Executive SummaryApproximately 56 million gallons of high-level radioactive mixed waste has accumulated in 177 buried single-and double-shell tanks at the Hanford Site in southeastern Washington State as a result of the past production of nuclear materials for the U.S. strategic defense arsenal. The United States Department of Energy (DOE) is proceeding with plans to permanently dispose of this waste. Plans call for separating the tank waste into high-level waste (HLW) and low-activity waste (LAW) fractions, which will be vitrified at the Hanford Tank Waste Treatment and Immobilization Plant (WTP). Between 150,000 and 345,000 m 3 of immobilized LAW (ILAW) glass are expected to be produced at Hanford. Principal radionuclides of concern in LAW are 99 Tc, 129 I, and U, while non-radioactive contaminants of concern are Cr and nitrate/nitrite (Mann et al., 2001;Mann et al., 2003). Between 9,000 and 20,000 m 3 of HLW glass will be sent off site to an undetermined federal facility for deep geological disposal, while the much larger volume of ILAW will be placed in the on-site, near-surface Integrated Disposal Facility (IDF).Before the ILAW can be disposed of at the IDF, a performance assessment (PA) must be conducted. The PA is a document that describes the long-term impacts of the disposal facility on public health and environmental resources. One of the major inputs to the PA is the estimate of radionuclide release rates from the engineered portion of the disposal facility into the surrounding environment. These estimates are expected to be based on chemical reactions that occur in the near-field, and to a certain extent, are controlled by the dissolution of the vitrified waste form. Once released from the vitrified matrix, the transport of the radionuclides of concern is based on chemical reactions that occur in the near-and farfield. Therefore, to provide credible estimates, a mechanistic understanding of the physical and geochemical processes that control glass dissolution, and thus radionuclide release, must be understood and incorporated into models used to predict radiation dose over the period of regulatory concern (~ 10,000 years). A cornerstone assumption for the approach to estimating the source term is that the glass matrix must dissolve for radionuclides to be released into the environment. This assumption has been demonstrated in pressurized unsaturated flow (PUF) experiments conducted with ILAW glass produced with actual radioactive low-activity waste (Pierce et al., 2006). The major parameters known to control glass dissolution are glass composition, temperature, and solution composition of the fluid contacting the glass (including pH and concentration of key ions [e.g., H 4 SiO 4 ]). The effect of these parameters on the glass dissolution rate is essential for developing credible PA models. Though the temperature of the IDF is expected to be roughly constant at 15 °C, the pH and fluid compositions are affected by flow rate (i.e., water infiltration), reactions with near-field engineered materials, gas-...