Thermodynamics of AFm-(I2, SO4) solid solution and of its end-members in aqueous media
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文摘
Cementitious materials are foreseen as being used for the immobilization of radionuclides in deep-storage facilities for nuclear waste. The 129I contained in the waste is of major concern due to its long half-life and its anionic speciation in groundwater (I?), which hinders the retention by most minerals due to their negatively charged structural surfaces at near-neutral pH. AFm-SO4 is one of the phases present in cementitious materials. Experimental data suggest that the formation of solid solution between AFm-SO4 and AFm-I2 has the potential to retard 129I mobility. In order to improve the present geochemical models, thermodynamic properties of AFm-I2 and of its solid solution with AFm-SO4 were evaluated based on precipitation and dissolution experiments in aqueous solutions between 4 ¡ãC and 60 ¡ãC. The solubility product of AFm-I2 was determined at 23 ¡ãC ¡À 2 ¡ãC to be (2¦Ò) for the dissolution reaction . The Gibbs energy of formation of AFm-I2 at standard state (1 bar, 25 ¡ãC) was assessed to be ?3325.0 ¡À 2.4 (2¦Ò) kJ mol?1. The experimental data for AFm-(I2, SO4) phases were consistent with the formation of a continuous solid solution without miscibility gaps. A good fit to these data was obtained using a sub-regular solid solution model with negative Margules interaction parameters WSO4 = ?1.0 kJ mol?1 and WI = ?8.0 kJ mol?1, and end-members (Ca2Al(OH)6I and Ca4Al2(OH)12SO4) defined according to the Vanselow convention for ion exchange. The results show the potential of AFm-SO4 to act as a sink for 129I, notably in carbonate-free systems. Small amounts of calcite can hamper the formation of AFm-(I2, SO4) solid solution. The study provides relevant thermodynamic data for geochemical modeling of 129I in the cementitious near-field of a nuclear waste repository.

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