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- W2017230157 abstract "Two tributary streams arise from a small forested catchment in the north of Sweden. The subcatchments of both tributaries, which were deepened half a century ago to improve forest drainage, appear outwardly similar. Between July and November 1990, however, one tributary had a specific output of organic C from its subcatchment of 2.8 g/m2. That was 50% greater than the output from the other tributary and similar to the specific output from the mire (3.1 g/m2) at the head of the catchment. The pH, the C/color relationship, the ratio of hydrophilic to hydrophobic organic substances, Al concentration and speciation all differed markedly in the runoff from the two tributaries. Detailed hillslope investigations suggested that the differences in the organic C output from the two tributaries were related to differences in their riparian soils. The tributary with the lower export of organics was routed just to the side of a wetland, while the tributary with the higher export of organics went through a small wetland. In this wetland, forest drainage created a relict peat perched above the hillslope flow pathways which passed beneath that peat. Soil solution under the relict peat had high concentrations of organic C and polymeric Al even at a depth of 40–50 cm. Farther up the slope where the soil is more podzolized, such large concentrations of TOC and Al were not found below the illuvial layer (i.e. below ~15 cm depth)." @default.
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- W2017230157 date "1993-01-01" @default.
- W2017230157 modified "2023-09-24" @default.
- W2017230157 title "Transfer of organic C from forest soils to surface waters: example from northern Sweden" @default.
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- W2017230157 doi "https://doi.org/10.1016/s0883-2927(09)80003-6" @default.
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