Aged riverine particulate organic carbon in four UK catchments

Adams, Jessica L.; Tipping, Edward ORCID: https://orcid.org/0000-0001-6618-6512; Bryant, Charlotte L.; Helliwell, Rachel C.; Toberman, Hannah; Quinton, John. 2015 Aged riverine particulate organic carbon in four UK catchments. Science of the Total Environment, 536. 648-654. https://doi.org/10.1016/j.scitotenv.2015.06.141

Before downloading, please read NORA policies.

Preview

Text
N511976PP.pdf - Accepted Version
Download (406kB) | Preview

Official URL: http://dx.doi.org/10.1016/j.scitotenv.2015.06.141

Abstract/Summary

The riverine transport of particulate organic matter (POM) is a significant flux in the carbon cycle, and affects macronutrients and contaminants. We used radiocarbon to characterise POM in 9 rivers of four UK catchments (Avon, Conwy, Dee, Ribble) over a one-year period. High-discharge samples were collected on three or four occasions at each site. Suspended particulate matter (SPM) was obtained by centrifugation, and the samples were analysed for carbon isotopes. Concentrations of SPM and SPM organic carbon (OC) contents were also determined, and were found to have a significant negative correlation. For the 7 rivers draining predominantly rural catchments, PO14C values, expressed as percent modern carbon absolute (pMC), varied little among samplings at each site, and there was no significant difference in the average values among the sites. The overall average PO14C value for all 7 sites of 91.2 pMC corresponded to an average age of 680 14C years, but this value arises from the mixing of differently-aged components, and therefore significant amounts of organic matter older than the average value are present in the samples. Although topsoil erosion is probably the major source of the riverine POM, the average PO14C value is appreciably lower than topsoil values (which are typically 100 pMC). This is most likely explained by inputs of older subsoil OC from bank erosion, or the preferential loss of high-14C topsoil organic matter by mineralisation during riverine transport. The significantly lower average PO14C of samples from the River Calder (76.6 pMC), can be ascribed to components containing little or no radiocarbon, derived either from industrial sources or historical coal mining, and this effect is also seen in the River Ribble, downstream of its confluence with the Calder. At the global scale, the results significantly expand available information for PO14C in rivers draining catchments with low erosion rates.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1016/j.scitotenv.2015.06.141
UKCEH and CEH Sections/Science Areas:	Shore
ISSN:	0048-9697
Additional Keywords:	particulate organic carbon, radiocarbon, rivers, soils
NORA Subject Terms:	Ecology and Environment
Date made live:	21 Oct 2015 14:00 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/511976

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1016/j.scitotenv.2015.06.141

UKCEH and CEH Sections/Science Areas:

Shore

ISSN:

0048-9697

Additional Keywords:

particulate organic carbon, radiocarbon, rivers, soils

NORA Subject Terms:

Ecology and Environment