Hostname: page-component-669899f699-g7b4s Total loading time: 0 Render date: 2025-04-25T18:26:06.899Z Has data issue: false hasContentIssue false
  • English
  • Français

Comparison of the methylene blue absorption and the ammonium acetate saturation methods for determination of CEC values of zeolite-rich tufts

Published online by Cambridge University Press:  09 July 2018

K. P. Kitsopoulos
K. P. Kitsopoulos*
Affiliation:
Geology Department, Leicester University, Leicester, LE1 7RH, UK
Get access Rights & Permissions [Opens in a new window]

Extract

One of the most important properties of zeolitized volcaniclastic materials is the cation exchange capacity (CEC). Numerous techniques are available for measuring CEC and the methylene blue absorption (MBA) (Nevins & Weintritt, 1967) and the ammonium acetate saturation (AMAS) (Chapman, 1965) methods are two of those commonly used. The aim of this study was to compare the results obtained by the two methods when used with zeolite-rich materials.

Type
Notes
Information
Clay Minerals , Volume 32 , Issue 2 , June 1997 , pp. 319 - 322
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1997

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

References

Breck, D.W. (1974) Zeolite Molecular Sieves - Structure, Chemistry and Uses. John Wiley & Sons Inc., New York.Google Scholar
Busenberg, E. & Clemency, C.V. (1973) Determination of the cation exchange capacity of clays and soils using an ammonia electrode. Clays Clay Miner. 21, 213–217.Google Scholar
Chapman, H.D. (1965) Cation exchange capacity. Pp. 891-901 in: Methods of Soil Analysis (Black, A., editor). No. 9 in the Series Agronomy, Am. Inst. Agronomy, Madison, Wisconsin.Google Scholar
Deer, W.A., Howie, R.A. & Zussman, J. (1992) An Introduction to the Rock-Forming Minerals. Longman Group UK Limited. 2nd Edition.Google Scholar
Kipling, J.J. & Wilson, R.B. (1960) Adsorption of methylene blue in the determination of surface areas. J. Appl. Chem. 10, 109–113.CrossRefGoogle Scholar
Kitsopoulos, K.P. (1995a) The mineralogy, geochemistry, physical properties and possible industrial applications of volcanic zeolitic tuffs from Santorini and Polyegos islands, Greece. PhD thesis, Univ. Leicester, UK.Google Scholar
Kitsopoulos, K.P. (1995b) The appliance of the ammonium saturation method for measuring CEC of zeolitic tufts and the required modifications. Abstracts ‘Sofia Zeolite Meeting 95', 139-140.Google Scholar
Kitsopoulos, K.P. (1996a) Zeolitization of the Akrotiri pre-caldera pyroclastics from Santorini island, Greece. Implications for existing zeolitization models as applied with volcaniclastic materials. GSA Abstracts with Programs 1996, 28, 7, A-104.Google Scholar
Kitsopoulos, K.P. (1996b) The genesis of a mordenite deposit by hydrothermal alteration of pyroclastics on Polyegos island, Greece. Clays Clay Miner. (in press).CrossRefGoogle Scholar
Kitsopoulos, K.P. & Dunham, A.C. (1996) Heulandite and mordenite-rich volcanic tufts from Greece: a potential source for pozzolanic materials. Mineral. Deposita, 31, 576–583.CrossRefGoogle Scholar
Koyama, M. & Takeuchi, Y. (1977) Clinoptilolite: the distribution of potassium atoms and its role in thermal stability. Zeitsch. Krist. Bd. 145, 216–239.Google Scholar
Morgan, D.J. (1990) Laboratory assessment ofbentonite deposits. EC/Asian training course on assessment procedures for clays and ceramic raw materials. Ipoh, Malaysia, 14 pp.Google Scholar
Nevins, M.J. & Weintritt, D.J. (1967) Determination of CEC by methylene blue adsorption. Am. Cer. Soc. Bull. 46, 587–592.Google Scholar
Taylor, R.K. (1985) Cation exchange in clays and mudrocks by methylene blue. J. Chem. Tech. Biotechnol. 35A, 195-207.Google Scholar
Tsolis-Katagas, P. & Katagas, C. (1989) Zeolites in precaldera pyroclastic rocks of the Santorini volcano, Aegean Sea, Greece. Clays Clay Miner. 37, 497–510.Google Scholar