Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

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Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation. / Asmala, E.; Bowers, D.G.; Autio, R. et al.
Yn: Journal of Geophysical Research: Biogeosciences, Cyfrol 119, Rhif 10, 10.2014, t. 1919-1933.

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

HarvardHarvard

Asmala, E, Bowers, DG, Autio, R, Kaartokallio, H & Thomas, DN 2014, 'Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation', Journal of Geophysical Research: Biogeosciences, cyfrol. 119, rhif 10, tt. 1919-1933. https://doi.org/10.1002/2014JG002722

APA

Asmala, E., Bowers, D. G., Autio, R., Kaartokallio, H., & Thomas, D. N. (2014). Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation. Journal of Geophysical Research: Biogeosciences, 119(10), 1919-1933. https://doi.org/10.1002/2014JG002722

CBE

Asmala E, Bowers DG, Autio R, Kaartokallio H, Thomas DN. 2014. Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation. Journal of Geophysical Research: Biogeosciences. 119(10):1919-1933. https://doi.org/10.1002/2014JG002722

MLA

Asmala, E. et al. "Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation". Journal of Geophysical Research: Biogeosciences. 2014, 119(10). 1919-1933. https://doi.org/10.1002/2014JG002722

VancouverVancouver

Asmala E, Bowers DG, Autio R, Kaartokallio H, Thomas DN. Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation. Journal of Geophysical Research: Biogeosciences. 2014 Hyd;119(10):1919-1933. Epub 2014 Hyd 2. doi: 10.1002/2014JG002722

Author

Asmala, E. ; Bowers, D.G. ; Autio, R. et al. / Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation. Yn: Journal of Geophysical Research: Biogeosciences. 2014 ; Cyfrol 119, Rhif 10. tt. 1919-1933.

RIS

TY - JOUR

T1 - Qualitative changes of riverine dissolved organic matter at low salinities due to flocculation

AU - Asmala, E.

AU - Bowers, D.G.

AU - Autio, R.

AU - Kaartokallio, H.

AU - Thomas, D.N.

PY - 2014/10

Y1 - 2014/10

N2 - The flocculation of dissolved organic matter (DOM) was studied along transects through three boreal estuaries. Besides the bulk concentration parameters, a suite of DOM quality parameters were investigated, including colored DOM (CDOM), fluorescent DOM, and the molecular weight of DOM as well as associated dissolved iron concentrations. We observed significant deviations from conservative mixing at low salinities (0.2 µm) and thereby removing them from the dissolved phase. We also measured flocculation of CDOM, especially in the UV region of the absorption spectrum. Protein-like fluorescence of DOM decreased, while humic-like fluorescence increased because of salt-induced flocculation. Additionally, there was a decrease in molecular weight of DOM. Consequently, the quantity and quality of the remaining DOM pool was significantly changed after influenced to flocculation. Based on these results, we constructed a mechanistic, two-component flocculation model. Our findings underline the importance of the coastal filter, where riverine organic matter is flocculated and exported to the sediments.

AB - The flocculation of dissolved organic matter (DOM) was studied along transects through three boreal estuaries. Besides the bulk concentration parameters, a suite of DOM quality parameters were investigated, including colored DOM (CDOM), fluorescent DOM, and the molecular weight of DOM as well as associated dissolved iron concentrations. We observed significant deviations from conservative mixing at low salinities (0.2 µm) and thereby removing them from the dissolved phase. We also measured flocculation of CDOM, especially in the UV region of the absorption spectrum. Protein-like fluorescence of DOM decreased, while humic-like fluorescence increased because of salt-induced flocculation. Additionally, there was a decrease in molecular weight of DOM. Consequently, the quantity and quality of the remaining DOM pool was significantly changed after influenced to flocculation. Based on these results, we constructed a mechanistic, two-component flocculation model. Our findings underline the importance of the coastal filter, where riverine organic matter is flocculated and exported to the sediments.

U2 - 10.1002/2014JG002722

DO - 10.1002/2014JG002722

M3 - Article

VL - 119

SP - 1919

EP - 1933

JO - Journal of Geophysical Research: Biogeosciences

JF - Journal of Geophysical Research: Biogeosciences

SN - 2169-8961

IS - 10

ER -