Ecological Indicators 48 (2015) 396–407
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Ecological Indicators
jo ur nal ho me page: www.elsevier.com/locate/ ecolind
Assessing the impact of agricultural pressures on N and P loads and
eutrophication risk
Rémi Dupas
a,b,∗
, Magalie Delmas
c
, Jean-Marcel Dorioz
d
, Josette Garnier
e
,
Florentina Moatar
f
, Chantal Gascuel-Odoux
a,b
a
INRA, UMR1069, Sol Agro and hydroSystem, F-35000 Rennes, France
b
Agrocampus Ouest, Sol Agro and hydroSystem, F-35000 Rennes, France
c
INRA, Infosol, F-45075 Orléans, France
d
INRA, UMR Carrtel, F74203 BP 11 Thonon les bains, France
e
CNRS, Univ Paris 06, UMR Sisyphe 7619, F-75252 Paris, France
f
Univ Tours, Fac Sci & Tech, EA 6293, F-37200 Tours, France
a r t i c l e i n f o
Article history:
Received 26 May 2014
Received in revised form 11 July 2014
Accepted 6 August 2014
Keywords:
Nitrogen
Phosphorus
Mass-balance model
Eutrophication
Indicator
Agriculture
a b s t r a c t
Excessive nutrient delivery into freshwater bodies results in increased eutrophication risk worldwide.
Because high-frequency monitoring cannot be generalised to all rivers, methods are needed to assess
eutrophication risk in contexts with scarce data. To this end, we present an assessment framework which
includes: (i) a mass-balance model to estimate diffuse N and P transfer/retention in unmonitored catch-
ments and (ii) a set of indicators based on N:P:Si molar ratios to assess the risk of eutrophication in
freshwaters. The model, called Nutting, integrates variables that describe both agricultural pressures and
physical attributes of catchments (climate, topography, soil). Nutting refines previous mass-balance mod-
els by describing nutrient pressures with soil N surplus and soil P content instead of N and P inputs, and
by considering physical attributes not only as lumped variables over the entire area but also within river
corridors. The model was calibrated on a set of 160 independent catchments across France and applied to
all headwater catchments. We found that apparent N and P retention represented 53 ± 24% and 95 ± 29%
of soil N and P surplus, respectively, and was mainly controlled by the climate and a hydrology-related
connectivity index. The spatial organisation of the landscape was of secondary importance compared
to the refined description of agricultural pressures. Estimated eutrophication risk was highly sensitive
to assumptions about P bioavailability, hence the potential range of headwaters at risk of eutrophica-
tion spanned 26–63% of the catchments, depending on assumptions. This framework provides a generic
method to assess the relative contribution of agriculture to nutrient loads and the subsequent risk of
eutrophication.
© 2014 Elsevier Ltd. All rights reserved.
1. Introduction
Degradation of surface water resulting from excessive nitrogen
(N) and phosphorus (P) inputs is a major concern for drinking water
quality and ecosystem health (Carpenter et al., 1998; Vitousek
et al., 1997). Due to improvement of point-source control in recent
decades, research and management efforts to decrease nutrient
pollution have been redirected towards diffuse sources (Van Drecht
et al., 2009). In industrialised countries, most source apportion-
ment studies have shown that agriculture is currently a major
∗
Corresponding author at: INRA, UMR1069, Sol Agro and hydroSystem, F-35000
Rennes, France. Tel.: +33 223487047.
E-mail address: rdupas@agrocampus-ouest.fr (R. Dupas).
source of nutrients in surface waters (e.g. Bouraoui and Grizzetti,
2011; Grizzetti et al., 2012; Windolf et al., 2012). Nutrient transfers
from agricultural landscapes result from combined hydrological
and biogeochemical processes controlling their mobilisation and
delivery in the terrestrial and aquatic compartments of catchments
(Bouwman et al., 2013; Haygarth et al., 2005; Seitzinger et al., 2006).
These processes are difficult to understand and to model due to
the complexity of agricultural landscapes (Burt and Pinay, 2005;
Strayer et al., 2003).
Low-order catchments (i.e. below Strahler order 5) are known
to contribute large amounts of nutrient loads to downstream water
bodies (Alexander et al., 2007; Lassaletta et al., 2010; Peterson
et al., 2001). In terms of scientifically understanding the processes
controlling N and P diffuse transfer/retention in agricultural land-
scapes, low-order catchments are relevant spatial units because
http://dx.doi.org/10.1016/j.ecolind.2014.08.007
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