Abstract
Under pressure and temperature conditions like those found in deep geological repositories (DGRs), rare-earth cations may react with silicates to form rare-earth disilicates. This study establishes the stability range of yttrium disilicates in response to changes in pH. The α, β, γ, and δ polymorphs of Y2Si2O7 were synthesized by the sol-gel process at temperatures between 1100 and 1650 °C and subjected to pHstat leaching tests. By measuring the Y and Si leaching rates and monitoring the transformation of the crystalline and amorphous phases, we showed that yttrium disilicates were stable at pH > 5. At pH < 5, the pH stability sequence was consistent with the temperature-dependent stabilities of Y2Si2O7 phases, with the δ polymorph showing the lowest leaching rates. Because rare-earth compounds can be used as a proxy for analogous actinide hosts, the results of this study can be used to predict the performance of engineered barriers in DGR.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Compressional wave velocity measurements through sandy sediments containing methane hydrate
- The turquoise-chalcosiderite Cu(Al,Fe3+)6(PO4)4(OH)8·4H2O solid-solution series: A Mössbauer spectroscopy, XRD, EMPA, and FTIR study
- Variability in sepiolite: Diffraction studies
- Rankamaite from the Urubu pegmatite, Itinga, Minas Gerais, Brazil: Crystal chemistry and Rietveld refinement
- Zeolitic-type Brønsted-Lowry sites distribution imaged on clinochlore
- Thermodynamic properties of alloys of gold-74/palladium-26 with variable amounts of iron and the use of Au-Pd-Fe alloys as containers for experimental petrology
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- Estimating compositions of natural ringwoodite in the heavily shocked Grove Mountains 052049 meteorite from Raman spectra
- Phase stability and compression study of (Fe0.89,Ni0.11)3S up to pressure of the Earth’s core
- The compression pathway of quartz
- Experimental investigations into the silicification of olivine: Implications for the reaction mechanism and acid neutralization
- The effect of polymorphic structure on the structural and chemical stability of yttrium disilicates
- Diffusion in yttrium aluminium garnet at the nanometer-scale: Insight into the effective grain boundary width
- Elasticity and anisotropy of Fe3C at high pressures
- Raman spectroscopy of titanomagnetites: Calibration of the intensity of Raman peaks as a sensitive indicator for their Ti content
- Experimental determination of stability relations between monazite, fluorapatite, allanite, and REE-epidote as a function of pressure, temperature, and fluid composition
- Quantum-mechanical calculations of the Raman spectra of Mg- and Fe-cordierite
- Coarsening kinetics of coexisting peristerite and film microperthite over 104 to 105 years
- Local structure variations observed in orthoenstatite at high pressures
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- Effect of hydration on the single-crystal elasticity of Fe-bearing wadsleyite to 12 GPa
- Early Proterozoic weathering processes under low O2 conditions reconstructed from a 2.45 Ga paleosol in Pronto, Canada
- Eliseevite, Na1.5Li[Ti2Si4O12.5(OH)1.5]∙2H2O, a new microporous titanosilicate from the Lovozero alkaline massif (Kola Peninsula, Russia)
- The development of shape- and crystallographic-preferred orientation in CaPtO3 post-perovskite deformed in pure shear
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