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美国河流中不断变化的氮格局:沉降减少与有机氮增加

The changing nitrogen landscape of United States streams: Declining deposition and increasing organic nitrogen.

作者信息

Lin Jiajia, Compton Jana E, Sabo Robert D, Herlihy Alan T, Hill Ryan A, Weber Marc H, Brooks J Renée, Paulsen Steve G, Stoddard John L

机构信息

Pacific Ecological Systems Division, Office of Research and Development, US Environmental Protection Agency, Corvallis, OR 97333, USA.

Oak Ridge Institute for Science and Education, Corvallis, OR 97333, USA.

出版信息

PNAS Nexus. 2023 Nov 3;3(1):pgad362. doi: 10.1093/pnasnexus/pgad362. eCollection 2024 Jan.

Abstract

Air quality regulations have led to decreased nitrogen (N) and sulfur deposition across the conterminous United States (CONUS) during the last several decades, particularly in the eastern parts. But it is unclear if declining deposition has altered stream N at large scales. We compared watershed N inputs with N chemistry from over 2,000 CONUS streams where deposition was the largest N input to the watershed. Weighted change analysis showed that deposition declined across most watersheds, especially in the Eastern CONUS. Nationally, declining N deposition was not associated with significant large-scale declines in stream nitrate concentration. Instead, significant increases in stream dissolved organic carbon (DOC) and total organic N (TON) were widespread across regions. Possible mechanisms behind these increases include declines in acidity and/or ionic strength drivers, changes in carbon availability, and/or climate variables. Our results also reveal a declining trend of DOC/TON ratio over the entire study period, primarily influenced by the trend in the Eastern region, suggesting the rate of increase in stream TON exceeded the rate of increase in DOC concentration during this period. Our results illustrate the complexity of nutrient cycling that links long-term atmospheric deposition to water quality. More research is needed to understand how increased dissolved organic N could affect aquatic ecosystems and downstream riverine nutrient export.

摘要

在过去几十年里,空气质量法规已导致美国本土(CONUS)的氮(N)和硫沉降减少,尤其是在东部地区。但尚不清楚沉降减少是否在大尺度上改变了溪流中的氮含量。我们将流域氮输入与美国本土2000多条溪流的氮化学特征进行了比较,在这些流域中,沉降是氮的最大输入来源。加权变化分析表明,大多数流域的沉降量都在下降,尤其是在美国本土东部地区。在全国范围内,氮沉降下降与溪流硝酸盐浓度的显著大规模下降并无关联。相反,溪流溶解有机碳(DOC)和总有机氮(TON)的显著增加在各地区普遍存在。这些增加背后的可能机制包括酸度和/或离子强度驱动因素的下降、碳可用性的变化和/或气候变量。我们的研究结果还揭示了在整个研究期间DOC/TON比值呈下降趋势,主要受东部地区趋势的影响,这表明在此期间溪流TON的增加速率超过了DOC浓度的增加速率。我们的研究结果说明了将长期大气沉降与水质联系起来的养分循环的复杂性。需要更多研究来了解溶解有机氮增加如何影响水生生态系统和下游河流养分输出。

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