丰度相对稳定。总的来说,这项研究揭示了酸化对 N 去除过程及其潜在机制的影响,并表明河口和沿海水域酸化的加剧可能会降低这些生态系统的 N 去除功能,加剧富营养化,并加速全球气候变化。