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Organomineral gel and ion-exchange properties of soils

Organomineral gel and ion-exchange properties of soils ISSN 0012-5008, Doklady Chemistry, 2006, Vol. 411, Part 2, pp. 230–233. © Pleiades Publishing, Inc., 2006. Original Russian Text © G.N. Fedotov, Yu.D. Tret’yakov, E.I. Pakhomov, 2006, published in Doklady Akademii Nauk, 2006, Vol. 411, No. 5, pp. 633–637. CHEMISTRY a b a G. N. Fedotov , Academician Yu. D. Tret’yakov , and E. I. Pakhomov Received July 21, 2006 DOI: 10.1134/S0012500806120032 Ion-exchange capacity, one of the most important water capacity [8]. Toluene was added to inhibit the soil properties, has long attracted the attention of microbial activity [9]. Vessels with soils were tightly researchers [1]. However, the ion-exchange mechanism covered, and samples were taken every day. is not fully understood [2]. Soil extracts were prepared as follows: a 20-g soil sample was placed in 50 ml of deionized water or a Multiple investigations showed that the ion- 0.001, 0.005, 0.01, 0.05, or 0.1 N potassium chloride exchange capacity of the soil is not a constant value. solution, shaken on a rotator for 1 h, and centrifuged Rather, it depends on many factors, including the deter- [10]. mination technique; test sample preparation; the disper- sion of the soil mass; the chemical and mineralogical The pH was measured with an http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Doklady Chemistry Springer Journals

Organomineral gel and ion-exchange properties of soils

Fedotov, G.; Tret’yakov, Yu.; Pakhomov, E.
Doklady Chemistry , Volume 411 (2) – Dec 17, 2006
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References (4)

Publisher
Springer Journals
Copyright
Copyright © 2006 by Pleiades Publishing, Inc.
Subject
Chemistry; Chemistry/Food Science, general; Industrial Chemistry/Chemical Engineering
ISSN
0012-5008
eISSN
1608-3113
DOI
10.1134/S0012500806120032
Publisher site
See Article on Publisher Site

Abstract

ISSN 0012-5008, Doklady Chemistry, 2006, Vol. 411, Part 2, pp. 230–233. © Pleiades Publishing, Inc., 2006. Original Russian Text © G.N. Fedotov, Yu.D. Tret’yakov, E.I. Pakhomov, 2006, published in Doklady Akademii Nauk, 2006, Vol. 411, No. 5, pp. 633–637. CHEMISTRY a b a G. N. Fedotov , Academician Yu. D. Tret’yakov , and E. I. Pakhomov Received July 21, 2006 DOI: 10.1134/S0012500806120032 Ion-exchange capacity, one of the most important water capacity [8]. Toluene was added to inhibit the soil properties, has long attracted the attention of microbial activity [9]. Vessels with soils were tightly researchers [1]. However, the ion-exchange mechanism covered, and samples were taken every day. is not fully understood [2]. Soil extracts were prepared as follows: a 20-g soil sample was placed in 50 ml of deionized water or a Multiple investigations showed that the ion- 0.001, 0.005, 0.01, 0.05, or 0.1 N potassium chloride exchange capacity of the soil is not a constant value. solution, shaken on a rotator for 1 h, and centrifuged Rather, it depends on many factors, including the deter- [10]. mination technique; test sample preparation; the disper- sion of the soil mass; the chemical and mineralogical The pH was measured with an

Journal

Doklady Chemistry – Springer Journals

Published: Dec 17, 2006

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