Executive SummaryThis report describes the results from laboratory tests performed at Pacific Northwest National Laboratory for the U.S. Department of Energy (DOE) EM-31 Support Program (EMSP) subtask, "Low temperature waste forms coupled with technetium removal using an alternative immobilization process such as Fe(II) treated-goethite precipitation" to increase our understanding of 99 Tc long-term stability in goethite mineral form and the process that controls the 99 Tc(VII) reduction and removal by the final Fe (oxy)hydroxide mineral forms.The overall objectives of this task were to 1) evaluate the transformation process of Fe (oxy)hydroxide minerals to more crystalline goethite (α-FeOOH) Tc removal was not considered to be from surface adsorption, but incorporation into transformed mineral product. Although a further analysis is essential to confirm 99 Tc speciation in the final transformed product from Fe(OH) 2 (s), mineral transformation from Fe(OH) 2 (s) can be used to effectively remove 99 Tc(VII) in alkaline pH conditions germane to off-gas scrubber secondary waste and low-activity waste streams. Slightly more transformation products were also found from Fe(OH) 2 (s) with a solution-to-solid ratio of 100 than with a ratio of 1000. The transformation product from ferrihydrite was similar, and solely goethite mineral was produced in most of the conditions. It is clear that comparison results from both Fe(OH) 2 (s) and ferrihydrite substrates show that high slurry pH and high temperature conditions favor more goethite formation from the transformation reaction. Unfortunately, we could not conduct 99 Tc removal using ferrihydrite as an initial substrate in this task, but based on previous results (Um et al. 2010), ferrihydrite can also be used to remove 99 Tc with additional aqueous Fe(II). Transformation product from magnetite was very limited and there were only small amounts of maghemite and goethite formed from magnetite reacted as initial substrate under high pH and temperature conditions. In addition, negligible 99 Tc removal (<5%) from solution was also found in magnetite slurry without aqueous Fe(II) addition.Even after long-term leaching in the Integrated Disposal Facility (IDF) pore water solution for two years, very limited amounts of 99 Tc and Fe(total) were detected in the IDF leachates. The limited 99 Tc release was attributed to more stabilized 99 Tc(IV) present in 99 Tc-goethite lattice even after long-term exposure to oxygen, while zero detected Fe(total) concentration in the IDF leachate indicated that the iv structure of the final goethite mineral was stable in a circumneutral pH condition similar to the IDF pore water. Reduced 99 Tc(IV) incorporated in the goethite was unlikely to be reoxidized to 99 Tc(VII), even when the final 99 Tc-goethite product (sample 2-5) was exposed to oxidizing conditions for three years (two years in IDF solution plus one year in air). In addition, the measured reductive capacity of both 99 Tc-goethite 2-2 sample (prepared without additional armoring pro...