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Delineating ‘groundwater bodies’ and optimisation of the groundwater monitoring network (in the scope of the EC Water Directive 2000/60/CE)

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(1)30/08/2013. Delineating ‘groundwater bodies’ and optimisation of the groundwater monitoring network (in the scope of the EC Water Directive 2000/60/CE). Outline - delineating ‘groundwater bodies’ theory … and practice. - optimisation of the groundwater monitoring network theory … and practice. A.Dassargues1,2 , C. Rentier1 , S. Brouyère1 , Fr. Delloye3. - test application of the SEQ-ESO as groundwater quality evaluation tool. 1. Hydrogeology, Dpt Georesources, Geotechnologies and Building Materials (GeomaC) & Aquapole, University of Liège, Belgium Hydrogeology & Engineering Geology, Dpt Geology-Geography, KULeuven, Belgium 3 Groundwater Direction, Water Division, DGRNE Walloon Region, Belgium 2. …in the scope of the EC Water Directive 2000/60/CE). Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Delineating ‘groundwater bodies’: theory. Terug naar eerste pagina. Delineating ‘groundwater bodies’: theory. Elements of Characterization Hydrology •. annual precipitation. Geology • • • • •. stratigraphy lithology thickness overlying strata depth to groundwater. Hydrogeology • • •. recharge (precipitation, surface waters, groundwaters, springs, irrigation) hydraulic conductivity annual piezometric amplitudes. Pressures • • • • •. land use water abstractions artifical recharge main infrastructures associated aquatic ecosytems. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Delineating ‘groundwater bodies’: theory. Terug naar eerste pagina. Delineating ‘groundwater bodies’ aims: characterization & management .  . Hydrogéologie. Terug naar eerste pagina. initial characterisation requires collation of data on pressures on GW body(ies):  diffuse sources of pollution  point sources of pollution  abstraction  artificial recharge  general character of overlying strata in recharge areas and dependent ecosystems use only existing data at initial characterisation data on distribution of pressures, observed impacts. Hydrogéologie. Terug naar eerste pagina. 1.

(2) 30/08/2013. Delineating ‘groundwater bodies’: practice. Delineating ‘groundwater bodies’: practice. (Observatoire des Eaux Souterraines, DGRNE, Ministère de la Région Wallonne, 2002). http://environnement.wallonie.be/de/eso/atlas/#1.1res. 50 km. 2 km. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Delineating ‘groundwater bodies’: practice. Terug naar eerste pagina. Optimisation of groundwater monitoring network. management reasons: - quantity - quality 50 km Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Optimisation of groundwater monitoring network. Terug naar eerste pagina. Optimisation of groundwater monitoring network   . collecting all existing data (quantity and quality) analysis of geological/hydrogeological conditions on the basis of few criteria: choice of the points for the monitoring network Special ‘vulnerable’ zones. * network density. Hydrogéologie. Terug naar eerste pagina. 16 km. Hydrogéologie. Terug naar eerste pagina. 2.

(3) 30/08/2013. Optimisation of groundwater monitoring network. Optimisation of groundwater monitoring network collecting all existing data (quantity and quality). 8 km. 8 km. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Optimisation of groundwater monitoring network. Terug naar eerste pagina. Optimisation of groundwater monitoring network. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Optimisation of groundwater monitoring network. Terug naar eerste pagina. Optimisation of groundwater monitoring network analysis of geological/hydrogeological conditions …on the basis of few criteria: choice of the points for the monitoring network . Piezometric head .   . 8 km.    . upward or downward position of the measurement point (with respect to the piezometry) integrating/representative character of the measurement/sampling point variability of the historical measured data point contamination sources accessibility of the measurement/sampling point well equipment present state and ownership of the well depth …. 1 point/25km2 in special zones and 1 point/100 km2 in other zones. Hydrogéologie. Terug naar eerste pagina. Hydrogéologie. Terug naar eerste pagina. 3.

(4) 30/08/2013. Optimisation of groundwater monitoring network. Optimisation of groundwater monitoring network   . collecting all existing data (quantity and quality) analysis of geological/hydrogeological conditions on the basis of few criteria: choice of the points for the monitoring network Special ‘vulnerable’ zones. * network density. 8 km. 1 point/25km2 in special zones and 1 point/100 km2 in other zones. Hydrogéologie. 16 km. Terug naar eerste pagina. collecting all existing data (quantity and quality). Hydrogéologie. Terug naar eerste pagina. GW levels: quantity control. 8 km. 8 km. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Terug naar eerste pagina. GW concentrations: quality control. 8 km. 8 km. Hydrogéologie. Terug naar eerste pagina. Hydrogéologie. Terug naar eerste pagina. 4.

