Saltwater intrusion in a three-dimensional large-scale coastal aquifer in t
he northern part of the province Noord-Holland, The Netherlands, is investi
gated. The computer code MOCDENS3D, which is the code MOC3D of Konikow et a
l. (1996) but adapted for differences in density, is used to model the disp
lacement of fresh, brackish and saline groundwater in this hydrogeologic sy
stem. It appears that a severe salinisation already occurs. This process is
initiated by the reclamation of the (low-lying) polders during the past ce
nturies. Though seepage quantities decreases in many polder araes due to an
increase in salinity, the salt load increases significantly. (C) 2001 Else
vier Science Ltd. All rights reserved.