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Sammanfattning

Stable Fe isotope compositions have been measured in water samples of the subarctic Kalix River, a first-order stream, and soil water samples from a riparian soil profile adjacent to the first-order stream (Northern Sweden). In the first-order stream, dominated by forest, both the particulate (>0.22 mu m) and dissolved (

Nyckelord

Fe aggregates; Fe isotope; soilwater; Krycklan Catchment; first-order stream; snowmelt; spring flood

Publicerad i

Geochimica et Cosmochimica Acta
2018, volym: 239, sidor: 49-60
Utgivare: PERGAMON-ELSEVIER SCIENCE LTD

SLU författare

UKÄ forskningsämne

Geokemi

Publikationens identifierare

  • DOI: https://doi.org/10.1016/j.gca.2018.07.030

Permanent länk till denna sida (URI)

https://res.slu.se/id/publ/96622