期刊
CLAY MINERALS
卷 42, 期 2, 页码 153-160出版社
MINERALOGICAL SOC
DOI: 10.1180/claymin.2007.042.2.02
关键词
bentonite; characterization; STEM; TEM; SEM; XRD; ICP-MS; FTIR
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.
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