Durch systematische Geländeuntersuchungen über 15 Monate an zwei Brunnengalerien der Berliner Wasserbetriebe wurde untersucht, ob und inwieweit kontinuierliche Temperaturmessungen entlang der Fließstrecke des Grundwassers geeignet sind, die Aufenthaltszeit so zuverlässig zu bestimmen, dass ein kritisches Unterschreiten der 50-Tage-Linie erkannt und entsprechende betriebliche Gegenmaßnahmen im Routinebetrieb eingeleitet werden können. Die Temperaturmessung erfolgte kontinuierlich mittels Datenloggern in Entnahmebrunnen und Grundwassermessstellen und zusätzlich manuell bei wöchentlichen Probenahmen. Zeitreihen konservativer Tracer (Chlorid, Bromid, d18O und d2H) dienten der Validierung der aus den Temperaturmessungen bestimmten thermischen Retardations- und Dispersionskoeffizienten. Trotz signifikanter Unterschiede zwischen den beiden untersuchten Standorten erwiesen sich die Temperaturmessungen als geeignetes Instrument zur Bestimmung der Verweilzeiten. Aus den untersuchten Tracern konnten darüber hinaus Aussagen zum Mischungsverhältnis von angereichertem und autochthonem Grundwasser abgeleitet werden.

Different types of managed aquifer recharge (MAR) schemes are widely distributed and applied on various scales and for various purposes in the European countries, but a systematic categorization and compilation of data has been missing up to now. The European MAR catalogue presented herein contains various key parameters collected from the available literature. The catalogue includes 224 currently active MAR sites found in 23 European countries. Large quantities of drinking water are produced by MAR sites in Hungary, Slovakia, the Netherlands, Germany, Finland, Poland, Switzerland and France. This inventory highlights that, for over a century, MAR has played an important role in the development of European water supply and contributes to drinking-water production substantially. This development has occurred autonomously, with “trial-and-error” within the full range of climatically and hydrogeologically diverse conditions of the European countries. For the future, MAR has the potential to facilitate optimal (re)use and storage of available water resources and to take advantage of the natural purification and low energy requirements during MAR operations. Particularly with respect to the re-use of wastewater treatment-plant effluent and stormwater, which is currently underdeveloped, the use of MAR can support the public acceptance of such water-resource efficient schemes. Particularly for the highly productive and urbanized coastal zones, where the pressure on freshwater supplies increases by growing water demand, salinization and increased agricultural needs for food production (such as along the Mediterranean and North Sea coasts), MAR is expected to be increasingly relied on in Europe.

Subsurface travel time from the area of recharge to the abstraction during Managed Aquifer Recharge (MAR) is a critical parameter to ensure sufficient attenuation for hygienic parameters and other undesired substances. This study investigates seasonal temperature fluctuations observed in recharge water and MAR wells as a proxy for cheap and reliable travel time control at a basin infiltration site in Berlin-Spandau (Germany). Based on a time series from seven years of manual measurements, temperature fluctuations observed in infiltration basins and abstraction wells were fitted to sinusoidal functions. Peak values represented as local maxima and local minima from the fitted curves were used for the approximation of travel times between infiltration basin and abstraction wells. Uncertainty was assessed by Monte Carlo simulation of fitted curves based on standard deviation (2s) from residuals. The calculated error propagation from 2s in infiltration basin and 2s in wells range from 7 to 19 days. This study indicates that travel time approximation based on biased manual measurements of temperature is associated with high uncertainty. Nevertheless, the water temperature method for estimating subsurface travel times shows encouraging results and if temperature can be accurately determined, this method can be readily applied at other sites with similar characteristics.

The paper presents semi-analytical mathematical model to estimate unsteady groundwater recharge resulting from variable depth of water in a large water body, influenced by time variant inflows and outflows. The model has been derived by integrating Hantush’s (1967) analytical expression for water table rise due to recharge from a rectangular spreading basin into the water balance equation of the water body. The model has been applied to a test study site in Raipur (India) for assessing viability of Managed Aquifer Recharge (MAR) from a lake located on an area dominated by the massive limestone formation. The components of the water balance equation have been carried out by the comprehensive analysis of the hydrological and hydrogeological aspects of the lake. The hydrological components include

This project report summarizes work conducted in work package 11. Along with the deliverable 11.1 and milestone report 11 it covers the tasks from work package 11 as formulated in the Description of Work (DoW). The content of the different sections is interrelated, but each section is organized as an independent part. Title of this report differs from DoW because recommendations for optimum design and operation will be handled in the deliverable 12.2. The sections in this report cover various topics and each section can be found as a stand-alone report in the DEMEAU tool box (http://demeaufp7.eu/toolbox/) for download. Detailed summaries can be found for each section separately.