TY - JOUR

T1 - Aged riverine particulate organic carbon in four UK catchments

AU - Adams, Jessica L.

AU - Tipping, Edward

AU - Bryant, Charlotte L.

AU - Helliwell, Rachel C.

AU - Toberman, Hannah

AU - Quinton, John

PY - 2015/12/1

Y1 - 2015/12/1

N2 - 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 at 9 riverine sites 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, (POC)-C-14 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 (POC)-C-14 value for the 7 sites of 91.2 pMC corresponded to an average age of 680 C-14 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 (POC)-C-14 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-C-14 topsoil organic matter by mineralisation during riverine transport. The significantly lower average (POC)-C-14 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 (POC)-C-14 in rivers draining catchments with low erosion rates. (C) 2015 Elsevier B.V. All rights reserved.

AB - 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 at 9 riverine sites 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, (POC)-C-14 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 (POC)-C-14 value for the 7 sites of 91.2 pMC corresponded to an average age of 680 C-14 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 (POC)-C-14 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-C-14 topsoil organic matter by mineralisation during riverine transport. The significantly lower average (POC)-C-14 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 (POC)-C-14 in rivers draining catchments with low erosion rates. (C) 2015 Elsevier B.V. All rights reserved.

KW - Particulate organic carbon

KW - Radiocarbon

KW - Rivers

KW - Soils

KW - PHOSPHORUS TRANSPORT

KW - SEDIMENT SOURCES

KW - LAND-USE

KW - MATTER

KW - C-14

KW - RADIOCARBON

KW - TEMPERATE

KW - SYSTEMS

KW - SOIL

KW - PROFILES

U2 - 10.1016/j.scitotenv.2015.06.141

DO - 10.1016/j.scitotenv.2015.06.141

M3 - Journal article

VL - 536

SP - 648

EP - 654

JO - Science of the Total Environment

JF - Science of the Total Environment

SN - 0048-9697

ER -