CRC LEME  
              Open File Report 180 
              ABSTRACT
             
             Combing Geology and Geophysics to Develop a Hydrogeologic Framework 
              for salt interception in the Loxton Sands Aquifer, Central Murray 
              Basin, Australia
             T.J. Munday, A.J. Hill, T. Wilson, B. Hopkins, A.L. Telfer, 
              G.J. White and A.A. Green
             
              CRC LEME OPEN FILE REPORT 180 / 
              CSIRO Exploration and Mining Report P2004/86
            EXECUTIVE SUMMARY 
             Salt interception schemes (SIS) have been developed to manage 
              high salt loads and to improve the health of the River Murray, both 
              in the Riverland (South Australia) and Sunraysia (Victoria/NSW) 
              areas. Currently SIS at Loxton and Bookpurnong are being developed, 
              both incorporating borefields in the Loxton Sands aquifer to intercept 
              saline groundwater flux from groundwater mounds that have formed 
              beneath irrigated areas. At Bookpurnong a sedimentological model 
              that defines lateral and vertical changes in facies associated with 
              the main aquifer systems relevant to the IS, has been refined from 
              a detailed interpretation of borehole geology, ground and airborne 
              geophysics, combined with the analysis of sediments for the Loxton 
              Sands and underlying Bookpurnong This is an important precursor 
              in the development of a predictive model of groundwater hydraulic 
              properties using available hydrogeological and geophysical data. 
              Definition of the sedimentological characteristics and depositional 
              setting of the principal aquifer system – the Loxton Sands, 
              has been critical. Relatively narrow zones of high transmissivity, 
              characterized by slightly reduced electrical conductivity response 
              at the watertable, are the target for ground TEM geophysical traverses. 
              These zones have been identified as elements of a Basin-wide beach-barrier 
              strandline sequence that developed in the Pliocene. Results from 
              the constrained inversion of helicopter EM data have helped to better 
              define the geometry of this sedimentary system and together with 
              a hydrogeological interpretation have contributed to a more informed 
              approach to the design, development and potential performance of 
              the Loxton Sands SIS borefields. 
             Keywords: Salt Interception Scheme, geophysics, Loxton Parilla 
              Sands, aquifers, groundwater 
              
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