Flocculated meltwater particles control Arctic land-sea fluxes of labile iron

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Standard

Flocculated meltwater particles control Arctic land-sea fluxes of labile iron. / Markussen, Thor Nygaard; Elberling, Bo; Winter, Christian; Andersen, Thorbjørn Joest.

I: Scientific Reports, Bind 6, 24033, 06.04.2016.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Markussen, TN, Elberling, B, Winter, C & Andersen, TJ 2016, 'Flocculated meltwater particles control Arctic land-sea fluxes of labile iron', Scientific Reports, bind 6, 24033. https://doi.org/10.1038/srep24033

APA

Markussen, T. N., Elberling, B., Winter, C., & Andersen, T. J. (2016). Flocculated meltwater particles control Arctic land-sea fluxes of labile iron. Scientific Reports, 6, [24033]. https://doi.org/10.1038/srep24033

Vancouver

Markussen TN, Elberling B, Winter C, Andersen TJ. Flocculated meltwater particles control Arctic land-sea fluxes of labile iron. Scientific Reports. 2016 apr. 6;6. 24033. https://doi.org/10.1038/srep24033

Author

Markussen, Thor Nygaard ; Elberling, Bo ; Winter, Christian ; Andersen, Thorbjørn Joest. / Flocculated meltwater particles control Arctic land-sea fluxes of labile iron. I: Scientific Reports. 2016 ; Bind 6.

Bibtex

@article{27bd6b826117458b8dd1c09d13a41869,
title = "Flocculated meltwater particles control Arctic land-sea fluxes of labile iron",
abstract = "Glacial meltwater systems supply the Arctic coastal ocean with large volumes of sediment and potentially bioavailable forms of iron, nitrogen and carbon. The particulate fraction of this supply is significant but estuarine losses have been thought to limit the iron supply from land. Here, our results reveal how flocculation (particle aggregation) involving labile iron may increase horizontal transport rather than enhance deposition close to the source. This is shown by combining field observations in Disko Fjord, West Greenland, and laboratory experiments. Our data show how labile iron affects floc sizes, shapes and densities and consequently yields low settling velocities and extended sediment plumes. We highlight the importance of understanding the flocculation mechanisms when examining fluxes of meltwater transported iron in polar regions today and in the future, and we underline the influence of terrestrial hotspots on the nutrient and solute cycles in Arctic coastal waters.",
author = "Markussen, {Thor Nygaard} and Bo Elberling and Christian Winter and Andersen, {Thorbj{\o}rn Joest}",
note = "CENPERMOA[2016]",
year = "2016",
month = apr,
day = "6",
doi = "10.1038/srep24033",
language = "English",
volume = "6",
journal = "Scientific Reports",
issn = "2045-2322",
publisher = "nature publishing group",

}

RIS

TY - JOUR

T1 - Flocculated meltwater particles control Arctic land-sea fluxes of labile iron

AU - Markussen, Thor Nygaard

AU - Elberling, Bo

AU - Winter, Christian

AU - Andersen, Thorbjørn Joest

N1 - CENPERMOA[2016]

PY - 2016/4/6

Y1 - 2016/4/6

N2 - Glacial meltwater systems supply the Arctic coastal ocean with large volumes of sediment and potentially bioavailable forms of iron, nitrogen and carbon. The particulate fraction of this supply is significant but estuarine losses have been thought to limit the iron supply from land. Here, our results reveal how flocculation (particle aggregation) involving labile iron may increase horizontal transport rather than enhance deposition close to the source. This is shown by combining field observations in Disko Fjord, West Greenland, and laboratory experiments. Our data show how labile iron affects floc sizes, shapes and densities and consequently yields low settling velocities and extended sediment plumes. We highlight the importance of understanding the flocculation mechanisms when examining fluxes of meltwater transported iron in polar regions today and in the future, and we underline the influence of terrestrial hotspots on the nutrient and solute cycles in Arctic coastal waters.

AB - Glacial meltwater systems supply the Arctic coastal ocean with large volumes of sediment and potentially bioavailable forms of iron, nitrogen and carbon. The particulate fraction of this supply is significant but estuarine losses have been thought to limit the iron supply from land. Here, our results reveal how flocculation (particle aggregation) involving labile iron may increase horizontal transport rather than enhance deposition close to the source. This is shown by combining field observations in Disko Fjord, West Greenland, and laboratory experiments. Our data show how labile iron affects floc sizes, shapes and densities and consequently yields low settling velocities and extended sediment plumes. We highlight the importance of understanding the flocculation mechanisms when examining fluxes of meltwater transported iron in polar regions today and in the future, and we underline the influence of terrestrial hotspots on the nutrient and solute cycles in Arctic coastal waters.

U2 - 10.1038/srep24033

DO - 10.1038/srep24033

M3 - Journal article

C2 - 27050673

VL - 6

JO - Scientific Reports

JF - Scientific Reports

SN - 2045-2322

M1 - 24033

ER -

ID: 167888265