The C-biogeochemistry of a Midwestern USA agricultural impoundment in context: Lake Decatur in the intensively managed landscape critical zone observatory

Neal E. Blair, Elana L. Leithold, A. N. Thanos Papanicolaou, Christopher G. Wilson, Laura Keefer, Erin Kirton, David Vinson, Doug Schnoebelen, Bruce Rhoads, Mingjing Yu, Quinn Lewis

Research output: Contribution to journalArticlepeer-review

9 Scopus citations


The damming of rivers has created hotspots for organic carbon sequestration and methane production on a global scale as the reservoirs intercept fluvial suspended and dissolved loads. To better understand how the C-biogeochemistry of a reservoir responds to watershed processes and evolves over time, Lake Decatur, located in the Intensively Managed Landscape Critical Zone Observatory (IML-CZO) was studied. Solid phase analyses (% organic C, C/N, δ13C, δ15N) of soils and sediments sampled from stream bank exposures, river suspensions, and the lake bottom were conducted to characterize organic C (OC) sources throughout the sedimentary system. Agriculturally-driven soil erosion rapidly altered lake bathymetry causing an evolution of sedimentary and OC deposition patterns, which in turn shaped where and when methane production occurred. A positive correlation between OC accumulation rate and porewater dissolved inorganic C (DIC) δ13C profiles indicates that methane generation is strongly influenced by OC burial rate. The sources of the lake bed particulate organic C (POC) have also evolved over time. Drowned vegetation and/or shoreline inputs were dominant initially in areas adjacent to the original river channel but were rapidly overwhelmed by the deposition of sediments derived from eroded agricultural soils. Eutrophication of the lake followed with the onset of heavy fertilizer application post-1960. This succession of sources is expected to be commonplace for reservoirs greater than ~ 50–60 years old in agricultural settings because of the relative timing of tillage and fertilizer practices. The 13C/12C ratios of methane from Lake Decatur were more depleted in 13C than what is commonly expected for freshwater sedimentary environments. The 13C-depletion suggests that CO2-reduction is the dominant methanogenic pathway rather than the anticipated acetate dissimilation process. The isotopic observations reveal that commonly held assumptions about methane production and its C-isotopic signature in freshwater systems are over-simplified and not strictly applicable to this system.

Original languageEnglish (US)
Pages (from-to)171-195
Number of pages25
Issue number2
StatePublished - Apr 1 2018

Bibliographical note

Funding Information:
Acknowledgements Financial support was provided by the US National Science Foundation (NSF) Grant # EAR-1331906 for the Critical Zone Observatory for Intensively Managed Landscapes (IML-CZO), a multi-institutional collaborative effort. Funding was also provided by the Institute for Sustainability and Energy at Northwestern (ISEN). DV received support from a NSF Earth Sciences Postdoctoral Fellowship (EAR 1249916). We thank Laurel Childress, Martin Goshev, Paul Roots, Yue Zeng and Koushik Dutta for their assistance with the field and laboratory work. Special thanks are given to Joe Nihiser of the City of Decatur for his support and assistance with this project. Andrew Stumpf provided information concerning soil sampling locations and classifications as well as assistance with soil sampling.

Publisher Copyright:
© 2018, Springer International Publishing AG, part of Springer Nature.

Copyright 2018 Elsevier B.V., All rights reserved.


  • C-cycle
  • Carbon sequestration
  • Methane
  • Reservoirs

Continental Scientific Drilling Facility tags

  • IML


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