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NMR evidence for formation of octahedral and tetrahedral Al and repolymerization of the Si network during dissolution of aluminosilicate glass and crystal

机译:铝硅酸盐玻璃和晶体溶解过程中形成八面体和四面体Al以及Si网络重新聚合的NMR证据

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摘要

Five sodium aluminosilicate glasses in the series Na2O: xAl2O3:(3–x) SiO2 and Na2O:Al2O3:ySiO2 were prepared and subjected to leaching at pH 2 under ambient conditions for up to 1000 h. Solid-state nuclear magnetic resonance (NMR) spectroscopy revealed the identity of aluminate and silicate environments in the leached surface layers of these glasses as well as a sample of albite crystal subjected to the same aqueous leaching. While 29Si and 27Al magic-angle spinning (MAS) NMR experiments report on the bulk structures of the samples, cross-polarization from hydrogen atoms that are present only in the surface layers provides structural information from the regions of the sample transformed during treatment. Aluminum in octahedral coordination by O atoms (AlVI) is confirmed for the first time on the near-surface region of an albite crystal under the treatment conditions of this study. A quantification of the change in the amount of six-coordinate aluminum as a function of bulk Al/Si ratio is made possible by comparing the relative amounts of 1H " BORDER="0"> 27Al CPMAS signals from AlIV and AlVI obtained from different samples under reproducible experimental conditions. The relative contribution of AlVI to total Al in the hydrated layers increases with the Al/Si ratio of the glasses studied. The leached albite crystal sample has an anomalously high concentration of AlVI given its Al/Si ratio. This anomaly is probably related to the relatively low thickness of the leached layer developed on this phase: little hydrogen penetrates the crystal surface and almost all of the Al in the thin leached layer is octahedrally coordinated, similar to Al in solution. These data suggest that hydrolysis of bridging O atoms around Al atoms in the glass or crystal hydrated layer is accompanied by a change in the coordination number of the Al atom. Aging of surfaces documents no formation of AlVI during storage after leaching. The MAS data, coupled with 27Al " BORDER="0"> 29Si CPMAS experiments, describe the bulk network structure and provide further insight into the surface structures, including documentation of repolymerization of the silicon network in the surface layer of a nepheline glass via formation of condensed Q4 units. Further triple-resonance experiments correlate 1H, 29Si, and 27Al environments in the glasses, and indicate that the repolymerized structures in nepheline glass are not phase-separated from aluminum-containing network structures. These data for acid dissolution under ambient conditions yield the first picture of the complicated series of reactions relating connectivity and coordination number of Al and Si at the altered surfaces of geologically interesting aluminosilicates.
机译:Na 2 O系列中的五个硅铝酸钠玻璃:xAl 2 O 3 :( 3-x) SiO制备了 2 和Na 2 O:Al 2 O 3 :ySiO 2 并在环境条件下于pH 2下进行 淋洗达1000小时。固态 核磁共振波谱显示了这些玻璃的浸出表面 层中铝酸盐和硅酸盐环境的身份 钠长石晶体样品 经受相同的水浸。虽然 29 Si和 27 Al 魔角旋转(MAS)NMR实验报告了该晶体的整体 结构样品中,仅存在于表面层中的氢 原子的交叉极化提供了在 处理过程中转化的样品区域的结构 信息。由O原子(Al VI 八面体配位的铝首次在 钠长石晶体的近表面区域被确认本研究的治疗条件。 量化六坐标 铝量随Al / Si体积比变化的变化 H“ BORDER =” 0“> 27 Al CPMAS信号的相对量 在可重复的 实验条件下从不同样品中获得的sup>和Al VI .Al VI 总量的相对贡献水合层中的Al随所研究玻璃的Al / Si比 而增加,浸出钠长石晶体样品的 异常高浓度的Al VI 给出其Al / Si比。 此异常可能与浸出层发育相对较低的厚度 有关在此阶段进行:几乎没有氢 穿透晶体表面,并且 薄层中几乎所有的Al都是八面体配位的,类似于Al 在解决方案中。这些数据表明,玻璃或晶体水合层 中Al原子周围的桥接 O原子的水解伴随着 铝原子。表面老化表明在浸出后的 储存期间没有形成Al VI 。 MAS数据结合 27 A1“ BORDER =” 0“> 29 Si CPMAS实验,描述了批量网络结构并提供了 深入了解表面结构,包括有关通过形成缩合Q 在霞石玻璃表面层 中硅网络进行再聚合的文档 4 单位。进一步的 三共振实验将 1 H, 29 Si和 27 Al关联起来表示玻璃中的环境 ,并表明霞石玻璃中的再聚合结构 与含铝的 网络结构没有相分离。环境 条件下酸的溶解产生了关于 Al和Si在改变后的表面上的连通性和配位数的复杂系列 的第一张图地质上有趣的 铝硅酸盐。

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  • 来源
    《American Mineralogist》 |2003年第1期|00000054-00000067|共14页
  • 作者单位

    Department of Chemistry and Materials Research Institute, Penn State University, University Park, Pennsylvania 16802, U.S.A.;

    Department of Geosciences and Materials Research Institute, Penn State University, University Park, Pennsylvania 16802, U.S.A.;

    Department of Materials Science and Engineering, and Materials Research Institute, Penn State University, University Park, Pennsylvania 16802, U.S.A.;

    Department of Materials Science and Engineering, and Materials Research Institute, Penn State University, University Park, Pennsylvania 16802, U.S.A.;

    Department of Chemistry and Materials Research Institute, Penn State University, University Park, Pennsylvania 16802, U.S.A.;

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