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Hydrological controls on temporal contributions of three nested forested subcatchments to the export of dissolved organic carbon

DOI zum Zitieren der Version auf EPub Bayreuth: https://doi.org/10.15495/EPub_UBT_00009373
URN zum Zitieren der Version auf EPub Bayreuth: urn:nbn:de:bvb:703-epub-9373-6

Titelangaben

Blaurock, Katharina ; Beudert, Burkhard ; Hopp, Luisa:
Hydrological controls on temporal contributions of three nested forested subcatchments to the export of dissolved organic carbon.
In: Hydrology and Earth System Sciences. Bd. 29 (2025) Heft 11 . - S. 2377-2391.
ISSN 1607-7938
DOI der Verlagsversion: https://doi.org/10.5194/hess-29-2377-2025

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Abstract

Assessing the export of dissolved organic carbon (DOC) from terrestrial systems into inland waters reliably is of vital importance to understand the global carbon cycle in detail. In this context, hydrological connectivity within catchments is the prerequisite for transport processes from terrestrial systems into inland waters. Using high-frequency measurements of DOC concentrations via ultraviolet–visible (UV–Vis) spectrometry, we quantified the DOC export at the outlets of three nested forested subcatchments within a 3.5 km2 headwater catchment in the Bavarian Forest National Park (BFNP), Germany, during a 12-month period. The subcatchments differ with respect to topography, elevation, vegetation, and soil types. We observed a high flow-weighted DOC export from the entire headwater catchment during spring and autumn. In contrast, during snowmelt, summer, and winter, DOC export was low due to either low runoff generated and/or relatively lower DOC available for mobilization. Flow-weighted DOC export also varied between the three subcatchments. Flow-weighted DOC export was always higher in the flat lower subcatchment than in the steep upper subcatchments, indicating a large DOC store that can be activated whenever hydrological connectivity is established. This was particularly evident during autumn, when large precipitation events mobilized DOC which had accumulated during the dry summer period and was also delivered from fresh leaf litter of deciduous trees. Our data show the strong hydrological control on seasonal DOC export. However, the runoff-based contribution of subcatchments over time is modulated by the interplay of soils, vegetation, topography, and microclimate, which can be seen as secondary controls. As hydrological connectivity varies with topography, the relative contribution of topographically different subcatchments varies seasonally. Since climate change is predicted to influence precipitation patterns, spatial and temporal DOC export patterns are likely to change depending on topography.

Weitere Angaben

Publikationsform: Artikel in einer Zeitschrift
Themengebiete aus DDC: 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie
Institutionen der Universität: Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften > Fachgruppe Geowissenschaften > Lehrstuhl Hydrologie > Lehrstuhl Hydrologie - Univ.-Prof. Dr. Stefan Peiffer
Forschungseinrichtungen > Zentrale wissenschaftliche Einrichtungen > Bayreuther Zentrum für Ökologie und Umweltforschung - BayCEER
Fakultäten
Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften
Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften > Fachgruppe Geowissenschaften
Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften > Fachgruppe Geowissenschaften > Lehrstuhl Hydrologie
Forschungseinrichtungen
Forschungseinrichtungen > Zentrale wissenschaftliche Einrichtungen
Sprache: Englisch
Titel an der UBT entstanden: Ja
URN: urn:nbn:de:bvb:703-epub-9373-6
Eingestellt am: 02 Jun 2026 12:00
Letzte Änderung: 02 Jun 2026 12:01
URI: https://epub.uni-bayreuth.de/id/eprint/9373

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