Long-term rise in riverine dissolved organic carbon concentration is predicted by electrolyte solubility theory

0571949 - ÚVGZ 2024 RIV US eng J - Článek v odborném periodiku
Monteith, D. T. - Henrys, Peter A. - Hruška, Jakub - de Wit, Heleen A. - Krám, Pavel - Moldan, F. - Posch, M. - Räike, A. - Stoddard, J. L. - Shilland, E.M. - Pereira, M.G. - Evans, Ch.D.
Long-term rise in riverine dissolved organic carbon concentration is predicted by electrolyte solubility theory.
Science Advances. Roč. 9, č. 3 (2023), č. článku eade3491. ISSN 2375-2548. E-ISSN 2375-2548
Grant CEP: GA ČR(CZ) GC21-22810J
Výzkumná infrastruktura: CzeCOS IV - 90248
Institucionální podpora: RVO:86652079
Klíčová slova: headwater catchment * streamwater * atmospheric deposition * electric conductivity
Obor OECD: Environmental sciences (social aspects to be 5.7)
Impakt faktor: 13.6, rok: 2022
Způsob publikování: Open access
https://www.science.org/doi/10.1126/sciadv.ade3491

The riverine dissolved organic carbon (DOC) flux is of similar magnitude to the terrestrial sink for atmospheric CO2 , but the factors controlling it remain poorly determined and are largely absent from Earth system models (ESMs). Here, we show, for a range of European headwater catchments, that electrolyte solubility theory explains how declining precipitation ionic strength (IS) has increased the dissolution of thermally moderated pools of soluble soil organic matter (OM), while hydrological conditions govern the proportion of this OM entering the aquatic system. Solubility will continue to rise exponentially with declining IS until pollutant ion deposition fully flattens out under clean air policies. Future DOC export will increasingly depend on rates of warming and any directional changes to the intensity and seasonality of precipitation and marine ion deposition. Our findings provide a firm foundation for incorporating the processes dominating change in this component of the global carbon cycle in ESMs.
Trvalý link: https://hdl.handle.net/11104/0342918