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矿物迈耶霍夫石 CaB3O3(OH)5·H2O 的振动光谱——分子结构评估。

Vibrational spectroscopy of the mineral meyerhofferite CaB3O3(OH)5·H2O--an assessment of the molecular structure.

机构信息

School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, Brisbane, Queensland 4001, Australia.

出版信息

Spectrochim Acta A Mol Biomol Spectrosc. 2013 Oct;114:27-32. doi: 10.1016/j.saa.2013.05.016. Epub 2013 May 20.

Abstract

Meyerhofferite is a calcium hydrated borate mineral with ideal formula: CaB3O3(OH)5·H2O and occurs as white complex acicular to crude crystals with length up to ~4 cm, in fibrous divergent, radiating aggregates or reticulated and is often found in sedimentary or lake-bed borate deposits. The Raman spectrum of meyerhofferite is dominated by intense sharp band at 880 cm(-1) assigned to the symmetric stretching mode of trigonal boron. Broad Raman bands at 1046, 1110, 1135 and 1201 cm(-1) are attributed to BOH in-plane bending modes. Raman bands in the 900-1000 cm(-1) spectral region are assigned to the antisymmetric stretching of tetrahedral boron. Distinct OH stretching Raman bands are observed at 3400, 3483 and 3608 cm(-1). The mineral meyerhofferite has a distinct Raman spectrum which is different from the spectrum of other borate minerals, making Raman spectroscopy a very useful tool for the detection of meyerhofferite in sedimentary and lake bed deposits.

摘要

镁硼钙石是一种水化钙硼酸盐矿物,理想的化学式为 CaB3O3(OH)5·H2O,呈白色复合针状至粗晶,长可达约 4 厘米,呈纤维状发散、辐射状聚集体或网状,通常存在于沉积或湖底硼酸盐矿床中。镁硼钙石的拉曼光谱主要由 880 cm(-1)处的强尖锐带主导,归因于三角硼的对称伸缩模式。1046、1110、1135 和 1201 cm(-1)处的宽拉曼带归因于 BOH 面内弯曲模式。900-1000 cm(-1)光谱区域的拉曼带归因于四面体硼的反对称伸缩。在 3400、3483 和 3608 cm(-1)处观察到明显的 OH 伸缩拉曼带。镁硼钙石具有独特的拉曼光谱,与其他硼酸盐矿物的光谱不同,使拉曼光谱成为检测沉积和湖底矿床中镁硼钙石的非常有用的工具。

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