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EXAFS study of rare-earth element coordination in calcite

机译:方解石中稀土元素配位的EXAFS研究

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Extended X-ray absorption fine-structure (EXAFS) spectroscopy is. used to characterize the local coordination of selected rare-earth elements (Nd3+, Sm3+, Dy3+, Yb3+) coprecipitated with calcite in minor concentrations from room-temperature aqueous solutions. Fitting results confirm substitution in the Ca site, but first-shell Nd-O and Sm-O distances are longer than the Ca-O distance in calcite and longer than what is consistent with ionic radii sums for sixfold coordination in the octahedral Ca site. In contrast, first-shell Dy-O and Yb-O distances are shorter than the Ca-O distance and are consistent with ionic radii sums for sixfold coordination. Comparison of Nd-O and Sm-O bond lengths with those in lanthanide sesquioxides and with ionic radii trends across the lanthanide series suggests that Nd3+ and Sm3+ have sevenfold coordination in a modified Ca site in calcite. This would require some disruption of the local structure, with an expected decrease in stability, and possibly a different charge compensation mechanism between Nd and Sm vs. Yb and Dy. A possible explanation for the increased coordination for the larger rare-earth elements involves bidentate ligation from a CO3 group. Because trivalent actinides such as Am3+ and Cm3+ have ionic radii similar to Nd3+, their incorporation in calcite may result in a similar defect structure. Copyright (C) 2002 Elsevier Science Ltd. [References: 34]
机译:是扩展的X射线吸收精细结构(EXAFS)光谱仪。用于表征与室温水溶液中少量方解石共沉淀的选定稀土元素(Nd3 +,Sm3 +,Dy3 +,Yb3 +)的局部配位。拟合结果证实了在Ca位点的取代,但第一壳Nd-O和Sm-O的距离长于方解石中的Ca-O距离,并且长于八面体Ca位点六倍配位的离子半径总和。相反,第一壳的Dy-O和Yb-O距离比Ca-O距离短,并且与离子半径总和保持六重配位。 Nd-O和Sm-O键长与镧系元素倍半氧化物中的键长以及整个镧系元素的离子半径趋势的比较表明,Nd3 +和Sm3 +在方解石的修饰Ca位置具有七倍配位。这将需要局部结构的某些破坏,以至于预期的稳定性下降,并且可能在Nd和Sm与Yb和Dy之间形成不同的电荷补偿机制。对于更大的稀土元素增强协调性的一种可能解释是来自CO3组的双齿连接。由于三价act系元素(例如Am3 +和Cm3 +)具有类似于Nd3 +的离子半径,因此它们掺入方解石中可能会导致相似的缺陷结构。版权所有(C)2002 Elsevier Science Ltd. [参考:34]

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