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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Fluorine speciation as a function of composition in peralkaline and peraluminous Na_2O–CaO–Al_2O_3–SiO_2 glasses: A multinuclear NMR study
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Fluorine speciation as a function of composition in peralkaline and peraluminous Na_2O–CaO–Al_2O_3–SiO_2 glasses: A multinuclear NMR study

机译:氟形态与高碱性碱和高铝酸钠Na_2O–CaO–Al_2O_3–SiO_2玻璃组成的关系:多核NMR研究

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摘要

The incorporation mechanisms of fluorine (F) into peralkaline and peraluminous Na_2O–CaO aluminosilicate glasses with ~65 mol% SiO_2 (model system for phonolites) were investigated by magic angle spinning (MAS) nuclear magnetic resonance (NMR) spectroscopy. In ~(19)F MAS NMR spectra of the fluorine-bearing peralkaline glasses at least five F sites could be distinguished, while only three of these sites could be found in the corresponding peraluminous glasses, which shows that there are more F incorporation mechanisms in peralkaline than in peraluminous glasses. In the peralkaline glasses containing up to 6.2 mol% F the following F environments were identified: F–Ca(n) at ~-113 ppm, Si–F–Na(n) or Al–F–Ca(n) at ~-146 ppm, Al–F–Al at ~-168 ppm, Al–F–Na(n) at ~-188 ppm and F–Na(n) at ~-225 ppm ("n" indicates that the number of atoms is variable or uncertain). F–Ca(n) is the most abundant site which is surprising as Ca is the least common cation in the glasses. The fraction of F–Ca(n) sites increases from 42% to 53% as the F content increases from 1.2 to 6.2 mol%. The addition of up to 16.5 mol% (5.3 wt%) water strongly affects F speciation in peralkaline glasses and results in a decrease in the fraction of F–Al sites compared to F–Ca(n) sites. It seems that hydroxyl groups (OH) and F occupy similar Al environments and that F cannot compete with OH. In the peraluminous glasses containing up to 18.3 mol% F only three F environments Si–F–Na(n) or Al–F–Ca(n) at ~-149 ppm, Al–F–Al at ~-170 ppm and Al–F–Na(n) at ~-190 ppm are observed. Al–F–Na(n) is the most abundant site with a fraction of 54–61%. The F speciation also changes with the F concentration, with a minimum in Al–F–Na(n) sites between 3.5 and 9.7 mol% F. Fluorine has only a small effect on the ~(23)Na and ~(29)Si MAS NMR spectra. ~(27)Al MAS NMR spectra of the peralkaline glasses show only four-coordinated Al while in the peraluminous glasses ~5% of the Al was found to be five-coordinated. The amount of five-coordinate Al does not change with increasing F content, but the environment of the five-coordinate Al becomes more symmetric with increasing F.
机译:通过魔角旋转(MAS)核磁共振(NMR)光谱研究了氟(F)掺入高碱性碱和含约65 mol%SiO_2的高铝酸钠Na_2O-CaO铝硅酸盐玻璃中的掺入机理。在含氟的高碱性玻璃的〜(19)F MAS NMR光谱中,至少可以分辨出五个F位置,而在相应的铝质玻璃中只能发现其中三个位置,表明在F中存在更多的F结合机理。与碱性玻璃相比,碱性高。在含有高达6.2 mol%F的碱性玻璃中,鉴定出以下F环境:〜-113 ppm时的F–Ca(n),~~时的Si–F–Na(n)或Al–F–Ca(n)。 146 ppm,〜-168 ppm的Al–F–Al,〜-188 ppm的Al–F–Na(n)和〜-225 ppm的F–Na(n)(“ n”表示原子数为可变或不确定)。 F–Ca(n)是最丰富的位点,令人惊讶,因为Ca是玻璃中最不常见的阳离子。随着F含量从1.2 mol%增加到F–Ca(n)部位的分数从42%增加到53%。添加最多16.5 mol%(5.3 wt%)的水会强烈影响过碱性玻璃中的F形态,与F-Ca(n)部位相比,导致F-Al部位的比例减少。似乎羟基(OH)和F占据着相似的Al环境,并且F无法与OH竞争。在含氟量高达18.3 mol%的高铝玻璃中,只有三种F环境,Si-F–Na(n)或Al–F–Ca(n)处于〜-149 ppm,Al–F–Al处于〜-170 ppm和Al观察到〜-190 ppm的–F–Na(n)。 Al–F–Na(n)是含量最高的站点,占54–61%的比例。 F的形态也随F的浓度而变化,在Al–F–Na(n)中的F含量最小,介于3.5和9.7 mol%F之间。氟对〜(23)Na和〜(29)Si的影响很小MAS NMR谱。高碱性玻璃的〜(27)Al MAS NMR光谱显示只有四配位的Al,而在高铝玻璃中,发现约5%的Al是五配位的。五坐标Al的量不随F含量的增加而变化,但是五坐标Al的环境随着F的增加变得更加对称。

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