The variation of hydraulic conductivity with depth in the object-oriented groundwater model ZOOMQ3D

This report documents the implementation of the variation of hydraulic conductivity with depth
within layers of the object-oriented regional groundwater model ZOOMQ3D. This
representation of the vertical variation of hydraulic conductivity provides an alternative to the
development of multi-layer models, in which individual layers are characterised by uniform
horizontal hydraulic conductivity in the vertical direction.
The approach has been developed to enable the more accurate description of the variation the
hydraulic conductivity in limestone, and particularly Chalk aquifers, in which higher hydraulic
conductivity values are often associated with the zone of fluctuation of the water table. The
method circumvents numerical difficulties that are related to the de-watering of layers in multilayer
models.
The incorporation of the vertical variation of hydraulic conductivity with depth (VKD)
mechanism has been rapidly incorporated into ZOOMQ3D due to the flexibility of the objectframework.
The model has been rigorously tested by its comparison with a modified
MODFLOW model (Environment Agency, 1999) in which VKD has also been implemented.