GSTDTAP  > 气候变化
DOI10.1029/2019GL082428
Exploring the Sources of Unexpected High Methane Concentrations and Fluxes From Alpine Headwater Streams
Flury, S.1; Ulseth, A. J.1,2
2019-06-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2019
卷号46期号:12页码:6614-6625
文章类型Article
语种英语
国家Switzerland; USA
英文摘要

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.


英文关键词Methane mountain streams carbon greenhouse gas emisisons production pathways stable carbon isotopes
领域气候变化
收录类别SCI-E
WOS记录号WOS:000477616300051
WOS关键词SIZE DISTRIBUTION ; GASEOUS CARBON ; ORGANIC-MATTER ; WATER ; EMISSIONS ; OXIDATION ; FRACTIONATION ; CHEMISTRY ; CONTINUUM ; SEDIMENT
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
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被引频次:22[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/184250
专题气候变化
作者单位1.Ecole Polytech Fed Lausanne, Sch Architecture Civil & Environm Engn, Inst Environm Engn, Stream Biofilm & Ecosyst Res Lab, Lausanne, Switzerland;
2.Sam Houston State Univ, Dept Biol Sci, Huntsville, TX 77340 USA
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GB/T 7714
Flury, S.,Ulseth, A. J.. Exploring the Sources of Unexpected High Methane Concentrations and Fluxes From Alpine Headwater Streams[J]. GEOPHYSICAL RESEARCH LETTERS,2019,46(12):6614-6625.
APA Flury, S.,&Ulseth, A. J..(2019).Exploring the Sources of Unexpected High Methane Concentrations and Fluxes From Alpine Headwater Streams.GEOPHYSICAL RESEARCH LETTERS,46(12),6614-6625.
MLA Flury, S.,et al."Exploring the Sources of Unexpected High Methane Concentrations and Fluxes From Alpine Headwater Streams".GEOPHYSICAL RESEARCH LETTERS 46.12(2019):6614-6625.
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