Direct current (dc) cross-borehole resistivity measurements were used
to monitor the melting and solidification processes of an in-situ vitr
ification (ISV) experiment at Oak Ridge National Laboratory (ORNL) in
Tennessee. Six boreholes, 6-m deep, were augured around the ISV site,
and five electrodes implanted in each hole. Three sets of crosswell, p
ole-pole resistivity data were collected: prior to the melt phase, imm
ediately after power shut-off, and after the melt zone had solidified
and returned to ambient temperature. These three sets of data were inv
erted using a conjugate-gradient scheme to produce conductivity images
of the melt phase and the vitrified end products. The images obtained
depend quite strongly on the model weighting function applied to the
inversion. With an optimum weighting function based on a priori spatia
l constraints, the resistivity images delineate the melt zone and prov
ide a reasonable indication of its geometry. The resistivity data supp
ort, but do not require, the existence of the melt zone.