Research at the Idaho National Engineering Laboratory investigated the
movement of water through a thick fractured basalt vadose zone. Measu
rements taken in 20-cm diameter boreholes completed with 10.2-cm diame
ter PVC casing and in specially constructed test containers filled wit
h basalt showed that 50-m Ci neutron moisture gauges could distinguish
differences in moisture levels in the basalt formation beyond the wel
l's annular space. Measurements made at depths up to 55 m in similarly
constructed monitoring wells in the field showed that moisture gauge
readings lead to the same interpretation of moisture movement as readi
ngs made with a 3-Ci neutron tool.