dc.contributor.author
Juhls, Bennet
dc.contributor.author
Stedmon, Colin A.
dc.contributor.author
Morgenstern, Anne
dc.contributor.author
Meyer, Hanno
dc.contributor.author
Hölemann, Jens
dc.contributor.author
Heim, Birgit
dc.contributor.author
Povazhnyi, Vasily
dc.contributor.author
Overduin, Pier P.
dc.date.accessioned
2020-05-15T11:57:33Z
dc.date.available
2020-05-15T11:57:33Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/27518
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-27274
dc.description.abstract
Warming air temperatures, shifting hydrological regimes and accelerating permafrost thaw in the catchments of the Arctic rivers is affecting their biogeochemistry. Arctic river monitoring is necessary to observe changes in the mobilization of dissolved organic matter (DOM) from permafrost. The Lena River is the second largest Arctic river and 71% of its catchment is continuous permafrost. Biogeochemical parameters, including temperature, electrical conductivity (EC), stable water isotopes, dissolved organic carbon (DOC) and absorption by colored dissolved organic matter (aCDOM) have been measured as part of a new high-frequency sampling program in the central Lena River Delta. The results show strong seasonal variations of all biogeochemical parameters that generally follow seasonal patterns of the hydrograph. Optical indices of DOM indicate a trend of decreasing aromaticity and molecular weight from spring to winter. High-frequency sampling improved our estimated annual fluvial flux of annual dissolved organic carbon flux (6.79 Tg C). EC and stable isotope data were used to distinguish three different source water types which explain most of the seasonal variation in the biogeochemistry of the Lena River. These water types match signatures of (1) melt water, (2) rain water, and (3) subsurface water. Melt water and rain water accounted for 84% of the discharge flux and 86% of the DOC flux. The optical properties of melt water DOM were characteristic of fresh organic matter. In contrast, the optical properties of DOM in subsurface water revealed lower aromaticity and lower molecular weights, which indicate a shift toward an older organic matter source mobilized from deeper soil horizons or permafrost deposits. The first year of this new sampling program sets a new baseline for flux calculations of dissolved matter and has enabled the identification and characterization of water types that drive the seasonality of the Lena River water properties.
en
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
optical indices
en
dc.subject
stable water isotopes
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::550 Geowissenschaften
dc.title
Identifying Drivers of Seasonality in Lena River Biogeochemistry and Dissolved Organic Matter Fluxes
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation
10.3389/fenvs.2020.00053
dcterms.bibliographicCitation.articlenumber
53
dcterms.bibliographicCitation.doi
10.3389/fenvs.2020.00053
dcterms.bibliographicCitation.journaltitle
Frontiers in Environmental Science
dcterms.bibliographicCitation.volume
8
dcterms.bibliographicCitation.url
https://doi.org/10.3389/fenvs.2020.00053
refubium.affiliation
Geowissenschaften
refubium.affiliation.other
Institut für Weltraumwissenschaften
refubium.note.author
Die Publikation wurde aus Open Access Publikationsgeldern der Freien Universität Berlin gefördert.
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.eissn
2296-665X
dcterms.isPartOf.zdb
2741535-1