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Water chemistry and its diversity in relation to local factors in the Latnjavagge drainage basin, arctic–oceanic Swedish Lapland
Ansvarlig organisasjon
2004 (engelsk)Inngår i: Geomorphology, ISSN 0169-555X, E-ISSN 1872-695X, Vol. 58, nr 1, s. 125-143Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The chemistry of precipitation, snow pack and surface water has been analysed on 205 samples collected during the 2001 field season at 25 selected sites within the Latnjavagge drainage basin in arctic–oceanic northern Swedish Lapland. Additionally, daily discharge and yield of dissolved solids have been calculated for several subcatchments and the entire Latnjavagge catchment during the years 2000, 2001 and 2002. Chemical water analysis included the components Ca2+, Mg2+, Na+, K+, Fe2+, Mn2+, Cl−, NO3−, SO42− and PO43−, with SO42− and Ca2+ being the dominant ones in the surface water. Solute concentrations and chemical denudation were low, but showed significant differences within the basin. In areas of shade, longer snow cover, frozen ground and thin regolith, concentrations over the summer were perceptible but so low that solutes brought into the basin from precipitation could be detected in the surface water. In one locality, it was even found that lake water could reflect snowmelt to such an extent that the solute concentration was less than that of summer precipitation. The highest concentrations were found at a radiation-exposed, W-facing, vegetated, moderately steep slope with relatively thick regolith that was thawed at the time of snowmelt in early June. In such well-drained sites with continuous subsurface water flow, a maximum of contact between water and mineral particles could take place. The concentration values revealed differences in the rate of thawing of frozen ground between shaded areas and/or areas at higher altitude on the one hand and radiation-exposed areas on the other. A comparison with published results from Kärkevagge a few kilometres to the northwest as well as from other periglacial locations indicates that the chemical denudation values from Latnjavagge are more representative of periglacial oceanic environments than the values from the Kärkevagge catchment, which shows especially high chemical denudation rates. The investigation in Latnjavagge stresses the importance of spatial variability within even small catchments of homogeneous lithology as it demonstrates that solute concentrations from different subbasins can differ substantially dependent on exposure to radiation, duration of snow cover and frozen ground conditions, regolith thickness and possibly also to vegetation cover and slope angle as factors steering water turbulence and retention of drainage.

sted, utgiver, år, opplag, sider
Elsevier, 2004. Vol. 58, nr 1, s. 125-143
Emneord [en]
Water chemistry, Chemical denudation, Spatial variability, Periglacial, Arctic–oceanic, Lapland
HSV kategori
Identifikatorer
URN: urn:nbn:se:polar:diva-8568DOI: 10.1016/S0169-555X(03)00228-9OAI: oai:DiVA.org:polar-8568DiVA, id: diva2:1518754
Tilgjengelig fra: 2021-01-17 Laget: 2021-01-17 Sist oppdatert: 2021-01-17bibliografisk kontrollert

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