首页> 外文期刊>Physics and chemistry of minerals >Characterisation of tobelite (NH_4)Al_2[AlSi_3O_(10)](OH)_2 and ND_4-tobelite (ND_4)Al_2[AlSi_3O_(10)](OD)_2 using IR spectroscopy and Rietveld refinement of XRD spectra
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Characterisation of tobelite (NH_4)Al_2[AlSi_3O_(10)](OH)_2 and ND_4-tobelite (ND_4)Al_2[AlSi_3O_(10)](OD)_2 using IR spectroscopy and Rietveld refinement of XRD spectra

机译:利用红外光谱和XRD光谱的Rietveld精炼表征Tobelite(NH_4)Al_2 [AlSi_3O_(10)] [OH)_2和ND_4-Tobelite(ND_4)Al_2 [AlSi_3O_(10)] [OD)_2

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摘要

Tobelite (NH_4) Al_2 [AlSi_3O_(10)] (OH)_2, the ammonium analogue of muscovite, and its deuterated form ND_4-tobelite (ND_4) Al_2 [AlSi_3O_(10)] (OD)_2 have been synthesised at 600 ℃ and 200 and 500 Mpa using a well homogenised, stoichiometric SiO_2-Al_2O_3 oxide mix with Al_2O_3 in excess of 5 mol% and a 25% NH_3 solution whose relative abundance was such that the amount of NH_4~+ stoichiometrically available was in excess of 50%. Characterisation of both tobelite and ND_4-tobelite using IR-spectroscopy, Rietveld refinement of X-ray powder diffraction data, and electron microprobe analysis indicate that, similar to K~+ in muscovite, the NH_4~+ or ND_4~+ molecule occupies the interlayer site. IR absorption bands caused by NH_4~+ and ND_4~+ can be explained, to a very good approximation, on the basis of T_d symmetry. Nevertheless, substantial line broadening and the occurrence of shoulders indicate a deviation from ideal T_d symmetry. However, even at 77 K, no discrete splitting of the degenerate states could be confirmed. The OH stretching frequencies observed for synthetic tobelite are quite similar to those for muscovite, indicating that the replacement of K~+ by NH_4~+ has no effect. The low FWHH of the OH bands indicate that the hydroxyl groups are well ordered within the structure. Rietveld refinement of tobelite and ND_4-tobelite indicates that all samples synthesised consist of the 3 different mica polytypes which are typical of muscovite-namely 1M (C2/m), 2M_1 (C2/c) and 2M_2 (C2/c). Tobelite and ND_4-tobelite synthesised at 500 Mpa principally contain the 1M polytype, whereas the principle polytype for ND_4-tobelite synthesised at 200 Mpa, is 2M_2. Rietveld refinement of X-ray diffraction spectra for tobelite synthesised at 200 Mpa was problematic due to the very broad FWHH of the X-ray peaks indicating poor crystallinity. In comparision to synthetic muscovite, the cell dimensions observed for tobelite and its deuterated analogue are quite similar except for the lattice constant c. Due to the larger radius of NH_4~+ or ND_4~+ compared to K~+ cation, the c-direction is expanded form 10.275 A in muscovite to approximately 10.540 A in tobelite and ND_4-tobelite.
机译:白云母的铵类似物Tobelite(NH_4)Al_2 [AlSi_3O_(10)](OH)_2及其氘代形式ND_4-tobelite(ND_4)Al_2 [AlSi_3O_(10)](OD)_2的合成温度为600℃,使用均质化良好的SiO_2-Al_2O_3氧化物与Al_2O_3的含量超过5 mol%的均匀混合的SiO_2-Al_2O_3氧化物和25%的NH_3溶液(其相对丰度使得化学计量的NH_4〜+的量超过50%)在200和500 Mpa下混合。利用红外光谱,X射线粉末衍射数据的Rietveld精炼和电子微探针分析对托贝石和ND_4-托贝石进行表征,表明与白云母中的K〜+相似,NH_4〜+或ND_4〜+分子占据了中间层现场。基于T_d对称性,可以很好地近似地解释由NH_4〜+和ND_4〜+引起的IR吸收带。然而,明显的线展宽和肩部的出现表明偏离了理想的T_d对称性。但是,即使在77 K下,也无法确认简并状态的离散分裂。合成方钠石的OH拉伸频率与白云母的拉伸频率非常相似,这表明用NH_4〜+替代K〜+没有影响。 OH带的FWHH低表明羟基在结构内排列良好。钙锰矿和ND_4-钙锰矿的Rietveld精炼表明,所有合成的样品均由3种不同的云母多型组成,这是白云母的典型特征,即1M(C2 / m),2M_1(C2 / c)和2M_2(C2 / c)。以500 Mpa合成的钠锰矿和ND_4-tobelite主要包含1M多型,而以200 Mpa合成的ND_4-tobelite的主多型为2M_2。由于X射线峰的FWHH非常宽,表明结晶度差,因此200 Mpa合成的钙锰矿的X射线衍射谱的Rietveld细化是有问题的。与合成白云母相比,除了晶格常数c外,观察到的方铁石及其氘代类似物的晶胞尺寸非常相似。由于NH_4〜+或ND_4〜+的半径比K〜+阳离子的半径大,所以c方向从白云母中的10.275 A扩展到钠锰矿和ND_4-钠锰矿中的约10.540A。

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