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首页> 外文期刊>The American mineralogist >A vibrational spectroscopic study of kernite to 25 GPa: Implications for the high-pressure stability of borate polyhedra
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A vibrational spectroscopic study of kernite to 25 GPa: Implications for the high-pressure stability of borate polyhedra

机译:核心核心致力的光谱研究25 GPA:对硼酸硼硼的高压稳定性的影响

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The Raman and infrared spectra of kernite [Na2B4O6(OH)(2)center dot 3H(2)O] have been characterized up to similar to 25 and 23 GPa, respectively, to explore pressure-induced changes in a structurally novel mineral that contains mixed coordination borate groups (threefold and fourfold), as well as both hydroxyl groups and water molecules. BO3 and BO4 vibrational modes are characterized in both the Raman and infrared spectra of kernite, and reassignments of some modes are made based on observed pressure shifts. Under compression to similar to 25 GPa, kernite undergoes three phase transitions: one initiates near similar to 2.5 GPa, the second occurs at similar to 7.0 GPa, and the third near 11.0 GPa. The first transition is characterized by a loss of both a subset of the Na-associated modes and a sharp OH peak, and it is fully reversible. The second transition is characterized by the loss of most of the BO3 modes, some of the BO4 modes at similar to 7 GPa, and further broadening of the H2O and OH peaks. This transition is partially reversible on decompression, but the Raman spectra indicate that the high-pressure structure and its reversion products are likely disordered. The third transition is characterized by the loss of most of the Raman and infrared modes, and it is not reversible on decompression. The decompression products from similar to 25 GPa have markedly different infrared and Raman spectra from the starting material, and appear to involve different bonding environments of boron than are present in the starting materials: thus, pressure treatment of boron-rich materials may generate novel quenchable structures. Notably, the BO3 groups in kernite are destabilized under compression, with the BO4 groups appearing to be more stable under compression. This shift in coordination may be endemic among borate glasses and crystalline borates under compression. The coordination conversion (and its products on decompression) is likely to highly depend on the detailed t
机译:核和红外光谱分别的亚克酸克隆和红外光谱分别表征了与25和23GPa相似的表征,以探讨含有的结构新型矿物的压力诱导的变化混合配位硼酸硼基团(三倍和四重),以及羟基和水分子。 BO3和BO4振动模式的特征在于Kernite的拉曼和红外光谱,并且基于观察到的压力移位进行了一些模式的重新分配。在压制到类似于25GPa的情况下,核经历三相转变:一个引发与2.5GPa相似的,第二个发生在类似于7.0GPa,第三个接近11.0 GPA。第一转变的特征在于Na相关模式的损失和锐孔峰值,并且它是完全可逆的。第二转变的特征在于丢失大部分BO3模式,一些类似于7GPa的BO4模式,以及进一步扩大H2O和OH峰。这种转变对减压部分可逆,但拉曼光谱表明高压结构及其逆转产物可能是紊乱的。第三次过渡的特点是损失大部分拉曼和红外模式,并且对减压不可逆转。从类似于25GPa类似的减压产品具有从起始材料的显着不同的红外和拉曼光谱,并且似乎涉及硼的不同粘接环境而不是在原料中存在:因此,富含硼材料的压力处理可能会产生新颖的淬火结构。值得注意的是,Kernite中的BO3组在压缩下稳定地稳定,BO4组出现在压缩下更稳定。这种在硼酸盐玻璃和压缩下的结晶硼酸盐之间的这种转变可能是流动的。协调转换(及其产品上的减压)可能高度依赖于详细的T.

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