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ABSTRACT
Soil clays containing pedogenically chloritized 2:1 layer silicates, after brief contact at 25C with 2% Na2CO3 (pH 11), developed a proportionately large increment of CEC which was retained after thorough washing with neutral salts (KCl, NaCl) to reduce the pH value below 7. A soil clay from Natal, S. Africa showed the largest increase—from 2.4 meq/100 g at pH 5 to 8.0 meq/100 g after alkaline and KCl treatments. This CEC hysteresis or delta value largely disappeared when washing with a NaOAc buffer of pH 5 followed the alkaline treatment. Similar effects were absent from specimen kaolinite, montmorillonite, and vermiculite. The presence of aluminous, pedogenic chlorite was shown, by X-ray and analytical investigation, to be a common property of the soil clays exhibiting pH dependent CEC. This finding is supported by separate studies on synthetic aluminous chlorite, which showed variable CEC properties essentially identical to those of these soil clays. Release of the initially blocked isomorphous substitutional negative charge by deprotonation of the positive hydroxy alumina in aluminated soils, clays and allophane is the indicated mechanism accounting for pH dependent, hysteretic CEC charge of the mineral portion of soils.
Key Words: aluminous chlorite pH dependent CEC
1 Contribution from the Department of Soil Science, University of Wisconsin, Madison. Supported in part by a study leave grant to the first author from the Department of Agricultural Technical Services and the University of Natal, Republic of South Africa, and in part by US National Science Foundation grant GP4144-Jackson. Presented before Div. S-2 and S-5, Soil Science Society of America, Nov. 1, 1965, Columbus, Ohio.
2 Senior Lecturer, University of Natal, Pietermaritzburg, South Africa (formerly Visiting Associate Professor at Wisconsin) and Professor of Soil and Water Sciences, respectively.
Received for publication December 12, 1966. Accepted for publication March 29, 1967.
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