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Identification and characterization of Fe-rich smectites in the Çamlıca Region of western Turkey

Published online by Cambridge University Press:  09 July 2018

Y. Seki  and
K. Yurdakoç
Y. Seki
Affiliation:
Dokuz Eylül University, Faculty of Arts & Sciences, Department of Chemistry, 35160 Buca, İzmir, Turkey
K. Yurdakoç*
Affiliation:
Dokuz Eylül University, Faculty of Arts & Sciences, Department of Chemistry, 35160 Buca, İzmir, Turkey
*
*E-mail: k.yurdakoc@deu.edu.tr
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Abstract

Fe-rich dioctahedral smectites are the main constituent of clays in Çamlıca 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 μm in size. These flakes are often aggregated into clusters up to 6.0 μm in size.

Keywords

bentonitecharacterizationSTEMTEMSEMXRDICP-MSFTIR
Type
Research Article
Information
Clay Minerals , Volume 42 , Issue 2 , June 2007 , pp. 153 - 160
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2007

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