Details zur Publikation

Referenztyp Zeitschriften
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Creative Commons Lizenz creative commons licence
Titel (primär) Iron exports from catchments are constrained by redox status and topography
Autor Tittel, J.; Büttner, O.; Friese, K.; Lechtenfeld, O.J.; Schuth, S.; von Tümpling, W.; Musolff, A.
Journal / Serie Global Biogeochemical Cycles
Erscheinungsjahr 2022
Department ASAM; SEEFO; FLOEK; ANA; HDG
Band/Volume 36
Heft 1
Seite von e2021GB007056
Sprache englisch
Topic T5 Future Landscapes
Datenlinks https://doi.org/10.4211/hs.43601618877945c5a46b715aa98db729
Supplements https://agupubs.onlinelibrary.wiley.com/action/downloadSupplement?doi=10.1029%2F2021GB007056&file=2021GB007056-sup-0001-Supporting+Information+SI-S01.pdf
Keywords river; mineral phosphorus; carbon; soil; watershed; metal; groundwater; NOSC
Abstract Fe(III) hydroxides stabilize organic carbon (OC) and P in soils. Observations of rising stream Fe concentrations are controversially posited to result from a flushing of iron-rich deeper soil layers or a decrease of competing electron acceptors inhibiting Fe reduction (urn:x-wiley:08866236:media:gbc21222:gbc21222-math-0001 and urn:x-wiley:08866236:media:gbc21222:gbc21222-math-0002). Here, we argue that catchment topography constrains the release of Fe, OC, and P to streams. We therefore incubated organic topsoil and mineral subsoil and modified the availability of urn:x-wiley:08866236:media:gbc21222:gbc21222-math-0003. We found that Fe leaching was highest in topsoil. Fe, OC, and P released at quantities proportional to their ratios in the source soil. Supply of urn:x-wiley:08866236:media:gbc21222:gbc21222-math-0004 reduced Fe leaching to 18% and increased pore water OC:Fe and P:Fe ratios. Subsoil, however, was an insignificant Fe source (<0.5%). Here, the leached quantities of Fe, OC and P were highly disproportionate to the soil source with an excess of released OC and P. We tested if experimental findings scale up using data from 88 German catchments representing gradients in urn:x-wiley:08866236:media:gbc21222:gbc21222-math-0005 concentration and topography. Average stream Fe concentrations increased with decreasing urn:x-wiley:08866236:media:gbc21222:gbc21222-math-0006 and were high in catchments with shallow topography where high groundwater levels support reductive processes and topsoils are hydrologically connected to streams; but Fe concentrations were low in catchments with steep topography where flow occurs primarily through subsoils. OC:Fe and P:Fe ratios in the streams similarly varied by urn:x-wiley:08866236:media:gbc21222:gbc21222-math-0007 and topography. This corroborates the findings from the laboratory experiment and suggests that catchment topography and competing electron acceptors constrain the formation of Fe-reducing conditions and control the release of Fe, OC, and P to streams.
dauerhafte UFZ-Verlinkung https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=25538
Tittel, J., Büttner, O., Friese, K., Lechtenfeld, O.J., Schuth, S., von Tümpling, W., Musolff, A. (2022):
Iron exports from catchments are constrained by redox status and topography
Glob. Biogeochem. Cycles 36 (1), e2021GB007056