Global Rivers Emit Greenhouse Gas Nitrous Oxide
Waterways receiving nitrogen from human activities are significant source
What goes in must come out, a truism that now may be applied to global river networks.
Human-caused nitrogen loading to river networks is a potentially important source of nitrous oxide emission to the atmosphere. Nitrous oxide is a potent greenhouse gas that contributes to climate change and stratospheric ozone destruction.
It happens via a microbial process called denitrification, which converts nitrogen to nitrous oxide and an inert gas called dinitrogen.
When summed across the globe, scientists report this week in the journal Proceedings of the National Academy of Sciences (PNAS), river and stream networks are the source of at least 10 percent of human-caused nitrous oxide emissions to the atmosphere.
That’s three times the amount estimated by the Intergovernmental Panel on Climate Change (IPCC).
Rates of nitrous oxide production via denitrification in small streams increase with nitrate concentrations.
“Human activities, including fossil fuel combustion and intensive agriculture, have increased the availability of nitrogen in the environment,” says Jake Beaulieu of the University of Notre Dame and the U.S. Environmental Protection Agency in Cincinnati, Ohio, and lead author of the PNAS paper.
“Much of this nitrogen is transported into river and stream networks,” he says, “where it may be converted to nitrous oxide, a potent greenhouse gas, via the activity of microbes.”
Beaulieu and co-authors measured nitrous oxide production rates from denitrification in 72 streams draining multiple land-use types across the United States. Their work was part of a broader cross-site study of nitrogen processing in streams.
“This multi-site experiment clearly establishes streams and rivers as important sources of nitrous oxide,” says Henry Gholz, program director in NSF’s Division of Environmental Biology, which funded the research.
“This is especially the case for those draining nitrogen-enriched urbanized and agricultural watersheds, highlighting the importance of managing nitrogen before it reaches open water,” Gholz says. “This new global emission estimate is startling.”
Atmospheric nitrous oxide concentration has increased by some 20 percent over the past century, and continues to rise at a rate of about 0.2 to 0.3 percent per year.
Beaulieu and colleagues, say the global warming potential of nitrous oxide is 300-fold greater than carbon dioxide.
Nitrous oxide accounts for some six percent of human-induced climate change, scientists estimate.
They believe that nitrous oxide is the leading human-caused threat to the atmospheric ozone layer, which protects Earth from harmful ultraviolet radiation from the Sun.
Researchers had estimated that denitrification in river networks might be a globally important source of human-derived nitrous oxide, but the process had been poorly understood, says Beaulieu, and estimates varied widely.
While more than 99 percent of denitrified nitrogen in streams is converted to the inert gas dinitrogen rather than nitrous oxide, river networks are still leading sources of global nitrous oxide emissions, according to the new results.
“Changes in agricultural and land-use practices that result in less nitrogen being delivered to streams would reduce nitrous oxide emissions from river networks,” says Beaulieu.
The findings, he and co-authors hope, will lead to more effective mitigation strategies.
Other authors of the paper are: Jennifer Tank of the University of Notre Dame; Stephen Hamilton of Michigan State University; Wilfred Wollheim of the University of New Hampshire; Robert Hall of the University of Wyoming; Patrick Mulholland of Oak Ridge National Laboratory and the University of Tennessee; Bruce Peterson of Marine Biological Laboratory in Woods Hole, Mass.; Linda Ashkenas of Oregon State University; Lee Cooper of the Chesapeake Biological Laboratory in Solomons, Md.; Clifford Dahm of the University of New Mexico; Walter Dodds of Kansas State University; Nancy Grimm of Arizona State University; Sherri Johnson of the U.S. Forest Service in Corvallis, Ore.; William McDowell of the University of New Hampshire; Geoffe Poole of Montana State University; HM Valett of Virginia Polytechnic Institute and State University; Clay Arango of Central Washington University; Melody Bernot of Ball State University; Amy Burgin of Wright State University; Chelsea Crenshaw of the University of New Mexico; Ashley Helton of the University of Georgia; Laura Johnson of Indiana University; Jonathan O’Brien of the University of Canterbury in Christchurch, New Zealand; Jody Potter of the University of New Hampshire; Richard Sheibley of the University of Notre Dame and the U.S. Geological Survey in Tacoma, Washington; Daniel Sobota of Washington State University; and Suzanne Thomas of the Marine Biological Laboratory in Woods Hole, Mass.
Image 1: The Corralles drainage ditch in Albuquerque, N.M., was one of 72 study sites in the research. Credit: Chelsea Crenshaw
Image 2: Scientists collect stream water samples on a golf course near Jackson Hole, Wyoming. Credit: Jake Beaulieu
Image 3: An urban drainage canal in Oregon was among the study sites in the experiment. Credit: Jake Beaulieu
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