Biogeochemistry

, Volume 136, Issue 1, pp 47–70 | Cite as

Organic matter distribution and retention along transects from hilltop to kettle hole within an agricultural landscape

  • Kai Nils Nitzsche
  • Michael Kaiser
  • Katrin Premke
  • Arthur Gessler
  • Ruth Heike Ellerbrock
  • Carsten Hoffmann
  • Andreas Kleeberg
  • Zachary Eric Kayler
Article

Abstract

In agricultural landscapes, the spatio-temporal distribution of organic matter (OM) varies greatly across landscape structures and soil types. We investigated patterns of organic carbon (OC) content, polyvalent cations, and isotopic values for specific OM fractions along transects spanning topographic positions from erosional to depositional areas, including aquatic sediments within a single kettle hole. We hypothesized different drivers exist at different scales. At the transect scale, we hypothesized (1) landscape form and land management to explain patterns of isotopic and OC content from different OM fractions. At the aggregate scale, (2) we expected different OM-mineral associations to explain stabilized OM. We also hypothesized, (3) that shallow sediment δ13C and δ15N of the kettle hole reflected different terrestrial sources. We found that distinct differences in the OM turnover rates existed between the fractions suggesting that different processes are affecting the transformation rates that are recorded in the isotopic composition patterns. Erosion along with plant productivity drive mineral-associated fractions over the transect, while microbial decomposition and slurry influence freely available and aggregated OM fractions. The type and magnitude of OM-mineral associations changed along the transect while binding OM of different decomposition status. OM in mineral-associated fractions in kettle hole sediments were derived from clay- and silt-sized particles from the field, whereas OM in freely available and aggregated fractions potentially originated from macrophytes. We conclude that kettle holes constitute important sinks for terrestrial OM across the landscape.

Keywords

Stable isotopes Erosion Soil organic matter Organo-mineral interaction Land management Depressional wetland 

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Copyright information

© Springer International Publishing AG 2017

Authors and Affiliations

  • Kai Nils Nitzsche
    • 1
    • 11
  • Michael Kaiser
    • 2
  • Katrin Premke
    • 1
    • 3
  • Arthur Gessler
    • 1
    • 4
    • 5
  • Ruth Heike Ellerbrock
    • 6
  • Carsten Hoffmann
    • 6
    • 7
  • Andreas Kleeberg
    • 8
  • Zachary Eric Kayler
    • 1
    • 9
    • 10
  1. 1.Leibniz Centre for Agricultural Landscape Research (ZALF)Institute of Landscape BiogeochemistryMuenchebergGermany
  2. 2.Department of Environmental ChemistryUniversity of KasselWitzenhausenGermany
  3. 3.Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Chemical Analytic and BiogeochemistryBerlinGermany
  4. 4.Swiss Federal Institute for Forest, Snow and Landscape Research (WSL)BirmensdorfSwitzerland
  5. 5.Berlin-Brandenburg Institute of Advanced Biodiversity Research (BBIB)BerlinGermany
  6. 6.Leibniz Centre for Agricultural Landscape Research (ZALF), Institute of Soil Landscape ResearchMuenchebergGermany
  7. 7.Leibniz Centre for Agricultural Landscape Research (ZALF), Agricultural Landscape Data CentreMuenchebergGermany
  8. 8.State Laboratory Berlin-BrandenburgDepartment Geology, Soil, WasteKleinmachnowGermany
  9. 9.Lawrence Livermore National LaboratoryCenter for Accelerator Mass SpectrometryLivermoreUSA
  10. 10.Department of Soil and Water SystemsUniversity of IdahoMoscowUSA
  11. 11.Research Institute for Humanity and Nature (RIHN)KyotoJapan

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