We devised a new conceptual model, water balance, geologic model, and numerical flow and solute transport models. Developing a hydrogeologic framework for the complex aquifer system was challenging, because erosion and deposition on the uplifted transgression-regression system of aquitards and aquifers created pathways within the Gap for seawater to travel inland. The pathways, called mergence zones, connect the seawater-intruded Recent Aquifer with several of the deeper aquifers used for water supply.
Using the new conceptual and geologic models as a foundation, INTERA constructed a three-dimensional transient groundwater flow model using the MODFLOW 2000 code. Over 19,000 head measurements in nearly 200 monitoring wells well were used for the transient calibration. INTERA also constructed a three-dimensional transient transport model using the MT3DMS transport code. The calibrated models were used to assess the performance of four different barrier configurations: a baseline (existing) and three future expansion options. We also investigated the impact of variable-density flow on Alamitos Barrier performance by simulating chloride migration through a sub-domain model that was run using SEAWAT. INTERA handed over the completed modeling tools to the three client agencies in autumn of 2010.
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