An Apatite II permeable reactive barrier to remediate groundwater containing Zn, Pb and Cd

Abstract

Phosphate-induced metal stabilization involving the reactive medium Apatite II™ [Ca 10− x Na x (PO 4) 6− x (CO 3) x (OH) 2], where x < 1, was used in a subsurface permeable reactive barrier (PRB) to treat acid mine drainage in a shallow alluvial groundwater containing elevated concentrations of Zn, Pb, Cd, Cu, SO 4 and NO 3. The groundwater is treated in situ before it enters the East Fork of Ninemile Creek, a tributary to the Coeur d’Alene River, Idaho. Microbially mediated SO 4 reduction and the subsequent precipitation of sphalerite [ZnS] is the primary mechanism occurring for immobilization of Zn and Cd. Precipitation of pyromorphite [Pb 10(PO 4) 6(OH,Cl) 2] is the most likely mechanism for immobilization of Pb. Precipitation is occurring directly on the original Apatite II. The emplaced PRB has been operating successfully since January of 2001, and has reduced the concentrations of Cd and Pb to below detection (2 μg L −1), has reduced Zn to near background in this region (about 100 μg L −1), and has reduced SO 4 by between 100 and 200 mg L −1 and NO 3 to below detection (50 μg L −1). The PRB, filled with 90 tonnes of Apatite II, has removed about 4550 kg of Zn, 91 kg of Pb and 45 kg of Cd, but 90% of the immobilization is occurring in the first 20% of the barrier, wherein the reactive media now contain up to 25 wt% Zn. Field observations indicate that about 30% of the Apatite II material is spent (consumed).