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Identification of methane cycling pathways in Quaternary alluvial-lacustrine aquifers using multiple isotope and microbial indicators.

Authors :
Tian H
Du Y
Deng Y
Sun X
Xu J
Gan Y
Wang Y
Source :
Water research [Water Res] 2024 Feb 15; Vol. 250, pp. 121027. Date of Electronic Publication: 2023 Dec 16.
Publication Year :
2024

Abstract

Groundwater rich in dissolved methane is often overlooked in the global or regional carbon cycle. Considering the knowledge gap in understanding the biogeochemical behavior of methane in shallow aquifers, particularly those in humid alluvial-lacustrine plains with high organic carbon content, we investigated methane sources and cycling pathways in groundwater systems at the central Yangtze River basins. Composition of multiple stable isotopes ( <superscript>2</superscript> H/ <superscript>18</superscript> O in water, <superscript>13</superscript> C in dissolved inorganic carbon, <superscript>13</superscript> C/ <superscript>2</superscript> H in methane, and <superscript>13</superscript> C in carbon dioxide) was combined with the characteristics of microbes and dissolved organic matter (DOM) in the study. The results revealed significant concentrations of biogenic methane reaching up to 13.05 mg/L in anaerobic groundwater environments with abundant organic matter. Different pathways for methane cycling (methanogenic CO <subscript>2</subscript> -reduction and acetate-fermentation, and methane oxidation) were identified. CO <subscript>2</subscript> -reduction dominated acetate-fermentation in the two methanogenic pathways primarily associated with humic DOM, while methane oxidation was more closely associated with microbially derived DOM. The abundance of obligate CO <subscript>2</subscript> -reduction microorganisms (Methanobacterium and Methanoregula) was higher in samples with substantial CO <subscript>2</subscript> -reduction, as indicated by isotopic composition. The obligate acetate-fermentation microorganism (Methanosaeta) was more abundant in samples exhibiting evident acetate-fermentation. Additionally, a high abundance of Candidatus Methanoperedens was identified in samples with apparent methane oxidation. Comparing our findings with those in other areas, we found that various factors, such as groundwater temperature, DOM abundance and types, and hydrogeological conditions, may lead to differences in groundwater methane cycling. This study offered a new perspective and understanding of methane cycling in worldwide shallow alluvial-lacustrine aquifer systems without geothermal disturbance.<br />Competing Interests: Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2023 Elsevier Ltd. All rights reserved.)

Details

Language :
English
ISSN :
1879-2448
Volume :
250
Database :
MEDLINE
Journal :
Water research
Publication Type :
Academic Journal
Accession number :
38113595
Full Text :
https://doi.org/10.1016/j.watres.2023.121027