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Biogeochemical causes of sixty-year trends and seasonal variations of river water properties in a large European basin

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Abstract

We evaluated long-term trends and seasonal variations in the major physical–chemical properties of the circum-neutral Slapy reservoir (Vltava, Czech Republic) from 1960 to 2019. Mean annual water temperature increased by 2.1 °C, flow maxima shifted by ~ 13 days from the early April to mid-March, and the onset of thermal stratification of water column and spring algal peaks advanced by 19 and 21 days, respectively, due to climate warming. Concentrations of major ions, phosphorus (P), and chlorophyll increased from the 1960s to the 1990–2000s, then decreased due to changing agricultural practices and legislation, intensified wastewater treatment, and decreasing atmospheric pollution. Concentrations of dissolved organic carbon (DOC) decreased from 1960 to the 1990s due to improved wastewater treatment, then began to increase in response to climate change and reduced acidic deposition. Concentrations of water constituents exhibited varying individual long-term and seasonal patterns due to the differing effects of following major processes on their production/removal in the catchment-river system: (1) applications of synthetic fertilizers, liming and farmland draining (NO3, SO42−, Cl, Ca2+, Mg2+, K+, and HCO3), (2) wastewater production and treatment (DOC, P, N forms), (3) road de-icing (Cl and Na+), (4) atmospheric pollution (SO42−), (5) climate change (DOC), and (6) the aging of reservoirs (NH4+). The water pH increased until the early 1990s, then decreased and exhibited pronounced seasonal variations, integrating the effects of changing external acidity sources and in-lake H+ sources and sinks (i.e., microbial CO2 production/consumption and availability and transformations of inorganic N), and changes in water buffering capacity. Anthropogenic and climatic effects, reservoir aging, and changes in water eutrophication thus may significantly affect water pH also in circum-neutral systems.

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Data availability

Data are available in databases of Biology Centre CAS and will be made available on reasonable request.

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Acknowledgements

We acknowledge our colleagues and our scientific predecessors who participated in the 6-decade-long chemical monitoring of the Slapy reservoir. We thank D. W. Hardekopf for proofreading, J. Nedoma for his help with trend analysis, and Editor and an anonymous Reviewer for helpful comments. This work was supported by Grant Agency of the Czech Republic (Project No. P503/19/16605S) and ERDF/ESF Project No. CZ.02.1.01/0.0/0.0/16_025/0007417 “Biomanipulation as a tool for improving water quality of dam reservoirs”.

Funding

Grant Agency of the Czech Republic (Project No. P503/19/16605S). ERDF/ESF Project No. CZ.02.1.01/0.0/0.0/16_025/0007417 “Biomanipulation as a tool for improving water quality of dam reservoirs”.

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JK: Conceptualization, writing, water and data analyses, funding acquisition; JH: writing, water and data analyses, funding acquisition; PP: data curation, data analyses, visualization, writing; PZ: data analyses, writing.

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Correspondence to Jiří Kopáček.

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The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

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Kopáček, J., Hejzlar, J., Porcal, P. et al. Biogeochemical causes of sixty-year trends and seasonal variations of river water properties in a large European basin. Biogeochemistry 154, 81–98 (2021). https://doi.org/10.1007/s10533-021-00800-z

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  • DOI: https://doi.org/10.1007/s10533-021-00800-z

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