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Methane in Lakes: Variability in Stable Carbon Isotopic Composition and the Potential Importance of Groundwater Input
Linköpings universitet, Institutionen för tema, Tema Miljöförändring. Linköpings universitet, Filosofiska fakulteten.
Linköpings universitet, Institutionen för tema, Tema Miljöförändring. Linköpings universitet, Filosofiska fakulteten.ORCID-id: 0000-0002-6815-7261
Linköpings universitet, Institutionen för tema, Tema Miljöförändring. Linköpings universitet, Filosofiska fakulteten.ORCID-id: 0000-0003-0472-7840
Linköpings universitet, Institutionen för tema, Tema Miljöförändring. Linköpings universitet, Filosofiska fakulteten.ORCID-id: 0000-0001-7960-0129
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2021 (Engelska)Ingår i: Frontiers in Earth Science, E-ISSN 2296-6463, Vol. 9, artikel-id 722215Artikel i tidskrift (Refereegranskat) Published
Hållbar utveckling
Klimatförbättringar, Miljöarbete
Abstract [en]

Methane (CH4) is an important component of the carbon (C) cycling in lakes. CH4 production enables carbon in sediments to be either reintroduced to the food web via CH4 oxidation or emitted as a greenhouse gas making lakes one of the largest natural sources of atmospheric CH4. Large stable carbon isotopic fractionation during CH4 oxidation makes changes in 13C:12C ratio (δ13C) a powerful and widely used tool to determine the extent to which lake CH4 is oxidized, rather than emitted. This relies on correct δ13C values of original CH4 sources, the variability of which has rarely been investigated systematically in lakes. In this study, we measured δ13C in CH4 bubbles in littoral sediments and in CH4 dissolved in the anoxic hypolimnion of six boreal lakes with different characteristics. The results indicate that δ13C of CH4 sources is consistently higher (less 13C depletion) in littoral sediments than in deep waters across boreal and subarctic lakes. Variability in organic matter substrates across depths is a potential explanation. In one of the studied lakes available data from nearby soils showed correspondence between δ13C-CH4 in groundwater and deep lake water, and input from the catchment of CH4 via groundwater exceeded atmospheric CH4 emissions tenfold over a period of 1 month. It indicates that lateral hydrological transport of CH4 can explain the observed δ13C-CH4 patterns and be important for lake CH4 cycling. Our results have important consequences for modelling and process assessments relative to lake CH4 using δ13C, including for CH4 oxidation, which is a key regulator of lake CH4 emissions.

Ort, förlag, år, upplaga, sidor
Lausanne, Switzerland: Frontiers Media S.A., 2021. Vol. 9, artikel-id 722215
Nyckelord [en]
General Earth and Planetary Sciences, stable carbon isotope, methane, lake, groundwater, endmember
Nationell ämneskategori
Miljövetenskap
Identifikatorer
URN: urn:nbn:se:liu:diva-181136DOI: 10.3389/feart.2021.722215ISI: 000717647200001Scopus ID: 2-s2.0-85118920484OAI: oai:DiVA.org:liu-181136DiVA, id: diva2:1612280
Forskningsfinansiär
EU, Europeiska forskningsrådetVetenskapsrådetForskningsrådet FormasKnut och Alice Wallenbergs Stiftelse
Anmärkning

Funding: European Research Council (ERC) under the European Unions Horizon 2020 research and innovation programmeEuropean Research Council (ERC) [725546]; Swedish Research CouncilSwedish Research CouncilEuropean Commission [201604829]; FORMASSwedish Research Council Formas [2018-01794]; Knut and Alice Wallenberg FoundationKnut & Alice Wallenberg Foundation [2016.0083]

Tillgänglig från: 2021-11-17 Skapad: 2021-11-17 Senast uppdaterad: 2023-08-28Bibliografiskt granskad
Ingår i avhandling
1. Methane dynamics in northern lakes: Insights from multi-scale observations
Öppna denna publikation i ny flik eller fönster >>Methane dynamics in northern lakes: Insights from multi-scale observations
2022 (Engelska)Doktorsavhandling, sammanläggning (Övrigt vetenskapligt)
Abstract [en]

Methane (CH4) is a potent greenhouse gas which is emitted to the atmosphere from both natural and anthropogenic sources. Current evidence indicates that lakes account for a large part of the global emissions of CH4, but their contribution is difficult to quantify because of large temporal and spatial variability in processes leading to CH4 fluxes from lakes to the atmosphere. Making sense of the complexity and variability of CH4 emissions from lakes requires observations covering the range of temporal and spatial scales at which these processes occur, both within and between lakes. Northern regions are of particular interest for such studies because they contain a larger number of lakes than any other region in the world and they are disproportionately affected by climate change, with possible consequences for future CH4 emissions.

