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Thermal Stability and Proton Conductivity of Rare Earth Orthophosphate Hydrates

机译:稀土正磷酸盐水合物的热稳定性和质子传导率

摘要

Hydrated orthophosphate powders of three rare earth metals, lanthanum, neodymium and gadolinium, were prepared and studied as potential proton conducting materials for intermediate temperature electrochemical applications. The phosphates undergo a transformation from the rhabdophane structure to the monazite structure upon dehydration. The thermal stability of the hydrate is studied and found to contain water of two types, physically adsorbed and structurally bound hydrate water. The adsorbed water is correlated to the specific surface area and can be reversibly recovered when dehydrated as long as the rhabdophane structure is preserved. The bound hydrate water is accommodated in the rhabdophane structure and is stable at temperatures of up to 650 oC. The thermal stability of the hydrate water and the phosphate structure are of significance for the proton conductivity. The LaPO4·0.6H2O and NdPO4•0.5H2O exhibited the structure dependence of the proton conductivity while the GdPO4•0.5H2O showed a large effect of the phosphate morphology.
机译:制备了三种稀土金属镧,钕和and的水合正磷酸盐粉末,并将其用作中温电化学应用的潜在质子传导材料。脱水后,磷酸盐从横纹烷结构转变为独居石结构。研究了水合物的热稳定性,发现其中包含两种类型的水:物理吸附的水合物和结构结合的水合物水。吸附的水与比表面积相关,并且只要保持大黄烷的结构就可以在脱水时可逆地回收。结合的水合物水被容纳在大黄烷结构中,并在高达650 oC的温度下稳定。水合物水的热稳定性和磷酸盐结构对于质子传导性是重要的。 LaPO4·0.6H2O和NdPO4·0.5H2O表现出质子传导性的结构依赖性,而GdPO4·0.5H2O表现出很大的磷酸盐形态影响。

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