Stage B Uranium Sequestration Amendment Delivery Monitoring Using Time-Lapse Electrical Resistivity Tomography
The Hanford Site 300 Area lies adjacent to the Columbia River, approximately 5 km north of Richland, Washington. Past waste disposal practices in the 300 Area resulted in vadose zone uranium contamination beneath former infiltration ponds and trenches. Stage-driven water table fluctuations and river water intrusion facilitate mobilization of uranium from contaminated sediments in regions periodically occupied by the water table (i.e., the periodically rewetted zone or PRZ), thereby raising groundwater uranium concentrations above the maximum allowable contaminant level for uranium. This report documents the ERT imaging operations and interpretation of imaging results in terms of the extent of amendment delivery (including phosphate and/or carrier fluid) within the treatment area. Based on the interpretation, amendment delivery to the LVZ and PRZ was observed to be variable between each of the three imaging clusters, as shown in Figure S.1. Amendment transport in Cluster 1 exhibited significant lateral flow in comparison to Clusters 2 and 3, resulting in a final amendment distribution throughout a large portion of the LVZ and PRZ sediment between the injection wells. Cluster 2 exhibited good amendment delivery in the LVZ only near the injection wells. In the PRZ at Cluster 2, amendment was effectively distributed through the full distance between injection wells. Cluster 3 exhibited the smallest amount of lateral flow and amendment was primarily distributed in the LVZ and PRZ very near the injection wells. Imaging results below the water table suggest that more amendment entered the groundwater in Cluster 2 and Cluster 3 than in Cluster 1.