The aim of this thesis was to investigate patterns of CH4 dynamics and emissions in several lakes distributed in different climatic regions of Sweden, paying particular attention to spatial and temporal variability of CH4 fluxes and concentrations. Fluxes, concentrations, carbon stable isotope signature of CH4, and a range of commonly monitored lake characteristics were measured several times during one year at multiple locations in each lake. The measurements provided an extensive set of observations of CH4 concentrations and fluxes in lakes, together with possible environmental drivers. These observations were then used to investigate patterns of CH4 dynamics in northern lakes and to assess the ability of empirical and process-based models to predict CH4 concentrations and fluxes in lakes.

The results indicate that simple empirical models, consisting of linear regressions between explanatory variables and CH4 fluxes and concentrations averaged over the lake surface and ice-free period of the year, can be useful in some specific cases (for example describing ebullitive fluxes from total phosphorus or chlorophyll a concentrations). However, it was also noted that using such models for extrapolation can lead to large errors, especially if the observations do not account for temporal and spatial variability of CH4 fluxes and concentrations. An example of high variability was seen in day-night measurements of CH4 fluxes in four lakes over several months. To try to compensate for some of the shortcomings of empirical models, an established process-based and one-dimensional lake model was used to simulate CH4 concentration in the water column of the studied lakes. Predictions were in good agreement with observations in several of the investigated lakes, considering that the model was not pre-calibrated for any of the lake specifically. However, it was also clear that there can be key processes that require specific consideration in process-based models, and some degree of simplification is needed, especially when detailed information on the modelled systems is not available. The simplifications and assumptions that need to be made can be informed by the study and observation of relevant processes in situ. For example, groundwater was found to potentially contribute a major part of CH4 stored in one small boreal lake using measurements of stable isotope signature of CH4 in littoral sediment and deep water of that lake, as well as in the groundwater in the mire next to it. Stable isotope measurements in five other lakes also revealed consistent differences in CH4 sources to the surface and deep zones of lakes when they are separated by thermal stratification of the water column. Such knowledge could be used in the design of numerical models of lakes with the objective to improve predictions of current and future emissions of CH4 from these environments.

Overall, this thesis contributes to the current knowledge on assessment of CH4 emissions from lakes at several temporal and spatial scales. It also emphasizes critical aspects which must be considered to reduce bias in future empirical and process-based models of CH4 in lakes.

Ort, förlag, år, upplaga, sidor
Linköping: Linköping University Electronic Press, 2022. s. 37
Serie
Linköping Studies in Arts and Sciences, ISSN 0282-9800 ; 837
Nyckelord
Methane, Lakes, Variability, Sampling design, Models
Nationell ämneskategori
Klimatforskning
Identifikatorer
urn:nbn:se:liu:diva-185123 (URN)10.3384/9789179293871 (DOI)9789179293864 (ISBN)9789179293871 (ISBN)
Disputation
2022-08-24, TEMCAS, Building T, Campus Valla, Linköping, 12:15 (Engelska)
Opponent
Handledare
Tillgänglig från: 2022-05-18 Skapad: 2022-05-18 Senast uppdaterad: 2022-05-18Bibliografiskt granskad

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Schenk, JonathanSawakuchi, Henrique OliveiraSieczko, Anna KatarzynaPajala, GustavRudberg, DavidBastviken, David

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Schenk, JonathanSawakuchi, Henrique OliveiraSieczko, Anna KatarzynaPajala, GustavRudberg, DavidHagberg, EmelieFors, KjellBastviken, David
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Frontiers in Earth Science
Miljövetenskap
Schenk, J., Sawakuchi, H. O., Sieczko, A. K., Pajala, G., Rudberg, D., Hagberg, E., . . . Bastviken, D. (2021). Data associated with the manuscript "Methane in Lakes: Variability in Stable Carbon Isotopic Composition and the Potential Importance of Groundwater Input". Linköping: Christoph Links Verlag

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