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Sedimentation in Boreal Lakes: the role of flocculation of allochthonous dissolved organic matter in the water column
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Biologiska sektionen, Institutionen för ekologi och evolution, Limnologi.
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Biologiska sektionen, Institutionen för ekologi och evolution, Limnologi.ORCID-id: 0000-0003-3509-8266
2008 (engelsk)Inngår i: Ecosystems (New York. Print), ISSN 1432-9840, E-ISSN 1435-0629, Vol. 11, nr 5, s. 803-814Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

We quantified sedimentation of organic carbon in 12 Swedish small boreal lakes (< , 0.48 km(2)), which ranged in dissolved organic carbon (DOC) from 4.4 to 21.4 mg C l(-1). Stable isotope analysis suggests that most of the settling organic matter is of allochthonous origin. Annual sedimentation of allochthonous matter per m(2) lake area was correlated to DOC concentration in the water (R-2 = 0.41), and the relationship was improved when sedimentation data were normalized to water depth (R-2 = 0.58). The net efflux of C as CO2 from the water to the atmosphere was likewise correlated to DOC concentration (R-2 = 0.52). The losses of organic carbon from the water column via mineralization to CO2 and via sedimentation were approximately of equal importance throughout the year. Our results imply that DOC is a precursor of the settling matter, resulting in an important pathway in the carbon cycle of boreal lakes. Thus, flocculation of DOC of terrestrial origin and subsequent sedimentation could lead to carbon sequestration by burial in lake sediments.

sted, utgiver, år, opplag, sider
2008. Vol. 11, nr 5, s. 803-814
Emneord [en]
sedimentation, carbon cycle, DOC, flocculation, allochthonous, boreal lakes
HSV kategori
Identifikatorer
URN: urn:nbn:se:uu:diva-97913DOI: 10.1007/s10021-008-9162-zISI: 000258958700012OAI: oai:DiVA.org:uu-97913DiVA, id: diva2:173030
Tilgjengelig fra: 2008-12-17 Laget: 2008-12-17 Sist oppdatert: 2017-12-14bibliografisk kontrollert
Inngår i avhandling
1. Flocculation of Allochthonous Dissolved Organic Matter – a Significant Pathway of Sedimentation and Carbon Burial in Lakes
Åpne denne publikasjonen i ny fane eller vindu >>Flocculation of Allochthonous Dissolved Organic Matter – a Significant Pathway of Sedimentation and Carbon Burial in Lakes
2008 (engelsk)Doktoravhandling, med artikler (Annet vitenskapelig)
Abstract [en]

Inland waters receive substantial amounts of organic carbon from adjacent watersheds. Only about half of the carbon exported from inland waters reaches the oceans, while the remainder is lost en route. This thesis identifies flocculation as an important and significant fate of carbon in the boreal landscape. Flocculation reallocates organic carbon from the dissolved state into particles which are prone to settle. Thus, flocculation relocates organic carbon from the water column to the sediment.

The dissolved organic carbon (DOC), mainly originating from terrestrial sources, in a set of Swedish lakes was found to determine the extent of sedimentation of particulate organic carbon. A major fraction of the settling particles were of allochthonous origin. This implies that allochthonous DOC was the precursor of the settling matter in these lakes. The gross sedimentation was of the same magnitude as the evasion of carbon dioxide to the atmosphere.

Sunlight, especially in the photosynthetically active region, stimulated flocculation of DOC. The effect of light appeared to involve a direct photochemical reaction. Iron was involved in the flocculation but it could not be unravelled whether the iron catalyzes the flocculation or just co-precipitates with the settling matter. Microbial activity was identified as the main regulator of the flocculation rates. Accordingly, alteration of temperature, oxygen concentration and pH did not affect flocculation only indirectly, via their effects on microbial metabolism.

A comparison of fluorescence characteristics of organic matter collected in sediment trap and in the sediment surface layer revealed that autochthonous organic carbon was preferentially lost in the sediments while allochthonous matter increased. The recalcitrant nature of the flocculated matter could favour sequestration of this matter in the lake sediment. Hence, the lakes will act as sinks of organic carbon due to a slower mineralization of the flocculated matter in the sediments.

sted, utgiver, år, opplag, sider
Uppsala: Universitetsbiblioteket, 2008. s. 42
Serie
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology, ISSN 1651-6214 ; 586
Emneord
flocculation, dissolved organic carbon, allochthonous, carbon sequestration, carbon cycle, boreal lakes
HSV kategori
Identifikatorer
urn:nbn:se:uu:diva-9500 (URN)978-91-554-7374-7 (ISBN)
Disputas
2009-01-21, Ekmansalen, Kärnhuset, EBC, Norbyvägen 18, Uppsala, 10:00
Opponent
Veileder
Tilgjengelig fra: 2008-12-17 Laget: 2008-12-17 Sist oppdatert: 2016-04-28bibliografisk kontrollert

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