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Clays and Clay Minerals; February 2006; v. 54; no. 1; p. 62-66; DOI: 10.1346/CCMN.2006.0540108
© 2006 Clay Minerals Society
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BASELINE STUDIES OF THE CLAY MINERALS SOCIETY SOURCE CLAYS: SPECIFIC SURFACE AREA BY THE BRUNAUER EMMETT TELLER (BET) METHOD

A. Umran Dogan1,2,*, Meral Dogan3, Muserref Onal4, Yuksel Sarikaya4, Aktham Aburub5,6 and Dale Eric Wurster5,7

1 Department of Geological Engineering, Ankara University, Ankara, Turkey
2 Department of Chemical and Biochemical Engineering, University of Iowa, Iowa City, Iowa, USA
3 Department of Geological Engineering, Hacettepe University, Ankara, Turkey
4 Department of Chemistry, Ankara University, Ankara, Turkey
5 College of Pharmacy, University of Iowa, Iowa City, Iowa, USA
6 Lilly Research Laboratories, Indianapolis, Indiana, USA
7 Obermann Center for Advanced Studies, University of Iowa, Iowa City, Iowa, USA

* E-mail address of corresponding author: umran-dogan{at}uiowa.edu

Specific surface area measurements of The Clay Minerals Society source clays were made by the Brunauer, Emmett and Teller (BET) method of adsorption of nitrogen gas. Two replicate measurements of specific surface area were performed for each source clay. All pair values were within 3%, which is very good agreement for this type of measurement.

Key Words: BET • Hectorite • Kaolinite • Montmorillonite • Palygorskite • Source Clays • Specific Surface Area




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M. Dogan, A. U. Dogan, F. I. Yesilyurt, D. Alaygut, I. Buckner, and D. E. Wurster
BASELINE STUDIES OF THE CLAY MINERALS SOCIETY SPECIAL CLAYS: SPECIFIC SURFACE AREA BY THE BRUNAUER EMMETT TELLER (BET) METHOD
Clays and Clay Minerals, October 1, 2007; 55(5): 534 - 541.
[Abstract] [Full Text] [PDF]


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