The dynamics of natural pipe hydrological behaviour in blanket peat

Smart, R.P.; Holden, J.; Dinsmore, K.J.; Baird, A.J.; Billett, M.F.; Chapman, P.J.; Grayson, R.. 2013 The dynamics of natural pipe hydrological behaviour in blanket peat. Hydrological Processes, 27 (11). 1523-1534. https://doi.org/10.1002/hyp.9242

Full text not available from this repository.

Abstract/Summary

Natural soil pipes are found in peatlands, but little is known about their hydrological role. This paper presents the most complete set of pipe discharge data to date from a deep blanket peatland in Northern England. In a 17.4-ha catchment, we identified 24 perennially flowing and 60 ephemerally flowing pipe outlets. Eight pipe outlets along with the catchment outlet were continuously gauged over an 18-month period. The pipes in the catchment were estimated to produce around 13.7% of annual streamflow, with individual pipes often producing large peak flows (maximum peak of 3.8 l s−1). Almost all pipes, whether ephemerally or perennially flowing, shallow or deep (outlets > 1 m below the peat surface), showed increased discharge within a mean of 3 h after rainfall commencement and were dominated by stormflow, indicating good connectivity between the peatland surface and the pipes. However, almost all pipes had a longer period between the hydrograph peak and the return to base flow compared with the stream (mean of 23.9 h for pipes, 19.7 h for stream). As a result, the proportion of streamflow produced by the pipes at any given time increased at low flows and formed the most important component of stream discharge for the lowest 10% of flows. Thus, a small number of perennially flowing pipes became more important to the stream system under low-flow conditions and probably received water via matrix flow during periods between storms. Given the importance of pipes to streamflow in blanket peatlands, further research is required into their wider role in influencing stream water chemistry, water temperature and fluvial carbon fluxes, as well as their role in altering local hydrochemical cycling within the peat mass itself. Enhanced piping within peatlands caused by environmental change may lead to changes in the streamflow regime with larger low flows and more prolonged drainage of the peat.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1002/hyp.9242
Programmes:	CEH Topics & Objectives 2009 - 2012 > Biogeochemistry > BGC Topic 2 - Biogeochemistry and Climate System Processes CEH Topics & Objectives 2009 - 2012 > Biogeochemistry CEH Topics & Objectives 2009 - 2012 > Water
UKCEH and CEH Sections/Science Areas:	Billett (to November 2013)
ISSN:	0885-6087
Additional Keywords:	peatland, pipes, piping, pipe flow, tunnel erosion, peatlands, Environmental Change Network
NORA Subject Terms:	Ecology and Environment
Date made live:	04 Jun 2014 10:44 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/506532

Actions (login required)

View Item

Document Downloads

More statistics for this item...