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Relationships between riverine and terrestrial dissolved organic carbon: Concentration, radiocarbon signature, specific UV absorbance.
Tipping, Edward; Elias, Jessica L; Keenan, Patrick O; Helliwell, Rachel C; Pedentchouk, Nikolai; Cooper, Richard J; Buckingham, Sarah; Gjessing, Egil; Ascough, Philippa; Bryant, Charlotte L; Garnett, Mark H.
Afiliación
  • Tipping E; UK Centre for Ecology and Hydrology, Lancaster Environment Centre, Lancaster LA1 4AP, UK. Electronic address: et@ceh.ac.uk.
  • Elias JL; UK Centre for Ecology and Hydrology, Lancaster Environment Centre, Lancaster LA1 4AP, UK.
  • Keenan PO; UK Centre for Ecology and Hydrology, Lancaster Environment Centre, Lancaster LA1 4AP, UK.
  • Helliwell RC; The James Hutton Institute, Craigiebuckler, Aberdeen AB15 8QH, Scotland, UK.
  • Pedentchouk N; School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK; Skolkovo Institute of Science and Technology, 30 Bld. 1 Bolshoy Boulevard, Moscow 121205, Russian Federation.
  • Cooper RJ; School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK.
  • Buckingham S; Carbon Crop and Soils Group, Scotland's Rural College, Edinburgh EH9 3JG, UK.
  • Gjessing E; Faculty of Mathematics and Natural Sciences, University of Oslo, NO-0316 Oslo, Norway.
  • Ascough P; NERC Radiocarbon Facility, East Kilbride G75 0QF, UK.
  • Bryant CL; NERC Radiocarbon Facility, East Kilbride G75 0QF, UK.
  • Garnett MH; NERC Radiocarbon Facility, East Kilbride G75 0QF, UK.
Sci Total Environ ; 817: 153000, 2022 Apr 15.
Article en En | MEDLINE | ID: mdl-35031358
ABSTRACT
The transfer of dissolved organic carbon (DOC) from land to watercourses plays a major role in the carbon cycle, and in the transport and fate of associated organic and inorganic contaminants. We investigated, at global scale, how the concentrations and properties of riverine DOC depend upon combinations of terrestrial source solutions. For topsoil, subsoil, groundwater and river solutions in different Köppen-Geiger climatic zones, we compiled published and new values of DOC concentration ([DOC]), radiocarbon signature (DO14C), and specific UV absorbance (SUVA). The average value of each DOC variable decreased significantly in magnitude from topsoil to subsoil to groundwater, permitting the terrestrial sources to be distinguished. We used the terrestrial data to simulate the riverine distributions of each variable, and also relationships between pairs of variables. To achieve good matches between observed and simulated data, it was necessary to optimise the distributions of water fractions contributed by each of the three terrestrial sources, and also to reduce the mean input terrestrial [DOC] values, to about 60% of the measured ones. One possible explanation for the required lowering of the modelled terrestrial [DOC] values might be unrepresentative sampling of terrestrial DOC, including dilution effects; another is the loss of DOC during riverine transport. High variations in simulated riverine DOC variables, which match observed data, are due predominantly to variations in source solution values, with a lesser contribution from the different combinations of source waters. On average, most DOC in rivers draining catchments with forest and/or grass-shrub land cover comes in similar amounts from topsoil and subsoil, with about 10% from groundwater. In rivers draining croplands, subsoil and groundwater solutions are the likely dominant DOC sources, while in wetland rivers most DOC is from topsoil.
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Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Asunto principal: Monitoreo del Ambiente / Materia Orgánica Disuelta Tipo de estudio: Prognostic_studies Idioma: En Revista: Sci Total Environ Año: 2022 Tipo del documento: Article

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Asunto principal: Monitoreo del Ambiente / Materia Orgánica Disuelta Tipo de estudio: Prognostic_studies Idioma: En Revista: Sci Total Environ Año: 2022 Tipo del documento: Article