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  4. Exploring the Sources of Unexpected High Methane Concentrations and Fluxes From Alpine Headwater Streams
 
research article

Exploring the Sources of Unexpected High Methane Concentrations and Fluxes From Alpine Headwater Streams

Flury, S.  
•
Ulseth, A. J.  
June 28, 2019
Geophysical Research Letters

The dynamics of methane generation and evasion from well-oxygenated, oligotrophic streams have been traditionally neglected. We estimated evasion of methane and assessed its sources and production pathways using a stable isotope approach in 16 oxygen-rich and C-poor (dissolved organic carbon: 55.32 +/- 57.56 mu mol/L) Alpine headwater streams. Methane was often supersaturated relative to the atmosphere (0.093 +/- 0.179 mu mol/L). Fluxes (0.87 +/- 1.34 mmol.m(-2).day(-1)) were unexpectedly high and comparable to those from high-latitude lakes and reservoirs. Our findings suggest that methane in the streambed was largely produced from carbon dioxide reduction, whereas acetoclastic pathways and major deliveries from adjacent soils, assessed from a mass balance, may have contributed to stream water methane. This study sheds new light on high-alpine streams as a hitherto unaccounted source of methane to the atmosphere.

Plain Language Summary The greenhouse gas methane is naturally produced and emitted from organic matter rich freshwater ecosystems. Normally, this gas is produced in places where oxygen is absent. However, recent studies have shown that methane is also emitted from oxygen-rich rivers and streams. But the knowledge and understanding of the underlying processes that cause this paradox is currently poor. In this light, we investigated organic matter-poor and oxygen-rich Alpine streams to better understand the methane dynamics in those systems. We found that methane emissions from these streams are similar to emissions from organic-rich lakes and reservoirs at high latitudes, probably due to high gas exchange velocities in these steep environments. Methane that is found in the streambed of these streams is likely produced from inorganic carbon in oxygen-depleted sediment pockets, while in the stream water it likely originates mainly from adjacent soils. Headwater streams are most numerous in river networks worldwide, often organic matter poor and oxygen rich. Together with the strong potential for methane emissions, it is clear that Alpine streams should be considered in future methane emission budgets and knowledge about methane sources should be improved for effective mitigation of methane emissions.

  • Details
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Type
research article
DOI
10.1029/2019GL082428
Web of Science ID

WOS:000477616300051

Author(s)
Flury, S.  
Ulseth, A. J.  
Date Issued

2019-06-28

Publisher

AMER GEOPHYSICAL UNION

Published in
Geophysical Research Letters
Volume

46

Issue

12

Start page

6614

End page

6625

Subjects

Geosciences, Multidisciplinary

•

Geology

•

methane

•

mountain streams

•

carbon

•

greenhouse gas emisisons

•

production pathways

•

stable carbon isotopes

•

size distribution

•

gaseous carbon

•

organic-matter

•

water

•

emissions

•

oxidation

•

fractionation

•

chemistry

•

continuum

•

sediment

Editorial or Peer reviewed

REVIEWED

Written at

EPFL

EPFL units
RIVER  
Available on Infoscience
August 13, 2019
Use this identifier to reference this record
https://infoscience.epfl.ch/handle/20.500.14299/159709
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