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Anneli Ågren

Researcher at Swedish University of Agricultural Sciences

Publications -  49
Citations -  3231

Anneli Ågren is an academic researcher from Swedish University of Agricultural Sciences. The author has contributed to research in topics: Soil water & Environmental science. The author has an hindex of 26, co-authored 39 publications receiving 2647 citations. Previous affiliations of Anneli Ågren include Umeå University.

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Patterns and dynamics of dissolved organic carbon (DOC) in boreal streams: The role of processes, connectivity, and scaling

TL;DR: In this article, the Krycklan Catchment Study was used to study the role of hydrological mechanisms, connectivity and scaling for understanding the pattern and dynamics of surface water DOC across complex landscapes.
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Role of lakes for organic carbon cycling in the boreal zone

TL;DR: In this paper, the authors calculated the carbon loss (mineralization plus sedimentation) and net CO2 escape to the atmosphere for 79,536 lakes and total running water in 21 major Scandinavian catchments.
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The Krycklan Catchment Study—A flagship infrastructure for hydrology, biogeochemistry, and climate research in the boreal landscape

TL;DR: The Krycklan Catchment Study (KCS) as mentioned in this paper provides a unique field infrastructure for hillslope to landscape-scale research on short and long-term ecosystem dynamics in boreal landscapes.
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Evasion of CO2 from streams - the dominant component of the carbon export through the aquatic conduit in a boreal landscape.

TL;DR: It is shown that evasion of C is greater than all the total dissolved C exported downstream in the waters of a boreal landscape as it more than doubled the magnitude of the aquatic conduit for C from this landscape.
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Dissolved organic carbon characteristics in boreal streams in a forest-wetland gradient during the transition between winter and summer

TL;DR: In this article, the character and quantity of dissolved organic carbon (DOC) were studied in nine small boreal streams and adjacent soils during two years, with focus on the spring snowmelt period.