ملخص
The high frequency OH-stretching band in micro-Raman spectra of kaolinites consistently exhibits two partly overlapping components with varying relative intensities. These bands, labelled A and Z, are located at ∼3700-3690 and 3690-3680 cm-1, respectively. Band Z displays greater intensity in Raman spectra of highly crystallized kaolinites which have large coherent domains. Both components are also observed in the curve fitted infrared (IR) spectra of kaolinites; band Z is stronger in IR spectra of highly crystallized samples. Data for kaolinites with different particle size support the idea that bands A and Z are the longitudinal optic and transverse optic modes of the high frequency OH-stretching band.
اللغة الأصلية | الإنجليزيّة |
---|---|
الصفحات (من إلى) | 551-563 |
عدد الصفحات | 13 |
دورية | Clay Minerals |
مستوى الصوت | 34 |
رقم الإصدار | 4 |
المعرِّفات الرقمية للأشياء | |
حالة النشر | نُشِر - ديسمبر 1999 |