...
首页> 外文期刊>The American mineralogist >An infrared spectroscopic study of the OH stretching frequencies of talc and 10-A phase to 10 GPa
【24h】

An infrared spectroscopic study of the OH stretching frequencies of talc and 10-A phase to 10 GPa

机译:滑石和10-A相至10 GPa的OH拉伸频率的红外光谱研究

获取原文
获取原文并翻译 | 示例
           

摘要

The effects of pressure on the OH stretching frequencies of natural talc and two samples of synthetic 10-angstrom phase have been measured using a diamond-anvil cell and a synchrotron infrared source. The 10-A phase was synthesized at 6.0-6.5 GPa, 600 degrees C for 46 hours (sample 10 angstrom-46) and 160 hours (10 angstrom-160). Spectra were collected up to 9.0 GPa (talc), 9.9 GPa (10 angstrom-46), and 9.6 GPa (10 angstrom-160). The OH stretching vibration of Mg3OH groups in talc occurs at 3677 cm(-1) at ambient pressure, and increases linearly with pressure at 0.97(2) cm(-1) GPa(-1). The same vibration occurs in 10-angstrom phase, but shows negligible pressure shift up to 2 GPa, above which the frequency increases linearly to the maximum pressure studied, at a rate of 0.96(3) cm(-1) GPa(-1) (10 angstrom-46) and 0.87(3) cm(-1) GPa(-1) (10 angstrom-160). Two other prominent bands in the 10-angstrom phase spectrum are suggested to be due to stretching of interlayer H2O, hydrogen-bonded to the nearest tetrahedral sheet. These bands also show little change over the first 2 GPa of compression, as most of the compression of the structure is taken up by closing non-hydrogen bonded gaps between interlayer H2O and tetrahedral sheets. Between 2 and 4 GPa, changes in band intensities suggest a rearrangement of the interlayer H2O.
机译:压力对天然滑石和合成10埃相的两个样品的OH拉伸频率的影响已使用钻石砧盒和同步加速器红外光源进行了测量。 10-A相在6.0-6.5 GPa,600摄氏度,46小时(样品10埃-46)和160小时(10埃-160)下合成。收集的光谱高达9.0 GPa(滑石),9.9 GPa(10埃-46)和9.6 GPa(10埃-160)。在环境压力下,滑石中Mg3OH基团的OH拉伸振动发生在3677 cm(-1)处,并且在0.97(2)cm(-1)GPa(-1)处随压力线性增加。相同的振动发生在10埃相中,但显示出高达2 GPa的可忽略的压力偏移,在此之上,频率线性增加至研究的最大压力,速率为0.96(3)cm(-1)GPa(-1) (10埃-46)和0.87(3)cm(-1)GPa(-1)(10埃-160)。有人建议在10埃相谱中出现另外两个明显的带,这是由于氢键合到最接近的四面体片的中间层H2O的拉伸。这些条带在压缩的前2 GPa上也显示很小的变化,因为结构的大部分压缩是通过封闭层间H2O和四面体片之间的非氢键结合间隙来吸收的。在2 GPa和4 GPa之间,谱带强度的变化表明中间层H2O发生了重排。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号