Modeling of ground water infiltration and movement in the wellhead are
a is a critical part of an effective wellhead protection program. Such
models depend on an accurate description of the aquifer in the wellhe
ad area so that reliable estimates of contaminant travel times can be
used in defining a protection area. Geophysical and hydraulic measurem
ents in boreholes provide one of the most important methods for obtain
ing the data needed to specify wellhead protection measures. Most effe
ctive characterization of aquifers in the wellhead vicinity results wh
en a variety of geophysical and hydraulic measurements are made where
geophysical measurements can be calibrated in terms of hydraulic varia
bles, and where measurements are made at somewhat different scales of
investigation. The application of multiple geophysical measurements to
ground water flow in the wellhead area is illustrated by examples in
alluvial, fractured sedimentary, and fractured crystalline rock aquife
rs. Data obtained from a single test well are useful, but cannot indic
ate how conductive elements in the aquifer are connected to form large
-scale flow paths. Geophysical and hydraulic measurements made in arra
ys of observation boreholes can provide information about such large-s
cale flow paths, and are especially useful in specifying aquifer prope
rties in wellhead protection studies.