Journal
LIMNOLOGY AND OCEANOGRAPHY
Volume 67, Issue 2, Pages 450-467Publisher
WILEY
DOI: 10.1002/lno.12003
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Funding
- USDA Forest Service
- Pacific Northwest Research Station
- National Fish and Wildlife Foundation
- University of Notre Dame
- National Science Foundation Graduate Research Fellowship Program
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Ponds play a larger role in the global freshwater methane (CH4) budget than predicted, with CH4 production in ponds being influenced by factors such as water-column temperature, chlorophyll a (Chl a), and microbial community structure. The study showed that a significant amount of CH4 produced in ponds is oxidized, and that pond ebullition is a major source of CH4 emissions. Additionally, pond ebullition rates were found to be correlated with production rates from previous months.
Ponds play a larger role in the global freshwater methane (CH4) budget than predicted from surface area alone. To improve our understanding of pond CH4 dynamics, we measured summer CH4 production, concentrations, and emissions to the atmosphere in nine Alaskan wetland ponds along with potential physical, chemical, and biological regulators. Pond CH4 production (0.64, 0.086-1.3 mmol m(-2) d(-1); median, interquartile range), as assessed with slurry incubations, was positively related to water-column temperature and chlorophyll a (Chl a), negatively influenced by oxygen levels, and varied with microbial community structure. Average water-column CH4 concentrations (0.39, 0.21-0.87 mu mol L-1) were lower in deeper ponds and at higher oxygen levels, and as expected, they were correlated with diffusive emissions (0.055, 0.024-0.20 mmol m(-2) d(-1)) assessed with flux chambers. Based on a mass balance approach, 39-99% of CH4 produced in ponds was oxidized. Pond ebullition (3.7, 0.60-24 mmol m(-2) d(-1)) was higher and more variable than diffusive emissions. Additionally, pond ebullition rates were better correlated with production rates from the previous month. We also systematically compared the ratio of ebullition to diffusive CH4 emissions in our ponds and other northern lakes, which was negatively related to water depth (n = 71), but positively related to Chl a (n = 28). Our study sheds light on the factors that influence pond CH4 dynamics and demonstrates that pond ebullition is a significant CH4 source worthy of continued study.
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