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An application of near-infrared and mid-infrared spectroscopy to the study of selected minerals

机译:近红外和中红外光谱在选定矿物研究中的应用

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Near-infrared (NIR) spectroscopy is a somewhat underutilised technique for the study of minerals. The technique has the ability to determine water content, hydroxyl groups and transition metals. In this paper, we show the application of NIR spectroscopy to the study of selected minerals. The structure and spectral properties of two Cu-tellurite minerals graemite and teineite are compared with bismuth containing tellurite mineral smirnite by the application of NIR and infrared (IR) spectroscopy. The position of Cu2+ bands and their splitting in the electronic spectra of tellurites are in conformity with the octahedral geometry distortion. The spectral pattern of smirnite resembles graemite and the observed band at 10,855 cm−1 with a weak shoulder at 7920 cm−1 is identified as due to a Cu2+ ion. Any transition metal impurities may be identified by their bands in this spectral region. Three prominent bands observed in the region of 7200-6500 cm−1 are the overtones of water while the weak bands observed near 6200 cm−1 in tellurites may be attributed to the hydrogen bonding between (TeO3)2− and H2O. The observation of a number of bands centred at around 7200 cm−1 confirms molecular water in tellurite minerals. A number of overlapping bands in the low wavenumbers 4500-4000 cm−1 is the result of combinational modes of (TeO3)2− ion. The appearance of the most intense peak at 5200 cm−1 with a pair of weak bands near 6000 cm−1 is a common feature in all the spectra and is related to the combinations of OH vibrations of water molecules and bending vibrations ν2 (δ H2O). Bending vibrations δ H2O observed in the IR spectra show a single band for smirnite at 1610 cm−1. The resolution of this band into a number of components is evidenced for non-equivalent types of molecular water in graemite and teineite. (TeO3)2− stretching vibrations are characterised by three main absorptions at 1080, 780 and 695 cm−1.View full textDownload full textKeywordstellurites, graemite, teineite, smirnite, near-infrared and mid-infrared spectroscopy, Cu2+ , (TeO3)2− Related var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/10420150903456493
机译:近红外(NIR)光谱学在矿物研究中是一种未被充分利用的技术。该技术具有确定水含量,羟基和过渡金属的能力。在本文中,我们展示了近红外光谱在选定矿物研究中的应用。利用近红外光谱和红外光谱技术,比较了两种铜碲矿,闪锌矿和黄铁矿与含铋的亚碲酸盐闪锌矿的结构和光谱性质。 Cu 2 + 的位置及其在亚碲酸盐电子光谱中的分裂与八面体几何畸变一致。闪锌矿的光谱模式类似于黑闪石,观察到的波段为10,855 cm -1 ,肩部弱于7920 cm -1 ,原因是Cu 2 + 离子任何过渡金属杂质都可以通过其在该光谱区域中的谱带来识别。在水的泛音中,在7200-6500 cm â1区域中观察到的三个突出带是水的泛音,而在6200 cm â1附近观察到的弱带可能在水中归因于(TeO 3 ) 2∴ 与H 2 O之间的氢键。对围绕7200 cm s1 中心的多个带的观察证实了亚碲酸盐矿物中的分子水。低波数4500-4000 cm â1’1 中的多个重叠带是(TeO 3 ) 2−的组合模式的结果。 sup>离子。在所有光谱中,最常见的特征是在5200 cm â1处出现最强峰,并在6000 cm â1附近有一对弱带。与水分子的OH振动和弯曲振动 2 (ΔH 2 O)的组合有关。在红外光谱中观察到的弯曲振动ÂH 2 O显示了1610 cm -1 上的闪锌矿带。对于钠闪石和黄铁矿中非等价类型的分子水,已证明该谱带可分解为许多成分。 (TeO 3 )2â€拉伸振动的特征在于在1080、780和695 cm â1处的三个主要吸收。 texttell全文,关键词,碲锌矿,teineite,smirnite,近红外和中红外光谱,Cu2 +,(TeO3)2â€相关的变量addthis_config = {ui_cobrand:“ Taylor&Francis Online”,services_compact:“同胞,网络犯罪,推特, technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more“,发布:” ra-4dff56cd6bb1830b“};添加到候选列表链接永久链接http://dx.doi.org/10.1080/10420150903456493

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