首页> 外文期刊>Journal of Nuclear Materials: Materials Aspects of Fission and Fusion >Enthalpies of formation of Ce-pyrochlore, Ca0.93Ce1.00Ti2.035O7.00, U-pyrochlore, Ca1.46U0.234+U0.466+Ti1.85O7.00 and Gd-pyrochlore, Gd2Ti2O7: three materials relevant to the proposed waste form for excess weapons plutonium
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Enthalpies of formation of Ce-pyrochlore, Ca0.93Ce1.00Ti2.035O7.00, U-pyrochlore, Ca1.46U0.234+U0.466+Ti1.85O7.00 and Gd-pyrochlore, Gd2Ti2O7: three materials relevant to the proposed waste form for excess weapons plutonium

机译:铈烧绿石,Ca0.93Ce1.00Ti2.035O7.00,U-烧绿石,Ca1.46U0.234 + U0.466 + Ti1.85O7.00和Gd-烧绿石,Gd2Ti2O7的形成焓:与拟议中的有关的三种材料多余武器weapons的废物形式

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High temperature oxide melt solution calorimetry was used to derive standard enthalpies of formation, AHf (kJ/mol), for three pyrochlore phases: Ca0.93Ce1.00Ti2.035O7.00 (-3656.0 +/- 5.6), Ca1.46U0.234+U0.466+Ti1.85O7.00 (-3610 +/- 4.1) and Gd2Ti2O7 (-3822.5 +/- 4.9). Enthalpy of drop solution data, DeltaH(ds), were used to calculate enthalpies of formation with respect to an oxide/perovskite phase assemblage AH(f-ox)(0): CaO + MO2 + 2TiO(2) = CaMTi2O7 or Gd2O3 + 2TiO(2) = Gd2Ti2O7, and an oxide/perovkite phas assemblage AH(f-pv+ox)(0): CaTiO3 + MO2 + TiO2 = CaMTi2O7, where M = Ce or U. All three pyrochlore samples were stable in enthalpy relative to an oxide assemblage with DeltaH(f-ox)(0) (kJ/mol) (Gd2Ti2O7) = -113.4 +/- 2.8; DeltaH(f-ox)(0)(Ca1.46U0.234+U0.466+Ti0.85O7.00) = -123.1 +/- 3.4; DeltaH(f-ox)(0)(Ca0.93Ce1.00Ti2.035O7.00) = -54.1 +/-5.2. U pyrochlore was stable in enthalpy relative to an oxide/perovskite assemblage (DeltaH(f-pv-ox)(0) = -5.1 +/- 4.0 kJ/mol). Ce-pyrochlore was metastable in enthalpy relative to the oxide/perovskite phase assemblage (DeltaH(f-pv-ox)(0) = +21.0 +/- 5.5 kJ/mol). A significant metastability field was defined with respect to an oxide.perovskite phase assemblage. However, the proposed waste form baseline composition lies in the stable regions of the phase diagrams. (C) 2002 Elsevier Science B.V. All rights reserved. [References: 59]
机译:高温氧化物熔体溶液量热法用于得出三个烧绿石相的标准形成焓AHf(kJ / mol):Ca0.93Ce1.00Ti2.035O7.00(-3656.0 +/- 5.6),Ca1.46U0.234 + U0.466 + Ti1.85O7.00(-3610 +/- 4.1)和Gd2Ti2O7(-3822.5 +/- 4.9)。液滴溶液数据的焓DeltaH(ds)用于计算相对于氧化物/钙钛矿相组件AH(f-ox)(0)的形成焓:CaO + MO2 + 2TiO(2)= CaMTi2O7或Gd2O3 + 2TiO(2)= Gd2Ti2O7,氧化物/钙钛矿相集合AH(f-pv + ox)(0):CaTiO3 + MO2 + TiO2 = CaMTi2O7,其中M = Ce或U.所有三个烧绿石样品在焓相对温度下均稳定生成具有DeltaH(f-ox)(0)(kJ / mol)(Gd2Ti2O7)= -113.4 +/- 2.8的氧化物ΔH(f-ox)(0)(Ca1.46U0.234 + U0.466 + Ti0.85O7.00)= -123.1 +/- 3.4; ΔH(f-ox)(0)(Ca0.93Ce1.00Ti2.035O7.00)= -54.1 +/- 5.2。烧绿石的焓相对于氧化物/钙钛矿组合物稳定(DeltaH(f-pv-ox)(0)= -5.1 +/- 4.0 kJ / mol)。铈烧绿石相对于氧化物/钙钛矿相组合在焓上是亚稳态的(DeltaH(f-pv-ox)(0)= +21.0 +/- 5.5 kJ / mol)。关于氧化物钙钛矿相组合定义了显着的亚稳场。但是,建议的废物形式基线组成位于相图的稳定区域。 (C)2002 Elsevier Science B.V.保留所有权利。 [参考:59]

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