Variability and drivers of CO2, CH4, and N2O concentrations in streams across the United States. Issue 2 (19th December 2022)

• Record Type: Journal Article
• Authors: DelVecchia, Amanda G.; Rhea, Spencer; Aho, Kelly S.; Stanley, Emily H.; Hotchkiss, Erin R.; Carter, Alice; Bernhardt, Emily S.
• Is Part Of: Limnology and oceanography. Volume 68:Issue 2(2023)
• Page Start: 394
• Page End: 408
• Publication Date: 2022-12-19
• Subjects: Limnology -- Periodicals; Oceanography -- Periodicals; Océanographie; Limnologie; Limnology; Oceanography; Computer network resources; Périodique électronique (Descripteur de forme); Ressource Internet (Descripteur de forme); Periodicals; 551.4805
• DOI: 10.1002/lno.12281
• Languages: English
• ISSNs: 0024-3590

Abstract

Abstract: Streams and rivers are major sources of greenhouse gases (GHGs) to the atmosphere, as carbon and nitrogen are converted and outgassed during transport. Although our understanding of drivers of individual GHG fluxes has improved with numerous site‐specific studies and global‐scale compilations, our ability to parse out interrelated physical and biogeochemical drivers of gas concentrations is limited by a lack of consistently collected, temporally continuous samples of GHGs and their associated drivers. We present a first analysis of such a dataset collected by the National Ecological Observatory Network across 27 streams and rivers across ecoclimatic domains of the United States. Average concentrations of CO2 ranged from 36.9 ± 0.88 to 404 ± 33 μ mol L −1, CH4 from 0.003 ± 0.0003 to 4.99 ± 0.72 μ mol L −1, and N2 O from 0.015 to 0.04 μ mol L −1 and spanned ranges of previous global compilations. Both CO2 and CH4 were strongly affected by physical drivers including mean air temperature and stream slope, as well as by dissolved oxygen and total nitrogen concentrations. N2 O was exclusively correlated with total nitrogen concentrations. Results suggested that potential for gas exchange dominated patterns in gas concentrations at the site level, but contributions of in‐stream aerobic and anaerobic metabolism, and groundwater also likely varied across sites. The highest gas concentrations as well as highest variability occurred in low‐gradient, warmer, and nonperennial systems. These results are a first step in providing unprecedented, continuous estimates of GHG flux constrained by temporally variable physical and biogeochemical drivers of GHG production.