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In situ spectroscopic study of water intercalation into talc: New features of 10 angstrom phase formation

机译:水嵌入滑石的原位光谱研究:10埃相形成的新特征

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The synthesis of 10 angstrom phase via the reaction of talc plus water at 8 GPa and 500 degrees C was studied by in situ Raman spectroscopy using a diamond-anvil cell. The initial fast (2 h) incorporation of interlayer H2O molecules into the talc structure is traced by gradual growth of new OH stretching bands at 3592 and 3621 cm(-1) and the shift of several framework bands. Further monitoring at HP-HT conditions over 7 h reveals gradual weakening of the 3592 cm(-1) band, which can probably be related to the onset of the formation of "long-run" 10 angstrom phase through the appearance of silanol groups following the model proposed by Pawley et al. (2010), influencing the interlayer hydrogen bonding.
机译:通过滑石与水在8 GPa和500摄氏度下的反应合成10埃相,使用金刚石-砧池通过原位拉曼光谱研究。最初的快速(2 h)层间H2O分子掺入滑石结构的过程是由新的OH拉伸带在3592和3621 cm(-1)处的逐渐生长以及几个构架带的移动所引起的。在7小时内在HP-HT条件下进行的进一步监测显示3592 cm(-1)谱带逐渐减弱,这可能与通过以下硅烷醇基团的出现形成“长期”的10埃相有关Pawley等人提出的模型。 (2010年),影响层间氢键。

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