Lithologic imaging using complex conductivity: Lessons learned from the Hanford 300 Area

ABSTRACTField-scale lithologic applications of complex conductivity (σ*) imaging have been hindered by the challenges of (1) acquiring reliable induced polarization (IP) measurements and (2) obtaining reliable σ* images from the measurements. We performed a series of 2D time domain resistivity/IP surveys at the Hanford 300 Area (Richland, Washington) where the challenge was to image the spatial distribution of two lithologic units that control the exchange between groundwater and surface water of the Columbia River. Exploiting the equivalence between time domain and frequency domain measurements of polarization, a 2D σ* inversion (real conductivity σ′, imaginary conductivity σ′′, and phase angle ϕ) was used to image the spatial distribution of σ* across the site. Synthetic studies were carried out to investigate the effects of noise on the resolution of σ* images and to add confidence on the interpretation of possible paleochannels observed in the field data sets. The synthetic studies show that, with inc...