SummaryThe objective of this project is to develop a method to emplace apatite precipitate in the 100-N Area vadose zone, resulting in sorption and ultimately incorporation of Sr-90 into the apatite structure. The Ca-citrate-phosphate (Ca-citrate-PO 4 ) solution can be infiltrated into unsaturated sediments to result in apatite precipitate to provide effective treatment of Sr-90 contamination. Microbial redistribution during solution infiltration and a high rate of citrate biodegradation for river water microbes (water used for solution infiltration) produces a relatively even spatial distribution of the citrate biodegradation rate and ultimately, apatite precipitate in the sediment. Manipulation of the Ca-citrate-PO 4 solution infiltration strategy can be used to induce apatite precipitation in the lower half of the vadose zone (where most of the Sr-90 is located) and within low-K layers (which may have higher Sr-90 concentrations):• infiltration rate: more rapid Ca-citrate-PO 4 solution infiltration resulted in greater depth of apatite precipitate, but less lateral spreading• decrease in infiltration rate: rapid then slow solution infiltration resulted in greater lateral spreading of the apatite precipitate at depth• sequential solution then water infiltration: water infiltration after solution infiltration effectively moved the apatite mass to depth in homogeneous sediment systems• solution concentration: infiltration of higher Ca-citrate-PO 4 solution concentrations resulted in a greater depth of apatite precipitate• infiltration cycles: repeated infiltration of the Ca-citrate-PO 4 solution with time between cycles to allow for water drainage increased depth and greater lateral spread of apatite• low-K zones had a higher apatite precipitate due to higher residual water content• solution then water infiltration into a complex heterogeneous system with low-K and high-K discontinuous zones (8 ft high) showed high apatite precipitate in low-K and medium-grained sediment, but low treatment in high-K zones due to low water contentThe most effective infiltration strategy to precipitate apatite at depth (and with sufficient lateral spread) was to infiltrate a high concentration solution (6 mM Ca, 15 mM citrate, 60 mM PO 4 ) at a rapid rate (near ponded conditions), followed by rapid, then slow water infiltration. Repeated infiltration events, with sufficient time between events to allow water drainage in the sediment profile can be used to build up the mass of apatite precipitate at greater depth. Low-K heterogeneities were effectively treated, as the higher residual water content maintained in these zones resulted in higher apatite precipitate concentration. High-K zones did not receive sufficient treatment by infiltration, although an alternative strategy of air/surfactant (foam) was demonstrated effective for targeting high-K zones. The flow rate manipulation used in this study to treat specific depths and heterogeneities is not as easy to implement at field scale due to the lack of characterization of heterogene...