Executive SummaryThis project was initiated to investigate whether in situ coupled abiotic/biotic degradation of N-nitrosodimethylamine (NDMA, an emerging contaminant) could be used as a permeable reactive barrier for remediation at the Aerojet, California site, where groundwater contains up to 36-ppb NDMA. The sediment mainly used in experiments is from the Aerojet groundwater aquifer (260-ft depth), with additional sediments from other groundwater aquifers (i.e., not shallow soils, Ft. Lewis, Washington, 60-ft depth, Puchack, New Jersey, 273-ft depth). Different in situ remediation processes were compared in this study: a) biostimulation (oxic, anaerobic, iron-reducing, sulfate-reducing), b) abiotic iron-reducing environment (by dithionite reduction of sediment or zero valent iron addition), c) coupled abiotic/biotic remediation (iron-reducing environment), and d) sequential iron-reducing, then oxic, biostimulation. The overall goal was to understand and optimize the combined effects of abiotic and biotic processes to degrade NDMA to nontoxic products. Iron-reducing conditions were created by chemical reduction of a sediment using sodium dithionite, and in a few cases, a natural reduced aquifer sediment or sediment with zero valent iron addition.When subsurface sediments are chemically or naturally reduced, abiotic surface phase(s) rapidly degraded NDMA (8-hour half-life for high reduction, slower for low reduction) to nontoxic dimethylamine (DMA). Experiments showed up to 80% conversion of NDMA to DMA, with further degradation to nitrate (up to 40% molar conversion), formate (trace concentration) and carbon dioxide (up to 82% molar conversion). Methylamine and formaldehyde (likely intermediates) were not detected. Experiments with 100 and 10 ng/L NDMA starting concentration had a rapid degradation half-life (4.7 hours), and NDMA was degraded to <3 ng/L (detection limit). Although degradation to DMA is sufficient for remediation (DMA is not toxic at <5 mg/L), because NDMA mass was degraded further to more toxic intermediates, NDMA mineralization (i.e., to CO 2 ) was considered the lowest risk product, and was the main focus of this study. NDMA degradation was most rapid with high sediment reduction. These sediments had a higher mass of ferrous surface phases (ferrous oxides, carbonates, sulfides, adsorbed ferrous iron, green rust) and a more alkaline pH (pH increased from 9.1 to 10.5). The NDMA reactivity of these different iron phases showed that adsorbed ferrous iron was the dominant reactive phase that promoted NDMA reduction. Alkaline hydrolysis by itself (no sediment, pH 11) did not degrade NDMA, nor did alkaline hydrolysis with anaerobic sediment (a potential catalyst). Iron sulfides, while present in the reduced sediment, did not change the NDMA degradation rate. Iron(II) carbonate (siderite) also showed little reactivity with NDMA, as its removal did not influence NDMA degradation. Although magnetite itself (with no sediment) did not promote NDMA degradation, magnetite removal from the reduced sediment...