Kristopher Kuhlman and Anke Schneider are collaborating to improve basin-scale groundwater flow and solute transport models near salt repositories. Their efforts include reimplementing and extending an existing 1996 groundwater model of the WIPP basin to include density dependent flow and improved mesh elements. They have implemented solute concentration-dependent fluid density in the PFLOTRAN model and conducted initial model comparisons. This work will lead to an updated regional groundwater flow and chemistry model for the WIPP area and improved understanding of issues in past and future regional models surrounding salt repositories.