Real-time spatially-resolved radiotracer and soil conductivity measurements were used to assess the fate of contaminants and the interaction of electrolysis products with Grout Vault Soil from the Department of Energy's Hanford site in Richland, Washington. Radiotracer techniques allowed the extent that a radioactive species was remediated to be unambiguously determined in the laboratory, and the method also provided insight into the immobilization of Cs + by adsorption to the soil. Conductivity measurements provided a window into the changing state of the porous medium and the propagation of electrochemically-generated species that were introduced by water electrolysis at each active electrode. Measurements of the velocity of conductivity fronts generated by water electrolysis were combined with detailed geochemical and geophysical data about the soil to evaluate plausible soil chemistries in the system. Based on ion transport rates, it was shown that the alkaline nature of the soil buffered protons generated at the anode and hydroxide anions generated at the cathode titrated surface groups in the soil.
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