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IR Spectroscopy of Natural and Synthetic Amethysts in the 3000―3700 cm~(-1) Region and Problem of Their Identification

机译:3000-3700 cm〜(-1)区域天然和合成紫水晶的红外光谱及其鉴定问题

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摘要

In recent years, we have scrutinized relations of formation conditions with optical absorption of natural and synthetic amethyst crystals in the 3000―3700 cm~(-1) region in order to evaluate the implication of IR spec-troscopy for their identification. We recorded and analyzed IR spectra of 580 amethyst crystals grown under standard conditions. In addition, 52 samples of natural amethyst crystals taken from deposits in Brazil, Uruguay, Bolivia, Russia, Bulgaria, and several countries of Africa were studied for comparison. The IR spectra were recorded on an Avatar 320 FT IR (Nicolet) device at room temperature in nonpolarized light. Plates (usually 2―3 mm thick) parallel to faces {c}, {x}, or other less common orientations were used. We investigated the dependence of the appearance and behavior of absorption bands on the solution composition, temperature, pressure, crystallographic orientation, growth rate, ionizing radiation (dose up to 7 Mrad, source ~(60)Co), and annealing rate at 300―700℃.
机译:近年来,我们仔细研究了形成条件与3000-3700 cm〜(-1)范围内的天然和合成紫水晶晶体的光吸收之间的关系,以评估IR光谱学对其鉴定的意义。我们记录并分析了在标准条件下生长的580个紫水晶的红外光谱。此外,还对52个从巴西,乌拉圭,玻利维亚,俄罗斯,保加利亚和几个非洲国家的矿床中提取的天然紫水晶晶体进行了比较。红外光谱是在室温下在Avatar 320 FT IR(Nicolet)设备上在非偏振光下记录的。使用平行于面{c},{x}或其他不太常见的方向的板(通常为2至3 mm厚)。我们研究了吸收带的外观和行为对溶液成分,温度,压力,晶体学取向,生长速率,电离辐射(剂量高达7 Mrad,源〜(60)Co)和在300〜 700℃。

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