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Please use this identifier to cite or link to this item: http://hdl.handle.net/11019/82

Title: N leaching to groundwater from dairy production involving grazing over the winter on a clay-loam soil
Authors: Necpalova, Magdalena
Fenton, Owen
Casey, I.
Humphreys, James
Keywords: extended grazing
permanent grassland
dairy production
N leaching
shallow groundwater
time lag
DNRA
Issue Date: 15-Aug-2012
Publisher: Elsevier B. V.
Citation: M. Necpalova, O. Fenton, I. Casey, J. Humphreys. N leaching to groundwater from dairy production involving grazing over the winter on a clay-loam soil, Science of The Total Environment, 432, (2012), 159-172. DOI:10.1016/j.scitotenv.2012.05.091.
Series/Report no.: Science of the Total Environment;vol 432
Abstract: This study investigated concentrations of various N species in shallow groundwater (< 2.2 m below ground level) and N losses from dairy production involving grazing over the winter period on a clay loam soil with a high natural attenuation capacity in southern Ireland (52˚51’N, 08˚21’W) over a two year period. A dense network of shallow groundwater piezometers was installed to determine groundwater flow direction and N spatial and temporal variation. Estimated vertical travel times through the unsaturated zone (<0.5 yr, time lag) allowed the correlation of management with groundwater N within a short space of time. There was a two way interaction of the system and sampling date (P < 0.05) on concentrations of DON, oxidised N and NO3--N. In contrast, concentrations of NH4+-N and NO2--N were unaffected by the dairy system. Grazing over the winter had no effect on N losses to groundwater. Mean concentrations of DON, NH4+-N, NO2--N and NO3--N were 2.16, 0.35, 0.01 and 0.37 mg L-1 respectively. Soil attenuation processes such as denitrification and DNRA resulted in increased NH4+-N levels. For this reason, DON and NH4+-N represented the highest proportion of N losses from the site. Some of the spatial and temporal variation of N concentrations was explained by correlations with selected chemical and hydro-topographical parameters (NO3--N/Cl- ratio, distance of the sampling point from the closest receptor, watertable depth, depth of sampling piezometer, DOC concentration). A high explanatory power of NO3--N/Cl- ratio and the distance of the sampling point from the closest receptor indicated the influence of point sources and groundwater-surface water interactions.
Description: peer-reviewed
URI: http://hdl.handle.net/11019/82
http://dx.doi.org/10.1016/j.scitotenv.2012.05.091
http://www.sciencedirect.com/science/article/pii/S0048969712008066
ISSN: 0048-9697
Appears in Collections:Environment, Soils & Land Use
Livestock Systems

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