Fernandes Arantxa, Moran Robert F, Sneddon Scott, Dawson Daniel M, McKay David, Bignami Giulia P M, Blanc Frédéric, Whittle Karl R, Ashbrook Sharon E
School of Chemistry, EaStCHEM and Centre of Magnetic Resonance, University of St Andrews, St Andrews KY16 9ST, UK. Email:
Department of Chemistry, Stephenson Institute for Renewable Energy, University of Liverpool, Crown Street, Liverpool, L69 7ZD, UK.
RSC Adv. 2018 Feb 13;8(13):7089-7101. doi: 10.1039/c8ra00596f. Epub 2018 Feb 14.
The potential of O NMR spectroscopy for the investigation of ABO ceramic oxides important in the encapsulation of radioactive waste is demonstrated, with post-synthetic enrichment by exchange with O gas. For YSnO, YTiO and LaSnO pyrochlores, enrichment of the two distinct O species is clearly non quantitative at lower temperatures (∼700 °C and below) and at shorter times, despite these being used in prior work, with preferential enrichment of OAB favoured over that of OA. At higher temperatures, the O NMR spectra suggest that quantitative enrichment has been achieved, but the integrated signal intensities do not reflect the crystallographic 1 : 6 (O1 : O2) ratio until corrected for differences in relaxation rates and, more importantly, the contribution of the satellite transitions. O NMR spectra of YZrO and YHfO defect fluorites showed little difference with any variation in enrichment temperature or time, although an increase in the absolute level of enrichment (up to ∼7.5%) was observed at higher temperature. DFT calculations show that the six distinct resonances observed cannot be assigned unambiguously, as each has contributions from more than one of the five possible next nearest neighbour environments. For LaTiO, which adopts a layered perovskite-like structure, little difference in the spectral intensities is observed with enrichment time or temperature, although the highest absolute levels of enrichment (∼13%) were obtained at higher temperature. This work demonstrates that O NMR has the potential to be a powerful probe of local structure and disorder in oxides, but that considerable care must be taken both in choosing the conditions for O enrichment and the experimental acquisition parameters if the necessary quantitative measurements are to be obtained for more complex systems.
通过与(^{18}O)气体交换进行合成后富集,展示了(^{17}O)核磁共振光谱在研究放射性废物封装中重要的ABO陶瓷氧化物方面的潜力。对于(YSnO)、(YTiO)和(LaSnO)烧绿石,在较低温度(约(700^{\circ}C)及以下)和较短时间内,两种不同的(^{18}O)物种的富集显然是非定量的,尽管这些在先前的工作中被使用,(^{18}O_{AB})的优先富集优于(^{18}O_{A})。在较高温度下,(^{17}O)核磁共振光谱表明已实现定量富集,但在对弛豫率差异以及更重要的卫星跃迁贡献进行校正之前,积分信号强度并不反映晶体学的(1:6)((O1:O2))比例。(YZrO)和(YHfO)缺陷萤石的(^{17}O)核磁共振光谱在富集温度或时间的任何变化下都显示出很小的差异,尽管在较高温度下观察到富集绝对水平有所增加(高达约(7.5%))。密度泛函理论计算表明,观察到的六个不同共振不能明确归属,因为每个共振都来自五个可能的次近邻环境中的多个环境的贡献。对于具有层状钙钛矿样结构的(LaTiO),在富集时间或温度下观察到光谱强度的差异很小,尽管在较高温度下获得了最高的绝对富集水平(约(13%))。这项工作表明,(^{17}O)核磁共振有潜力成为氧化物中局部结构和无序的有力探针,但如果要对更复杂的系统进行必要的定量测量,在选择(^{18}O)富集条件和实验采集参数时都必须格外小心。