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首页> 外文期刊>Journal of Molecular Structure >Infrared and Raman spectroscopic characterization of the silicate-carbonate mineral carletonite - KNa_4Ca_4Si_8O _(18)(CO_3)_4(OH,F)·H_2O
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Infrared and Raman spectroscopic characterization of the silicate-carbonate mineral carletonite - KNa_4Ca_4Si_8O _(18)(CO_3)_4(OH,F)·H_2O

机译:硅酸盐-碳酸盐矿物通钙石-KNa_4Ca_4Si_8O _(18)(CO_3)_4(OH,F)·H_2O的红外和拉曼光谱表征

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An assessment of the molecular structure of carletonite a rare phyllosilicate mineral with general chemical formula given as KNa _4Ca_4Si_8O_(18)(CO_3) _4(OH,F)·H_2O has been undertaken using vibrational spectroscopy. Carletonite has a complex layered structure. Within one period of c, it contains a silicate layer of composition NaKSi_8O _(18)·H_2O, a carbonate layer of composition NaCO _3·0.5H_2O and two carbonate layers of composition NaCa_2CO_3(F,OH)_(0.5). Raman bands are observed at 1066, 1075 and 1086 cm~(-1). Whether these bands are due to the CO32- ν_1 symmetric stretching mode or to an SiO stretching vibration is open to question. Multiple bands are observed in the 300-800 cm~(-1) spectral region, making the attribution of these bands difficult. Multiple water stretching and bending modes are observed showing that there is much variation in hydrogen bonding between water and the silicate and carbonate surfaces.
机译:利用振动光谱法对一种化学通式为KNa _4Ca_4Si_8O_(18)(CO_3)_4(OH,F)·H_2O的稀有页硅酸盐矿物的分子结构进行了评估。钙矾石具有复杂的层状结构。在c的一个周期内,它包含组成为NaKSi_8O_(18)·H_2O的硅酸盐层,组成为NaCO_3·0.5H_2O的碳酸盐层和两个组成为NaCa_2CO_3(F,OH)_(0.5)的碳酸盐层。在1066、1075和1086 cm〜(-1)处观察到拉曼带。这些频带是由于CO32-ν_1对称拉伸模式还是由于SiO拉伸振动引起的,这值得商question。在300-800 cm〜(-1)的光谱区域中观察到多个波段,使这些波段的归属变得困难。观察到多种水拉伸和弯曲模式,表明水与硅酸盐和碳酸盐表面之间的氢键存在很大变化。

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