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机构地区:[1]Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China [2]Laboratory of Magnetic Resonance and Atom and Molecular Physics, Wuhan Institute of Physics, Chinese Academy of Sciences, Wuhan 430071, China
出 处:《Science China Earth Sciences》1997年第2期159-165,共7页中国科学(地球科学英文版)
基 金:Project supported by the Foundation of Magnetic Resonance and Atom and Molecular Physics,Wuhan Institute of Phyiscs,Chinese Academy of Sciences
摘 要:^(29)Si, ^(27)Al MAS NMR and IR spectra of monophase K-feldspars (sanidine, orthoclase and micro-cline) and Na-feldspars (monalbite, anorthoclase and low albite) in different structural states have been studied. The NMR and IR spectra of K-feldspars and Na-feldspars vary regularly along with their degrees of Si/Al ordering evolution. Si in orthoclase occupies T2m, T2o and T1m, and the high-temperature Na-feldspar (monalbite and anorthoclase) coincides in 29Si, 27Al NMR and IR spectra. Moreover, all the high-temperature Na-feldspars and sanidine have the same 27Al NMR and IR spectra.<sup>29</sup>Si, <sup>27</sup>Al MAS NMR and IR spectra of monophase K-feldspars (sanidine, orthoclase and micro-cline) and Na-feldspars (monalbite, anorthoclase and low albite) in different structural states have been studied. The NMR and IR spectra of K-feldspars and Na-feldspars vary regularly along with their degrees of Si/Al ordering evolution. Si in orthoclase occupies T2m, T2o and T1m, and the high-temperature Na-feldspar (monalbite and anorthoclase) coincides in 29Si, 27Al NMR and IR spectra. Moreover, all the high-temperature Na-feldspars and sanidine have the same 27Al NMR and IR spectra.
关 键 词:K-FELDSPAR Na-feldspar NMR IR ORDERING
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