The Publications Warehouse does not have links to digital versions of this publication at this time
Interpretation of geochemical reactions and isotopic composition of groundwater provides a method to determine hydrological parameters such as porosity, hydraulic conductivity, and groundwater flow rates. This geochemical method is largely independent of the more conventional approach of determining these parameters by an evaluation of physical properties of aquifer systems. -from Authors
Additional Publication Details
Deciphering hydrological systems by means of geochemical processes.
Hydrological Sciences Journal/Journal des Sciences Hydrologiques