title: Analytic Element Modeling of Steady Interface Flow in Multilayer Aquifers Using AnAqSim.
abstract: This paper presents the analytic element modeling approach implemented in the software AnAqSim for simulating steady groundwater flow with a sharp fresh-salt interface in multilayer (three-dimensional) aquifer systems. Compared with numerical methods for variable-density interface modeling, this approach allows quick model construction and can yield useful guidance about the three-dimensional configuration of an interface even at a large scale. The approach employs subdomains and multiple layers as outlined by Fitts (2010) with the addition of discharge potentials for shallow interface flow (Strack 1989). The following simplifying assumptions are made: steady flow, a sharp interface between fresh- and salt water, static salt water, and no resistance to vertical flow and hydrostatic heads within each fresh water layer. A key component of this approach is a transition to a thin fixed minimum fresh water thickness mode when the fresh water thickness approaches zero. This allows the solution to converge and determine the steady interface position without a long transient simulation. The approach is checked against the widely used numerical codes SEAWAT and SWI/MODFLOW and a hypothetical application of the method to a coastal wellfield is presented.
authors.affiliation: McLane Environmental, LLC, 707 Alexander Rd, Suite 206, Princeton, NJ 08540.
authors.forename: Charles R
authors.initials: CR
authors.lastname: Fitts
authors.forename: Joshua
authors.initials: J
authors.lastname: Godwin
authors.forename: Kathleen
authors.initials: K
authors.lastname: Feiner
authors.forename: Charles
authors.initials: C
authors.lastname: McLane
authors.forename: Seth
authors.initials: S
authors.lastname: Mullendore
mesh_terms: D003198:Computer Simulation; D004784:Environmental Monitoring / Q000379:methods*; D005618:Fresh Water; D060587:Groundwater / Q000737:chemistry*; D054712:Salinity; D012623:Seawater; D012984:Software; D014872:Water Movements