Abstract
AbstractA 90Sr‐contaminated groundwater seep on the perimeter of a low‐level radioactive solid waste disposal area at the Oak Ridge National Laboratory (ORNL) was treated by burying 315 kg of soda ash in the groundwater flow path leading to the seep, and placing 45 kg of soda ash on the surface of the seep. The concentration of 90Sr in the seep water fell from an average of 7000 Bq L−1 to 900 Bq L−1 for the 90 d after burial, followed by a period of gradual rise back to pretreatment levels over the next 100 d. The electrical conductivity and pH of the seep water increased following soda ash burial, while water hardness fell. Hardness was highly correlated (r = 0.84) with 90Sr concentrations over the entire 2‐year observation period, indicating the similar behavior of 90Sr and soluble Ca and Mg. This in situ softening of, and 90Sr precipitation from, the seep water was achieved by coprecipitation of 90Sr with Ca(Mg)CO3 until the buried soda ash was depleted by dissolution in the groundwater. The soda ash treatment of groundwater seeps appears to be most practical as an interim technique for those situations requiring an immediate, but temporary, corrective action. During this limited but effective period, more permanent corrective actions could be planned at the source of contamination. The electrical conductivity, pH, and hardness of the larger surface stream, into which this seep discharges, were not affected by the soda ash burial, most likely due to the approximately 2000‐fold dilution effected by this stream.
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