1982
DOI: 10.1149/1.2123480
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Solubility of Yttrium Oxide in Na2 SO 4 and NaCl Melts

Abstract: Equilibrium constants for the acidic and basic dissolution reactions of Y2O3 , Y2O3=2Y+3+3O2− , and Y2O3+O2−=2YO2− , respectively, have been measured in molten normalNaCl at 1100 K and in molten Na2SO4 at 1200 K by coulometric and potentiometric titrations. In normalNaCl , the equilibrium constants on an ion fraction scale are false(1.4–2.2false)×10−36 and false(0.7–5.5false)×10−3 , respectively; in Na2SO4 , the constants are false(4.5–6.4false)×10−31 and false(0.1–1.4false)×10−2 .

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Cited by 26 publications
(7 citation statements)
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“…If the activity coefficient of the dissolved nickel species is presumed to be constant, then a plot of the log of NiO solubility as a function of -log a(MsO) should show two distinct regimes of dissolution. [7] and [8]. This type of plot has been the primary interest of this work.…”
Section: Theoretical Backgroundmentioning
confidence: 99%
“…If the activity coefficient of the dissolved nickel species is presumed to be constant, then a plot of the log of NiO solubility as a function of -log a(MsO) should show two distinct regimes of dissolution. [7] and [8]. This type of plot has been the primary interest of this work.…”
Section: Theoretical Backgroundmentioning
confidence: 99%
“…For the crystals shown in Figure 6(b), the EDS analysis indicates that these crystals are composed of yttrium, vanadium, sodium and oxygen elements. In our experience, there is not great research done on the corrosion behaviour of silicates in molten salts containing both vanadium and sulfur compounds Jacobson, 1986;Jacobson and Fox, 1988;Deanhardt and Stern, 1982;Shi and Rapp, 1986;Rapp, 2002). However, the main mechanism present is the dissolution of 7YSZ (yttria stabilized zirconia) in the melt followed by the re-precipitation of both YVO 4 and Y-depleted (Jones, 1997;Hertl, 1988;Afrasiabi et al, 2008;Habibi et al, 2012).…”
Section: Resultsmentioning
confidence: 99%
“…At the substrate-salt interface, there is a higher PSO 3 partial pressure because of the release of acidic gases, whereas the PSO 3 partial pressure is lower at the salt-gas interface due to salt evaporation and flowing air. In acidic molten salts, it has been reported that the solubility of Y 2 O 3 increases with the acidity in a slope of 3/2 (Deanhardt and Stern, 1982;Shi and Rapp, 1986). From this, in our experiment, the Y 31 ions formed at the more acidic oxide-salt interface would transfer to the salt-gas interface due to the acidity negative solubility gradient, and re-precipitate as a Y-rich compound (4): On the other hand, it has been reported that silica has a very small solubility in acidic molten salts and the solubility is independent of the acidity (Siemers and McKee, 1982;Rapp, 2002).…”
Section: Resultsmentioning
confidence: 99%
“…Deanhardt and Stern measured the solubility of Y 2 O 3 in sodium molten salt. 27 YO 2 − formed at the substrate/salt interface, which had a high Na 2 O activity and high YO 2 − solubility, would diffuse to the salt/gas interface and reprecipitate as yttria.…”
Section: Discussionmentioning
confidence: 99%