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dc.contributor.authorGrand-Clement, Emilie
dc.contributor.authorLuscombe, David J.
dc.contributor.authorAnderson, K
dc.contributor.authorGatis, Naomi
dc.contributor.authorBenaud, P
dc.contributor.authorBrazier, Richard E.
dc.date.accessioned2015-04-21T14:43:26Z
dc.date.accessioned2015-04-21T14:50:18Z
dc.date.issued2014-09-15
dc.description.abstractLosses of dissolved organic carbon (DOC) from drained peatlands are of concern, due to the effects this has on the delivery of ecosystem services, and especially on the long-term store of carbon and the provision of drinking water. Most studies have looked at the effect of drainage in deep peat; comparatively, little is known about the behaviour of shallow, climatically marginal peatlands. This study examines water quality (DOC, Abs(400), pH, E4/E6 and C/C) during rainfall events from such environments in the south west UK, in order to both quantify DOC losses, and understand their potential for restoration. Water samples were taken over a 19 month period from a range of drains within two different experimental catchments in Exmoor National Park; data were analysed on an event basis. DOC concentrations ranging between 4 and 21 mg L(-1) are substantially lower than measurements in deep peat, but remain problematic for the water treatment process. Dryness plays a critical role in controlling DOC concentrations and water quality, as observed through spatial and seasonal differences. Long-term changes in depth to water table (30 days before the event) are likely to impact on DOC production, whereas discharge becomes the main control over DOC transport at the time scale of the rainfall/runoff event. The role of temperature during events is attributed to an increase in the diffusion of DOC, and therefore its transport. Humification ratios (E4/E6) consistently below 5 indicate a predominance of complex humic acids, but increased decomposition during warmer summer months leads to a comparatively higher losses of fulvic acids. This work represents a significant contribution to the scientific understanding of the behaviour and functioning of shallow damaged peatlands in climatically marginal locations. The findings also provide a sound baseline knowledge to support research into the effects of landscape restoration in the future.en_GB
dc.description.sponsorshipNatural Environment Research Council (NERC)
dc.description.sponsorshipSouth West Water
dc.description.sponsorshipKnowledge Transfer Partnership
dc.identifier.citationVol. 493, pp. 961 - 973en_GB
dc.identifier.doi10.1016/j.scitotenv.2014.06.091
dc.identifier.grantnumberKTP ID 8099
dc.identifier.grantnumberSK04823
dc.identifier.otherS0048-9697(14)00964-4
dc.identifier.urihttp://hdl.handle.net/10871/16940
dc.language.isoenen_GB
dc.publisherElsevieren_GB
dc.relation.replaceshttp://hdl.handle.net/10871/16939
dc.relation.replaces10871/16939
dc.relation.urlhttp://www.ncbi.nlm.nih.gov/pubmed/25010944en_GB
dc.rightsCC-BY
dc.subjectDOCen_GB
dc.subjectDrainageen_GB
dc.subjectDroughten_GB
dc.subjectE4/E6en_GB
dc.subjectExmooren_GB
dc.subjectWater qualityen_GB
dc.titleAntecedent conditions control carbon loss and downstream water quality from shallow, damaged peatlands.en_GB
dc.typeArticleen_GB
dc.date.available2015-04-21T14:43:26Z
dc.date.available2015-04-21T14:50:18Z
dc.identifier.issn0048-9697
exeter.place-of-publicationNetherlands
dc.descriptionJournal Articleen_GB
dc.descriptionResearch Support, Non-U.S. Gov'ten_GB
dc.description© 2014 Published by Elsevier B.V.en_GB
dc.descriptionThis is an open access article that is freely available in ORE or from the publisher's web site. Please cite the published version doi:10.1016/j.scitotenv.2014.06.091en_GB
dc.identifier.journalScience of the Total Environmenten_GB


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