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Baseline studies of the clay minerals society source clays: Specific surface area by the Brunauer Emmett Teller (BET) method

Published online by Cambridge University Press:  01 January 2024

A. Umran Dogan ,
Meral Dogan ,
Muserref Onal ,
Yuksel Sarikaya ,
Aktham Aburub  and
Dale Eric Wurster
A. Umran Dogan*
Affiliation:
Department of Geological Engineering, Ankara University, Ankara, Turkey Department of Chemical and Biochemical Engineering, University of Iowa, Iowa City, Iowa, USA
Meral Dogan
Affiliation:
Department of Geological Engineering, Hacettepe University, Ankara, Turkey
Muserref Onal
Affiliation:
Department of Chemistry, Ankara University, Ankara, Turkey
Yuksel Sarikaya
Affiliation:
Department of Chemistry, Ankara University, Ankara, Turkey
Aktham Aburub
Affiliation:
College of Pharmacy, University of Iowa, Iowa City, Iowa, USA Lilly Research Laboratories, Indianapolis, Indiana, USA
Dale Eric Wurster
Affiliation:
College of Pharmacy, University of Iowa, Iowa City, Iowa, USA Obermann Center for Advanced Studies, University of Iowa, Iowa City, Iowa, USA
*
*E-mail address of corresponding author: umran-dogan@uiowa.edu
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Abstract

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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.

Keywords

BETHectoriteKaoliniteMontmorillonitePalygorskiteSource ClaysSpecific Surface Area
Type
Research Article
Information
Clays and Clay Minerals , Volume 54 , Issue 1 , February 2006 , pp. 62 - 66
Copyright
Copyright © 2006, The Clay Minerals Society

References

Borden, D. and Griese, R.F., (2001) Baseline studies of The Clay Minerals Society Source Clays: Cation exchange capacity measurements by the ammonia-electrode method Clays and Clay Minerals 49 444–445 10.1346/CCMN.2001.0490510.CrossRefGoogle Scholar
Brunauer, S. Deming, L.S. Deming, D.M. and Teller, E., (1940) On a theory of the van der Waals adsorption of gases Journal of the American Chemical Society 62 1723–1732 10.1021/ja01864a025.CrossRefGoogle Scholar
Brunauer, S. Emmett, P.H. and Teller, E., (1938) Adsorption of gases in multimolecular layers Journal of the American Chemical Society 60 309–319 10.1021/ja01269a023.CrossRefGoogle Scholar
Chipera, S.J. and Bish, D.L., (2001) Baseline studies of The Clay Minerals Society Source Clays: Powder X-ray diffraction analyses Clays and Clay Minerals 49 398–409 10.1346/CCMN.2001.0490507.CrossRefGoogle Scholar
Costanzo, P.M., (2001) Baseline studies of The Clay Minerals Society Source Clays: Introduction Clays and Clay Minerals 49 372–373 10.1346/CCMN.2001.0490502.CrossRefGoogle Scholar
Elzea Kogel, J. and Lewis, S.A., (2001) Baseline studies of The Clay Minerals Society Source Clays: Chemical analyses by inductively coupled plasma-mass spectroscopy (ICP-MS) Clays and Clay Minerals 49 387–392 10.1346/CCMN.2001.0490505.CrossRefGoogle Scholar
Emmett, P.H. and Brunauer, S., (1937) The use of low temperature van der Waals’ adsorption isotherms in determining the surface areas of various adsorbents Journal of the American Chemical Society 59 2682–2689 10.1021/ja01291a060.CrossRefGoogle Scholar
Fischer, C. and Gaupp, R., (2004) Multi-scale rock surface area quantification — a systematic method to evaluate the reactive surface area of rocks Chemie der Erde 64 241–256 10.1016/j.chemer.2003.12.002.CrossRefGoogle Scholar
Gregg, S. and Sing, K.S.W., (1982) Adsorption, Surface Area, and Porosity London Academic Press.Google Scholar
Grim, R.E., (1968) Clay Mineralogy 2nd New York McGraw-Hill.Google Scholar
Guggenheim, S. and van Koster Groos, A.F., (2001) Baseline studies of The Clay Minerals Society Source Clays: Thermal analyses Clays and Clay Minerals 49 433–443 10.1346/CCMN.2001.0490509.CrossRefGoogle Scholar
IUPAC, Reporting Physisorption Data for Gas/Solid Systems Pure and Applied Chemistry (1985) 57 603–619 10.1351/pac198557040603.Google Scholar
Madejová, J. and Komadel, P., (2001) Baseline studies of The Clay Minerals Society Source Clays: Infrared methods Clays and Clay Minerals 49 410–432 10.1346/CCMN.2001.0490508.CrossRefGoogle Scholar
Makower, B. Shaw, T.M. and Alexander, L.T., (1937) The specific surface and density of soils and their colloids Soil Science Society of America Proceedings 2 101–108 10.2136/sssaj1938.036159950002000C0016x.CrossRefGoogle Scholar
Mermut, A.R. and Cano, A.F., (2001) Baseline studies of The Clay Minerals Society Source Clays: Chemical analyses of major elements Clays and Clay Minerals 49 381–386 10.1346/CCMN.2001.0490504.CrossRefGoogle Scholar
Mermut, A.R. and Lagaly, G., (2001) Baseline studies of The Clay Minerals Society Source Clays: Layer-charge determination and characteristics of those minerals containing 2:1 layers Clays and Clay Minerals 49 393–397 10.1346/CCMN.2001.0490506.CrossRefGoogle Scholar
Moll, W.F. Jr., (2001) Baseline studies of The Clay Minerals Society Source Clays: Geological origin Clays and Clay Minerals 49 374–380 10.1346/CCMN.2001.0490503.CrossRefGoogle Scholar
Nelson, R.A. and Hendricks, S.B., (1944) Specific surface of some clay minerals, soils, and soil colloids Soil Science 56 285–296 10.1097/00010694-194310000-00004.CrossRefGoogle Scholar
Ritter, H.L. and Drake, L.C., (1945) Pore size distribution in porous materials. I. Pressure porosimeter and determination of complete macropore size distributions Industrial Engineering Chemical Analysis Edition 17 782–786 10.1021/i560148a013.CrossRefGoogle Scholar
Ritter, H.L. and Drake, L.C., (1945) Pore size distribution in porous materials. II. Macropore size distributions in some typical porous substances Industrial Engineering Chemical Analysis Edition 17 787–791 10.1021/i560148a014.Google Scholar
Rootare, H.M. and Prenzlow, C.F., (1967) Surface areas from mercury porosimeter measurements Journal of Physical Chemistry 71 2733–2736 10.1021/j100867a057.CrossRefGoogle Scholar
Rouquerol, F. Rouquerol, J. and Sing, K., (1999) Adsorption by Powders and Porous Solids London Academic Press.Google Scholar
Van Olphen, H. and Fripiat, J J, (1979) Data Handbook for Clay Minerals and Other Non-metallic Minerals Oxford, England Pergamon Press.Google Scholar
Wardlaw, N.C. and McKellar, M., (1981) Mercury porosimetry and the interpretation of pore geometry in sedimentary rocks and artificial models Powder Technology 29 127–143 10.1016/0032-5910(81)85011-5.CrossRefGoogle Scholar
Washburn, E.W., (1921) The dynamics of capillary flow Physics Review Series 2 17 273–283.Google Scholar
Wu, W., (2001) Baseline studies of The Clay Minerals Society Source Clays: Colloid and surface phenomena Clays and Clay Minerals 49 446–452 10.1346/CCMN.2001.0490511.CrossRefGoogle Scholar