{"refrec":{"BRefID":220556,"RR":"<b>Vandenbohede, A.; Van Houtte, E.; Lebbe, L.</b> (2008). Study of the feasibility of an aquifer storage and recovery system in a deep aquifer in Belgium. <i>Hydrol. Sci. J. 53(4)</i>: 844-856. <a href=\"http://dx.doi.org/10.1623/hysj.53.4.844\" target=\"_blank\">http://dx.doi.org/10.1623/hysj.53.4.844</a>","BEntID":212290,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Hydrol. Sci. J. 53(4)</i>: 844-856. <a href=\"http://dx.doi.org/10.1623/hysj.53.4.844\" target=\"_blank\">http://dx.doi.org/10.1623/hysj.53.4.844</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vandenbohede, A.; Van Houtte, E.; Lebbe, L.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vandenbohede, A. <i>et al.</i>","Englishabstract":"The feasibility of aquifer storage and recovery (ASR) was tested in a deep aquifer near Koksijde, Belgium. To achieve this, oxic drinking water was injected into a deep aquifer (the Tienen Formation) that contains anoxic brackish water. The hydraulic properties of the aquifer were determined using a step-drawdown test. Chemical processes caused by the injection of the water were studied by two push—pull tests. The step-drawdown test was interpreted by means of an inverse numerical model, resulting in a transmissivity of 3.38 m<sup>2</sup>/d and a well loss coefficient of 0.00038 d<sup>2</sup>/m<sup>5</sup>. The push—pull tests identified mixing between the injection and pristine waters, and cation exchange, as the major processes determining the quality of the recovered water. 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