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Sökning: onr:"swepub:oai:DiVA.org:kau-4672" > Spatial variation o...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003445naa a2200445 4500
001oai:DiVA.org:kau-4672
003SwePub
008090914s2008 | |||||||||||000 ||eng|
024a https://urn.kb.se/resolve?urn=urn:nbn:se:kau:diva-46722 URI
024a https://doi.org/10.1002/hyp.67792 DOI
040 a (SwePub)kau
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Andersson, Jan-Olov,d 1966-u Karlstads universitet,Avdelningen för biologi4 aut0 (Swepub:kau)janoande
2451 0a Spatial variation of wetlands and flux of dissolved organic carbon in boreal headwater streams
264 c 2008
264 1b Wiley,c 2008
338 a print2 rdacarrier
520 a In order to investigate the relation between water chemistry and functional landscape elements, spatial data sets of characteristics for 68 small (0·2–1·5 km2) boreal forest catchments in western central Sweden were analysed in a geographical information system (GIS). The geographic data used were extracted from official topographic maps. Water sampled four times at different flow situations was analysed chemically. This paper focuses on one phenomenon that has an important influence on headwater quality in boreal, coniferous forest streams: generation and export of dissolved organic carbon (DOC). It is known that wetland cover (bogs and fens) in the catchment is a major source of DOC. In this study, a comparison was made between a large number of headwater catchments with varying spatial locations and areas of wetlands. How this variation, together with a number of other spatial variables, influences the DOC flux in the streamwater was analysed by statistical methods. There were significant, but not strong, correlations between the total percentages of wetland area and DOC flux measured at a medium flow situation, but not at high flow. Neither were there any significant correlations between the percentage of wetland area connected to streams, nor the percentage of wetland area within a zone 50 m from the stream and the DOC flux. There were, however, correlations between catchment mean slope and the DOC flux in all but one flow situations. This study showed that, considering geographical data retrieved from official sources, the topography of a catchment better explains the variation in DOC flux than the percentage and locations of distinct wetland areas. This emphasizes the need for high-resolution elevation models accurate enough to reveal the sources of DOC found in headwater streams.
650 7a NATURVETENSKAPx Biologi0 (SwePub)1062 hsv//swe
650 7a NATURAL SCIENCESx Biological Sciences0 (SwePub)1062 hsv//eng
653 a boreal
653 a landscape
653 a catchment hydrology
653 a headwater streams
653 a streamwater quality
653 a DOC
653 a wetland
653 a GIS
653 a Biology
653 a Biologi
653 a Biology
653 a Biologi
700a Nyberg, Lars,d 1962-u Karlstads universitet,Centrum för klimat och säkerhet4 aut0 (Swepub:kau)larsnybe
710a Karlstads universitetb Avdelningen för biologi4 org
773t Hydrological Processesd : Wileyg :22, s. 1965-1975q :22<1965-1975x 0885-6087x 1099-1085
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:kau:diva-4672
8564 8u https://doi.org/10.1002/hyp.6779

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