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Low temperature synthesis and characterisation of lecontite, (NH4)Na(SO4)·2H20

机译:(NH4 )Na(SO4 )·2H2 0的方铁矿的低温合成与表征

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摘要

Lecontite, (NH4)Na(SO4).2H2O, was synthesised at room temperature in high purity compared to earlier work with a minor impurity of mascagnite, (NH4)2SO4. Rietveld refinement of the XRD results confirmed the crystal structure and unit cell dimensions as published earlier. Raman and Infrared spectroscopy, in conjunction with factor group analysis, resulted in a complex pattern of overlapping sulphate, NH and OH modes. The NH modes υ1 was observed around 2880 cm−1, υ2 around 1700 cm−1 overlapping with water OH-bending modes, υ3 around 3300 cm−1 overlapping with water OH-stretching modes around 3023, 3185 and 3422 cm−1, and υ4 around 1432, 1447 and 1462 cm−1. The sulphate group in the crystal structure displays a decrease in symmetry from T d as evidenced by the activation of the ν1 mode at 982 cm−1 and the ν2 mode around 452 cm−1 in the Infrared spectrum. The υ3 mode shows clear splitting in the infrared spectra with a strong band at 1064 cm−1 accompanied by two shoulders at 1107 and 1139 cm−1. The Raman spectra show three weak bands at 1068, 1109 and 1135 cm−1 with a shoulder at 1155 cm−1. Similar splitting was observed for the υ4 mode around 611 and 632 cm−1 in the Infrared and Raman spectra, respectively.
机译:与较早的工作与少量的锡石杂质(NH4 )相比,在室温下以高纯度合成了Lecontite(NH4 )Na(SO4 )。2H2 O。 )2 SO4 。 XRD结果的Rietveld改进证实了晶体结构和晶胞尺寸,如先前所发表。拉曼光谱和红外光谱结合因子组分析导致硫酸盐,NH和OH模式重叠的复杂模式。 NH模式υ1在2880 cm−1 附近观察到,υ2在1700 cm−1 与水OH弯曲模式重叠,υ3在3300 cm附近观察到-1 与水的OH拉伸模式在3023、3185和3422 cm-1 和υ4在1432、1447和1462 cm-1 附近重叠。晶体结构中的硫酸根基团相对于T d 呈对称性下降,这在982 cm-1 处的ν1模和周围的ν2模被激活所证明。红外光谱中为452 cm-1 。 υ3模式在红外光谱中显示清晰的分裂,在1064 cm-1 处有很强的谱带,并在1107和1139 cm-1 处有两个肩部。拉曼光谱显示在1068、1109和1135 cm-1 处的三个弱带,其肩部在1155 cm-1 。在红外光谱和拉曼光谱中,分别在611和632 cm-1 附近的υ4模式观察到类似的分裂。

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  • 来源
    《Journal of Materials Science》 |2006年第11期|3535-3539|共5页
  • 作者单位

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of Technology;

    Department of Mineral Resources Geological Survey of Norway;

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of TechnologyAnalytical Electron Microscopy Facility Queensland University of Technology;

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of Technology;

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of Technology;

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of Technology;

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