Impacts of inland boundary conditions on modeling seawater intrusion in coastal aquifers due to sea-level rise

Inland boundary conditions have significant impacts on seawater intrusion (SWI) due to sea-level rise (SLR). This study investigated the impacts of three inland boundary conditions (flux-controlled (FC), head-controlled (HC) and general-head boundary (GHB)) on modeling SWI due to SLR in coastal aquifers. First, we used the TOUGH2/EOS7 software program to solve the standard Henry's problem and compared the results with those from the literatures. Numerical simulations were performed to investigate the impacts of the three inland boundary conditions on SWI induced by SLR in confined coastal aquifers (standard Henry's problem) and unconfined coastal aquifers (Henry's problem extended to unconfined domains). The simulation results show that HC systems in both confined and unconfined coastal aquifers are remarkably vulnerable to the effects of SLR owing to the resulting decreased head difference, while FC systems are relatively insensitive to SLR because the equivalent freshwater head at the inland boundary can increase by a similar magnitude to the SLR. The GHB boundary is more realistic than the other two boundary conditions: the recharge decreases because of SLR depending on the aquifer properties and the head difference between the reference head and the equivalent freshwater head at the seaside boundary.