Journal of the Mineralogical Society of Korea (한국광물학회지)

The Mineralogical Society of Korea (한국광물학회)
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Effect of Spinning Speed on 29Si and 27Al Solid-state MAS NMR Spectra for Iron-bearing Silicate Glasses

시료의 회전 속도가 함철 비정질 규산염의 고상 NMR 신호에 미치는 영향

  • Kim, Hyo-Im (School of Earth and Environmental Science, Seoul National University) ;
  • Lee, Sung Keun (School of Earth and Environmental Science, Seoul National University)
  • 김효임 (서울대학교 지구환경과학부) ;
  • 이성근 (서울대학교 지구환경과학부)
  • Received : 2018.12.05
  • Accepted : 2018.12.18
  • Published : 2018.12.31
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Abstract

Despite the utility of solid-state NMR, NMR studies of iron-bearing silicate glasses remain a challenge because the variations in the peak position and width with increasing iron content reflect both paramagnetic effect and iron-induced structural changes. Therefore, it is essential to elucidate the effect of temperature on the NMR signal for iron-bearing silicate glasses. Here, we report the $^{29}Si$ and $^{27}Al$ MAS NMR spectra for $(Mg_{0.95}Fe_{0.05})SiO_3$ and $Fe_2O_3$-bearing $CaAl_2Si_2O_8$ (anorthite) glasses with varying spinning speed to interpret the NMR spectra for iron-bearing silicate glasses. The increase in the spinning speed results in an increase in the sample temperature. The current NMR results allow us to understand the origins of the changes in NMR signal with increasing iron content and to provide information on the dipolar interaction between nuclear spins. The $^{29}Si$ NMR spectra for $(Mg_{0.95}Fe_{0.05})SiO_3$ glass and $^{27}Al$ NMR spectra for $Fe_2O_3$-bearing $CaAl_2Si_2O_8$ glasses show that the peak shape and position of iron-bearing glasses do not change with increasing spinning speed up to 30 kHz. These results suggest that the NMR signal in the Fe-bearing glasses may stem from the 'survived nuclear spins' beyond the cutoff radius from the Fe, not from the paramagnetic shift. Based on the current results, the observed apparent shifts toward lower frequency of Al peak for $Fe_2O_3$-bearing $CaAl_2Si_2O_8$ glasses with increasing $Fe_2O_3$ at all spinning speed (15 kHz to 30 kHz) indicate the increase in the fraction of ${Q^4}_{Al}$(nSi) with lower n (i.e., 1 or 2) with increasing $Fe_2O_3$ and the spatial proximity between Fe and ${Q^4}_{Al}$(nSi) with higher n (i.e., 3 or 4). The present results show that changes in the NMR signal for iron-bearing silicate glasses reflect the actual iron-induced structural changes. Thus, it is clear that the applications of solid-state NMR for iron-bearing silicate glasses hold strong promise for unraveling the atomic structure of natural silicate glasses.

고상 핵자기공명 분광분석은 비정질의 원자 구조를 제공하는 효과적인 방법론으로 다양한 비정질 규산염의 원자구조를 규명해왔다. 하지만, 함철 비정질 규산염의 경우, 철 함량 증가에 따른 신호의 변화가 상자성 효과와 구조 변동을 모두 반영하고 있기 때문에 분석에 많은 어려움이 있다. 이에 철 함량 증가에 따른 신호 변화가 실제 구조의 변동으로부터 기인한 것인지 확인하기 위해서는 온도변화에 따른 신호의 이동 여부를 관찰하는 것이 필수적이다. 본 연구에서는 철 함량에 따른 함철 비정질 규산염의 신호 변화를 해석하기 위하여 철이 포함된 휘석과 아노르다이트 조성의 비정질의 가변회전 속도 $^{29}Si$와 $^{27}Al$ NMR 실험을 수행하였다. 이는 온도 상승에 따른 신호의 변화 여부를 확인할 수 있게 하며, 쌍극자 효과에 관한 정보를 제공한다. 함철 휘석 비정질의 $^{29}Si$ NMR과 함철 아노르다이트 비정질의 $^{27}Al$ NMR 결과, 회전 속도 증가에도 불구하고 신호의 형태 및 위치가 달라지지 않았다. 회전 속도의 증가가 신호에 변화를 야기하지 않음을 확인한 본 결과는 철 함량 증가로 인한 신호의 변화가 상자성 이동 기원이 아니라, 철로부터 컷오프 반경 너머의 생존 신호임을 지시한다. 이에 철 함량 증가에 따라 아노르다이트 비정질의 Al 신호가 음의 화학적 차폐 방향으로 이동하는 현상은, 철의 진입에 따른 ${Q^4}_{Al}$(1 또는 2Si) 비율의 상대적 증가와 철과 ${Q^4}_{Al}$(3 또는 4Si) 구조간의 높은 공간적 근접도를 지시한다. 본 결과는 철 함량에 따른 규산염 비정질의 고상 NMR 신호 변화가 실제 구조적 변화를 지시하고 있음을 보여주며, 고상 NMR이 자연계에 존재하는 각종 유리질의 구조 분석에 효과적으로 적용될 수 있음을 제시한다.

Keywords

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