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Disordered lithium niobate rock-salt materials prepared by hydrothermal synthesis

机译:水热合成制备无序铌酸锂岩盐材料

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摘要

An investigation of the one-step hydrothermal crystallisation of lithium niobates reveals that reaction between Nb_2O_5 and aqueous LiOH at 240 °C yields materials with a disordered rock-salt structure where the metals are statistically distributed over the cation sites. This contrasts with the well-studied reaction between Nb_2O_5 and NaOH or KOH that produces ANbO_3 (A = Na, K) perovskites. Powder neutron diffraction shows that materials prepared at short reaction times and lower LiOH concentration (2.5 M) are lithium deficient and have a slight excess of niobium, but that at longer periods of reaction in 5 M LiOH, close to the ideal, stoichiometric Li_(0.75)Nb_(0.25)O composition is produced. Upon annealing this phase cleanly transforms into the known ordered rock-salt material Li_3NbO_4, a process we have followed using thermodiffractometry, which indicates that transformation begins at ~700 °C. Solid-state ~(93)Nb and ~7Li NMR of the disordered and ordered rock-salt phases shows that both contain single metal sites but there is clear evidence for local disorder in the disordered samples. For the ordered material, NMR parameters derived from experiment are also compared to those calculated using density functional theory and are shown to be in good agreement.
机译:铌酸锂的一步式水热结晶研究表明,Nb_2O_5与LiOH水溶液在240°C的反应产生具有无序岩石盐结构的材料,其中金属统计分布在阳离子位点上。这与经过深入研究的Nb_2O_5与NaOH或KOH之间产生ANbO_3(A = Na,K)钙钛矿的反应相反。粉末中子衍射表明,在较短的反应时间和较低的LiOH浓度(2.5 M)下制备的材料缺乏锂,铌含量略有过量,但是在5 M LiOH中较长的反应时间,接近理想的化学计量Li_(产生0.75)Nb_(0.25)O组成。退火后,该相便干净地转变为已知有序的岩盐材料Li_3NbO_4,我们使用热衍射法进行了跟踪,表明转变始于〜700°C。杂乱有序的岩石盐相的固态〜(93)Nb和〜7Li NMR表明,两者均包含单个金属位点,但有明确的证据表明杂乱的样品中存在局部杂乱。对于有序材料,还将实验得出的NMR参数与使用密度泛函理论计算出的NMR参数进行比较,并显示出很好的一致性。

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