Fluvial organic carbon composition and concentration variability within a peatland catchment-Implications for carbon cycling and water treatment
Autor: | Martin Evans, Andrew G. Stimson, Stephen Boult, Timothy E H Allott |
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Rok vydání: | 2017 |
Předmět: |
Total organic carbon
Hydrology Peat 010504 meteorology & atmospheric sciences DOC 010501 environmental sciences Peatlands Fluvial OC transformations 01 natural sciences Carbon cycle Greenhouse gas Dissolved organic carbon Soil water Water Treatment Environmental science Water treatment Surface runoff Fluvial OC composition POC 0105 earth and related environmental sciences Water Science and Technology |
Zdroj: | Stimson, A, Allott, T E H, Boult, S & Evans, M G 2017, ' Fluvial organic carbon composition and concentration variability within a peatland catchment : implications for carbon cycling and water treatment ', Hydrological Processes . https://doi.org/10.1002/hyp.11352 |
ISSN: | 0885-6087 |
Popis: | Fluvial organic carbon (OC) transformations are an important component of carbon cycling and greenhouse gas production in inland waters resulting in considerable recent interest in the fate of fluvial OC exported from carbon rich soils such as peatlands. Additionally, peatland catchments are important drinking water collection areas, where high OC concentrations in runoff have water treatment implications. This analysis presents the results from a year-round intensive study within a water treatment catchment draining an area of peatland, considering carbon transformations along a continuum from headwater river, through a storage reservoir and pipe, to a water treatment works. The study uses a unique combination of methods (colourmetric, ultrafiltration and 14C radiocarbon dating) to assess catchment wide changes in fluvial carbon composition (colour, size and age) alongside concentration measures. The results indicate clear patterns of carbon transformations in the river and reservoir, and dissolved Low Molecular Weight (LMW) coloured carbon to be most subject to change, with both loss and replacement within the catchment residence time. Whilst the evidence suggests Dissolved OC (DOC) gains are from Particulate OC (POC) breakdown, the mechanisms of DOC loss are less certain and may represent greenhouse gas losses or conversions to POC. The transformations presented here appear to have minimal impact on the amount of harder to treat ( |
Databáze: | OpenAIRE |
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