Identification and characterization of Fe-rich smectites in the Camlica Region of western Turkey
CLAY MINERALS, cilt.42, sa.2, ss.153-160, 2007 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Tam Makale
- Cilt numarası: 42 Sayı: 2
- Basım Tarihi: 2007
- Doi Numarası: 10.1180/claymin.2007.042.2.02
- Dergi Adı: CLAY MINERALS
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Sayfa Sayıları: ss.153-160
- Anahtar Kelimeler: bentonite, characterization, STEM, TEM, SEM, XRD, ICP-MS, FTIR
- Dokuz Eylül Üniversitesi Adresli: Evet
Özet
Fe-rich dioctahedral smectites are the main constituent of clays in Camlica Region of Turkey. The structural, chemical and morphological characteristics of these smectites after washing are examined by X-ray diffraction, electron microscopy, inductively coupled plasma mass spectrometry and Fourier transform infrared spectroscopy. Smectite particles occur as individual flakes 0.2-2.0 mu m in size. These flakes are often aggregated into clusters up to 6.0 mu m in size.