Long term response of water and nitrogen fluxes to Good Agricultural Practices at field and catchment scales

被引:3
作者
Beaudoin, N. [1 ]
Venet, E. [1 ]
Maucorps, J. [2 ]
Vandenberghe, C. [3 ]
Pugeaux, N. [1 ]
Viennot, P. [4 ]
Gourcy, L. [5 ]
Brayer, C. [6 ]
Machet, J. M. [1 ]
Couturier, A. [2 ]
Billy, C. [1 ]
Vigour, N. [1 ]
Hulin, G. [1 ]
Dorel, G. [7 ,8 ]
Mary, B. [1 ]
机构
[1] BioEcoAgro Joint Res Unit, 180 PG Gennes, F-02000 Barenton B, France
[2] URSOLS, Sci Sol Orleans, 2163 Ave pomme Pin,CS 40001, F-40001 Ardon, Orleans, France
[3] BioEcoAgro Joint Res Unit ULgGxABT, Passage Deportes 2, B-5030 Gembloux, Belgium
[4] Univ PSL, MINES ParisTech, ARMINES, F-77305 Fontainebleau, France
[5] Bur Rech Geol & Minieres, 3 Ave Claude, F-45100 Orleans, France
[6] Chambre Agr Aisne, Bd Lyon, F-02000 Laon, France
[7] Mairie, 1 Pl Gen Gaulle, F-02860 Bruyeres Le Chatel, France
[8] Mairie, 1 Pl Gen Gaulle, F-02860 Montberault, France
关键词
Cropping systems; Soil organic nitrogen; Nitrate; Cost/efficiency; Deep aquifer; Residence time; GROUNDWATER NITRATE CONTAMINATION; SOIL-CROP MODEL; LAND-USE; MANAGEMENT-PRACTICES; STICS MODEL; LAG TIME; SEINE; POLLUTION; SYSTEMS; QUALITY;
D O I
10.1016/j.scitotenv.2021.145954
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Facing the nitrate pollution problem, the European Union has encouraged a code of "Good Agricultural Practices" (GAP) in order to recover a good chemical and ecological status of waterbodies. In this study, we hypothesized that the systematic application of GAP in time and space would allowtomeet the EU standard of nitrate concentration (50 mg NO3 L-1) under arable cropping systems. Water and nitrogen fluxes were determined in an agricultural catchment (187 ha) during 22 years after GAP implementation, at field and catchment scales. The aquifer outlet is a set of springs which were monitored for water flow and nitrate concentration. GAP management mainly consisted in adjustingNfertilization rates and establishing catch crops. CropNuptake, soilwater and mineral N were measured respectively two and three times per year on 36 sites representing soil variability. These data were used to initialize the STICS model which simulated the fluxes of infiltrated water and nitrate leached below the rooting zone at field scale. The elementary fluxes (calculated for each site-year) were then used as independent inputs of the hydrological model MODCOU which made the integration at catchment scale. Simulations of agricultural scenarios allowed to calculate the cost/efficiency ratio of GAP implementation per soil type. The mean amounts of infiltrated water and N leached calculated below rooting depth in agricultural fields were 179 mm yr(-1) and 19 kg N ha(-1) yr(-1), respectively, yielding a mean weighted nitrate concentration of 41 mg NO3 L-1 during 22 years over the whole catchment. The mean residence time of water in the catchment was estimated at 17-22 years using tritium and CFC tracers. The observed nitrate concentration in the main spring declined 11 years after GAP implementation and levelled off to 49 mg NO3 L-1. The agro-hydrological model satisfactorily predicted water flow and nitrate concentration in springs but overestimated their response time. It predicted a positive impact of GAP application on water quality. GAP management appeared to be efficient on the long termwith a lowcost/efficiency ratio. Amore flexible and motivating management could consist in including GAP as a first step in a loop progress towards agro-ecological systems. (C) 2021 Elsevier B.V. All rights reserved.
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页数:15
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