Groundwater nitrogen composition and transformation within a moorland catchment, mid-Wales

Lapworth, D. J. ORCID: https://orcid.org/0000-0001-7838-7960; Shand, P.; Abesser, C.; Darling, W. G.; Haria, A. H.; Evans, C. D. ORCID: https://orcid.org/0000-0002-7052-354X; Reynolds, B.. 2008 Groundwater nitrogen composition and transformation within a moorland catchment, mid-Wales. Science of the Total Environment, 390 (1). 241-254. https://doi.org/10.1016/j.scitotenv.2007.09.043

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Official URL: http://dx.doi.org/10.1016/j.scitotenv.2007.09.043

Abstract/Summary

The importance of upland groundwater systems in providing a medium for nitrogen transformations and processes along flow paths is investigated within the Afon Gwy moorland catchment, Plynlimon, mid-Wales. Dissolved organic nitrogen (DON) was found to be the most abundant form of dissolved nitrogen (N) in most soils and groundwaters, accounting for between 47 and 72% of total dissolved nitrogen in shallow groundwater samples and up to 80% in deeper groundwaters. Groundwater DON may also be an important source of bio-available N in surface waters and marine systems fed by upland catchments. A conceptual model of N processes is proposed based on a detailed study along a transect of nested boreholes and soil suction samplers within the interfluve zone. Shallow groundwater N speciation reflects the soilwater N speciation implying a rapid transport mechanism and good connectivity between the soil and groundwater systems. Median nitrate concentrations were an order of magnitude lower within the soil zone (< 5–31 μg/L) than in the shallow groundwaters (86–746 μg/L). Given the rapid hydrostatic response of the groundwater level within the soil zone, the shallow groundwater system is both a source and sink for dissolved N. Results from dissolved N2O, N2/Ar ratios and dissolved N chemistry suggests that microbial N transformations (denitrification and nitrification) may play an important role in controlling the spatial variation in soil and groundwater N speciation. Reducing conditions within the groundwater and saturated soils of the wet-flush zones on the lower hillslopes, a result of relatively impermeable drift deposits, are also important in controlling N speciation and transformation processes.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1016/j.scitotenv.2007.09.043
Programmes:	CEH Programmes pre-2009 publications > Biogeochemistry BGS Programmes 2008 > Groundwater resources
UKCEH and CEH Sections/Science Areas:	Emmett Harding (to July 2011)
ISSN:	0048-9697
Additional Keywords:	Dissolved Organic Nitrogen (DON), Groundwater, Denitrification, Nitrification, Nitrate, Transformations, Upland catchments
NORA Subject Terms:	Ecology and Environment Hydrology
Date made live:	09 Jan 2008 11:50 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/1745

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1016/j.scitotenv.2007.09.043

Programmes:

CEH Programmes pre-2009 publications > Biogeochemistry
BGS Programmes 2008 > Groundwater resources

UKCEH and CEH Sections/Science Areas:

Emmett
Harding (to July 2011)

ISSN:

0048-9697

Additional Keywords:

Dissolved Organic Nitrogen (DON), Groundwater, Denitrification, Nitrification, Nitrate, Transformations, Upland catchments