Groundwater quality in rural watersheds with environmental land
use conflicts
R.F. Valle Junior
a,b
, S.G.P. Varandas
b
, L.F. Sanches Fernandes
b
, F.A.L. Pacheco
c,
⁎
a
IFTM – Instituto Federal do Triangulo Mineiro, Campus Uberaba, Uberaba, MG, Brazil
b
CITAB-UTAD – Centre for Research and Technology of Agro-Environment and Biological Sciences, University of Trás-os-Montes e Alto Douro, Quinta de Prados, 5001-801 Vila Real, Portugal
c
DG-CQVR-UTAD – Department of Geology and Chemistry Research Centre, University of Trás-os-Montes e Alto Douro, Quinta de Prados, 5001-801 Vila Real, Portugal
HIGHLIGHTS
• Conceive environmental land use conflicts (LUC) in rural watersheds
• Investigate groundwater quality in watersheds with LUC
• Investigate environmental implications of LUC
abstract article info
Article history:
Received 16 April 2014
Received in revised form 16 June 2014
Accepted 16 June 2014
Available online xxxx
Editor: D. Barcelo
Keywords:
Groundwater quality
Land capability
Land use conflict
Nitrification
Rural watershed
The quality of groundwater was evaluated in a rural watershed of northern Portugal (River Sordo basin) where
environmental land use conflicts have developed in the course of a progressive invasion of forest and pasture
lands by agriculture, especially by vineyards. The selected groundwater quality parameters were the concentra-
tions of sodium, calcium, bicarbonate, chloride and nitrates, derived from natural and anthropogenic sources. The
environmental land use conflicts were revealed by the coupling of land use and land capability raster maps. The
land capability evaluation allocated 70.3% of the basin to the practicing of agriculture, 20% to livestock pasturing
and 9.7% to a mosaic of land uses including agriculture, livestock pasturing and forestry. The assessment of land
use conflicts allocated 93.9% of the basin to no conflict areas. Minor conflict areas (4.1%) were found concentrated
in the western region of the watershed. They correspond to an invasion of farmlands towards sectors of the catch-
ment capable for the practicing of livestock pasturing. Moderate (1.6%) and major (0.4%) conflict areas were
found limited to the eastern region, matching steep hillsides capable for the practicing of livestock pasturing or
forestry but presently occupied with vineyards. The spatial distributions of ion concentrations were generally
justified by common geochemical processes. The dominance of high concentration levels in moderate and
major conflict areas was justified within the framework of nutrient dynamics in vineyard environment. Nitrate
in groundwater was likewise produced via the nitrification of N-fertilizers. Apparently, this process promoted
the weathering of plagioclase by the nitric acid reaction, in concurrence with the weathering by the carbonic
acid reaction. The impact of nitrification was found more important in moderate and major conflict areas, relative
to no conflict areas.
© 2014 Elsevier B.V. All rights reserved.
1. Introduction
Groundwater contamination in rural areas is controlled by numer-
ous factors, including the use of the land. For example, in a county of
China nitrate concentrations in groundwater were found to be higher
in areas used for rotating irrigated cultures, in comparison with areas
occupied by forests where a fast-growing tree system could act as buffer
to retain the nitrate content (Chen et al., 2010). Another example is
reported in Korea, where increasing nitrate concentrations were found
to occur in cropping areas, cropping-livestock farming complex areas,
and residential areas (Choi et al., 2007). The scenario of groundwater
contamination changes as land use changes in space and time. An exam-
ple supporting this statement comes from the Neal Smith National
Wildlife Refuge, Iowa, USA, where the conversion of cropland to peren-
nial land cover (prairie) resulted in a significant drop of nitrate and
chloride concentrations in groundwater within a decade (Schilling
and Jacobson, 2010). Another example comes from the region of Fife,
Scotland, where the nitrate concentrations in public borehole water
more than doubled in three decades, because the pumped sandstone
aquifer is recharged by water draining from a land that is intensively
Science of the Total Environment 493 (2014) 812–827
⁎ Corresponding author. Tel.: +351 259 350 280; fax: +351 259 350 480.
E-mail address: fpacheco@utad.pt (F.A.L. Pacheco).
URL: http://www.utad.pt (F.A.L. Pacheco).
http://dx.doi.org/10.1016/j.scitotenv.2014.06.068
0048-9697/© 2014 Elsevier B.V. All rights reserved.
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