(5) 30/08/2013. Optimisation of groundwater monitoring network 1 point/25km2 in special zones and 1 point/100 km2 in other zones 10 points - 2 galleries - 1 source - 7 wells. Test of the SEQ-ESO as a groundwater quality evaluation tool Objectives  check the groundwater quality with respect to the existing standards (nitrates, pesticides, …)  check the drinking water standards without heavy processing at the source (resource)  check the quality objectives for the depending surface ecosytems  check anomalies with respect to the ‘natural state’ and to the present background then select the most difficult objective for synthesis, conclusions and remediation. ‘Système d’Evaluation de la Qualité des Eaux Souterraines’ (SEQ-ESO) developed by the French ‘Agences de l’Eau’. 8 km. . coherent with SEQ for surface water quality. . evaluation in function of the use. . distinction between different kinds of water quality ‘alterations’. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Test of the SEQ-ESO as a groundwater quality evaluation tool  . Terug naar eerste pagina. Test of the SEQ-ESO as a groundwater quality evaluation tool. 17 different possible alterations … receiving a score between 0 and 100 3 main functions of groundwater: consumed water (different kind of use), patrimonial state, chemical aptitude for biology of surface waters. only three kinds of index:. Usage AEP (alimentation en eau potable): Eau de qualité optimale pour être consommée. Adaptations: 1) drinking water; 2) patrimonial state;. NO3 = 25 mg/l. Eau de qualité acceptable pour être consommée mais pouvant le cas échéant faire l'objet d'untraitement de désinfection.. 3) global. NO3=50mg/l Eau non potable nécessitant un traitement de potabilisation. six groups of alteration modification of some thresholds (gw quality limits between two categories). Eau inapte à la production d'eau potable. NO3=100mg/l. Indice global SEQ: Eau de très bonne qualité I = 80% NO3=10 Eau de bonne qualité I = 60% NO3=20 Eau de qualité moyenne I = 40% NO3=50 Eau de qualité I = 20% NO3=100 médiocre Eau de mauvaise qualité I = 0%. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. NO3=10mg/l Eau de composition proche de l'état naturel, mais détection d'une NO3=20mg/l contamination d'origine anthropique.. NO3=50mg/l. NO3=100mg/l. Dégradation significative par rapport à l'état naturel. Dégradation importante par rapport à l'état naturel. Dégradation très importante par rapport à l'état naturel.. Hydrogéologie. Terug naar eerste pagina. Test of the SEQ-ESO as a groundwater quality evaluation tool: example of result. Etat patrimonial: Eau dont la composition est naturelle ou "sub-naturelle".. Terug naar eerste pagina. Conclusions: … a lot of work !! the choices and the work done now will have a enormous influence on the future management of the groundwater bodies !. Hydrogéologie. Terug naar eerste pagina. 5.

(6) 30/08/2013. Large-scale groundwater modelling within the PIRENE programme in the Walloon Region of Belgium S. Brouyère1 , Ph. Orban, A.Dassargues1,2. Quantitative and qualitative objectives • Collect of data and using existing characterization of aquifers Modelling groundwater quantity • Hydrogeological balance of the aquifers • Effect of the infiltration fluxes • Estimation of groundwater-river interactions. 1. Hydrogeology, Dpt Georesources, Geotechnologies and Building Materials (GeomaC) & Aquapole, University of Liège, Belgium 2 Hydrogeology & Engineering Geology, Dpt Geology-Geography, KULeuven, Belgium 3 Groundwater Direction, Water Division, DGRNE Walloon Region, Belgium. • Impacts of pumping, recharge, … and any changes in stress-factors • Trends of the groundwater quantity for different scenarios of the future Modelling groundwater quality • Trends in nitrates and pesticides • Effect of the infiltration fluxes • Estimation of groundwater-river interactions • Impacts of any change in stress-factors. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Terug naar eerste pagina. Methodology of work Modelling groundwater flow and transport at an unusual scale: the scale of the Walloon Region. 5 different steps: • Collect of data • Data Base and formating data • Development of numerical tools adn tests • Conceptual model for each zone • Implementation of the chosen model, calibration, validation and use for scenarios. Hydrogéologie. Hydrogéologie. Terug naar eerste pagina. Terug naar eerste pagina. Adaptation of the SUFT3D code Modelling groundwater flow and transport at an unusual scale: the scale of the Walloon Region simplified approaches development of new boundary conditions improvement of computation performances. ÉCOULEMENT. TRANSPORT. Hydrogéologie. Terug naar eerste pagina. Réservoir linéaire simple Réservoir linéaire distribué Écoulement en milieu poreux. Réservoir linéaire simple. Modèle de mixage distribué. OK. impossible. impossible. OK. OK. impossible. OK. OK. OK. Advectiondispersion. Hydrogéologie. Terug naar eerste pagina. 6.

(7) 30/08/2013. Tests of a regional discretization. 2D Mean surface of an element = 0.4 km2 difficult to take into account explicitely rivers, wells, …. Hydrogéologie. Terug naar eerste pagina. 7.

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