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Cation-Exchange Capacity (CEC) of Zeolitic Volcaniclastic Materials: Applicability of the Ammonium Acetate Saturation (AMAS) Method

Published online by Cambridge University Press:  28 February 2024

Konstantinos P. Kitsopoulos*
Affiliation:
Geology Department, Leicester University, Leicester, LEI 7RH, UK
*
E-mail of corresponding author: 111@otenet.gr

Abstract

The ammonium acetate saturation (AMAS) method was used to study the cation-exchange capacity (CEC) of zeolitic volcaniclastic materials from Santorini and Polyegos Islands, Greece. The AMAS method was tested with respect to the time required to saturate the samples of zeolites with ammonium (NH4+) ions, the efficient liberation of NH4+ ions, and the suitability of two widely used techniques to measure ammonia (NH3) (Kjeldahl ammonia distillation technique and the ammonia electrode technique). By using the inductively coupled plasma-mass spectrometry (ICP-MS) technique and measuring the number of cations exchanged during ammonium acetate (NH4OAc) saturation, it was found that the saturation period for zeolitic materials must be increased to 12-day cycles to ensure effective saturation. Following NH4OAc saturation, the AMAS method produces NH4+ solutions, after the NH4+-saturated samples of zeolites are washed with 10% NaCl. The amount of the NH4+ ions in solution (i.e., exchangeable cations) is a measure of the CEC. The NH4+ ions can not be directly measured and must be converted to NH3. The Kjeldahl ammonia distillation technique and the ammonia electrode technique for measuring NH3 give identical CEC results. However, the ammonia electrode technique, when used directly with the NH4+ samples of zeolite without 10% NaCl treatment, generally gives higher CEC values. The amount of NH4+ treated (converted to NH3), when the NH4+-saturated zeolitized samples were used directly, was higher than the amount of the NH4+ treated when the NH4+ solutions were obtained after washing the NH4+-saturated zeolitized samples with 10% NaCl. Therefore, washing with 10% NaCl does not facilitate the release of all NH4+ initially within the zeolite structure. A modified AMAS technique is proposed for measuring the CEC of zeolitic material.

Type
Research Article
Copyright
Copyright © 1999, The Clay Minerals Society

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References

Bain, D.C. Smith, B.F.L. and Wilson, M.J., 1987 Chemical analysis A Handbook of Determinative Methods in Clay Mineralogy Glasgow Blackie 248274.Google Scholar
Busenberg, E. and Clemency, C.V., 1973 Determination of the cation exchange capacity of clays and soils using an ammonia electrode Clays and Clay Minerals 21 213217 10.1346/CCMN.1973.0210403.CrossRefGoogle Scholar
Chapman, H.D. and Black, A., 1965 Cation exchange capacity Methods of Soil Analysis (Number 9 in the Series Agronomy), Part 2 Madison, Wisconsin American Institute of Agronomy 891901.Google Scholar
Fraser, A.R. and Russel, J.D., 1969 A spectrophotometric method for determination of cation exchange capacity of clay minerals Clay Minerals 8 229230 10.1180/claymin.1969.008.2.10.CrossRefGoogle Scholar
IGME, 1980 Geological map “Thera”. 1: 50,000 IGME (1980) Geological map “Thera”. 1: 50,000. Institute of Institute of Geological and Mineralogical Research of Greece (IGME), Athens .Google Scholar
Kanaris, I.T., 1989 Zeolites of the Island of Polyegos .Google Scholar
Kitsopoulos, K.P., 1995 The mineralogy, geochemistry, physical properties and possible industrial applications of volcanic zeolitic tuffs from Santorini and Polyegos islands, Greece .Google Scholar
Kitsopoulos, K.P. (1995b) The relation of the reduction of the 020 diffraction peak of heulandite with its mineral chemistry. Geological Society of America 1995 Annual Meeting, New Orleans (Louisiana, USA), November 1995, Abstract with Programs, 27, A-362.Google Scholar
Kitsopoulos, K.P., 1997 The comparison of the methylene blue absorption and ammonium acetate saturation methods for determine CEC values of volcanic zeolitic tuffs from Greece Clay Minerals 32 319322 10.1180/claymin.1997.032.2.13.CrossRefGoogle Scholar
Kitsopoulos, K.P., 1997 Genesis of heulandite group of minerals in pyroclastics (Santorini, Greece). Implications for models of zeolitization of volcaniclastic materials Zeolite ’97, 5th International Conference on the Occurrence, Properties, and Utilization of Natural Zeolites, Ischia (Naples, Italy), September 1997, Program and Abstracts 195197.Google Scholar
Kitsopoulos, K.P., 1997 The genesis of a mordenite deposit by hydrothermal alteration of pyroclastics on Polyegos island, Greece Clays and Clay Minerals 45 632648 10.1346/CCMN.1997.0450503.CrossRefGoogle Scholar
Kitsopoulos, K.P. and Dunham, A.C., 1998 Compositional variations of mordenite from Polyegos island, Greece: Na-Ca and K-rich mordenite European Journal of Mineralogy 10 569577 10.1127/ejm/10/3/0569.CrossRefGoogle Scholar
Mackenzie, R.C., 1951 A micromethod for determination of cation-exchange capacity of clays Journal of Colloid Science 6 219222.Google Scholar
Nevins, M.J. and Weintritt, D.J., 1967 Determination of CEC by methylene blue adsorption American Ceramic Society Bulletin 46 587592.Google Scholar
Noda, S., 1980 A simple method for determining the cation exchange capacity of natural zeolites Nendo Kagaku 20 7882.Google Scholar
Peech, M., 1945 Determination of exchangeable cations and exchange capacity of soils—Rapid micromethods utilizing centrifuge and spectrophotometer Soil Science 59 2538 10.1097/00010694-194501000-00005.CrossRefGoogle Scholar
Schonenberger, C.J. and Dreibelbis, F.R., 1930 Analytical methods in base-exchange investigations on soils Soil Science 30 161173 10.1097/00010694-193009000-00001.CrossRefGoogle Scholar
Schollenberger, C.J. and Simon, R.H., 1945 Determination of exchange capacity and exchangeable bases in soil. Ammonium acetate method Soil Science 59 1324 10.1097/00010694-194501000-00004.CrossRefGoogle Scholar
Tsolis-Katagas, P. and Katagas, C., 1989 Zeolites in Pre-Caldera pyroclastic rocks of the Santorini Volcano, Aegean Sea, Greece Clays and Clay Minerals 37 497510 10.1346/CCMN.1989.0370601.CrossRefGoogle Scholar