The mineralogy and firing behaviour of pottery clays of the Lake Van region, eastern Turkey

Aras A., Kılıç S.

CLAY MINERALS, cilt.52, sa.4, ss.453-468, 2017 (SCI İndekslerine Giren Dergi) identifier identifier

  • Cilt numarası: 52 Konu: 4
  • Basım Tarihi: 2017
  • Doi Numarası: 10.1180/claymin.2017.052.4.04
  • Dergi Adı: CLAY MINERALS
  • Sayfa Sayıları: ss.453-468


The present study focused on the mineralogical and chemical characterization and firing behaviour of clays from the Lake Van region and compared them with the same characteristics established for two ancient pot sherds. Four pottery clays collected from Kutki and Kusluk in the Kesan Valley to the south, from Kavakbasi to the southwest and from Bardakci village on the east coast of Lake Van were analysed by X-ray diffraction to identify mineralogical composition (bulk clays and <2 mu m fractions after heating at 300-500 degrees C and ethylene glycol solvation). Further analyses were conducted to determine the size distribution, chemical composition and physical properties of test bodies derived from these clays. The in situ weathered schist forming the primary micaceous red clays which are suitable for local pottery production are characterized by large muscovite-sericite-illite and small calcite contents. In contrast, the Bardakci clays are dominated by large smectite contents and are only used sparingly in mixtures of local pottery production because they undergo firing shrinkage and present drying and firing flaws in the fired bodies. Firing ranges of similar to 800-900 degrees C were inferred from the mineralogy and colours of the two ancient sherds from Kutki. As a result of mineralogical analysis of fired and unfired test bodies of these pottery clays and pot sherds, two different types of pastes were determined for pottery production in the Lake Van region: metamorphic and volcanic paste, the former characterized by a calcite-poor and mica-sericite-rich matrix and the latter by large smectite and small calcite contents.