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Chemistry of Variable Charge Soils (Topics in Sustainable Agronomy) PDF

518 Pages·1997·19.68 MB·English
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Chemistry of Variable Charge Soils Topics in Sustainable Agronomy SERIES EDITORS Rattan Lal Pedro Sanchez Malcolm Sumner M. E. Swisher P. B. Tinker Robert E. White VOLUMES T. R. Yu Chemistry of Variable Charge Soils M.E. Sumner and R. Naidu Sodic Soils: Distribution Properties, Management, and Environmental Consequences Chemistry of Variable Charge Soils Edited by T. R. YU with the assistance of G.L. Ji and other members of the staff of the Department of Soil Electrochemistry Institute of Soil Science Chinese Academy of Sciences New York Oxford Oxford University Press 1997 Oxford University Press Oxford New York Athens Auckland Bangkok Bogota Bombay Buenos Aires Calcutta Cape Town Dar es Salaam Delhi Florence Hong Kong Istanbul Karachi Kuala Lumpur Madras Madrid Melbourne Mexico City Nairobi Paris Singapore Taipei Tokyo Toronto and associated companies in Berlin Ibadan Copyright © 1997 by Oxford University Press, Inc. Published by Oxford University Press, Inc. 198 Madison Avenue, New York, New York 10016 Oxford is a registered trademark of Oxford University Press All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without prior permission of Oxford University Press. Library of Congress Cataloging-in-Publication Data Yu, T. R. Chemistry of variable charge soils / T.R. Yu. p. cm. — (Topics in sustainable agronomy) Includes bibliographical references and index. ISBN 0-19-509745-9 1. Variable charge soils. I. Title. II. Series. S592.53.Y85 1996 631.4')—dc20 95-41882 1 3 5 7 9 8 6 42 Printed in the United States of America on acid-free paper PREFACE In the vast areas of tropical and subtropical regions there is a category of widely distributed, highly weathered soils known as "Red Earths," also referred to as Ferralsols, Acrisols, Oxisols, Ultisols, Latosols, Lateritic Soils, Krasnozems, Ferrisols, and Ferrallitic Soils. Because of the abundant rainfall and high temperature, this type of soil is considered one of the most important agricultural soils in the world. However, because of some unfavorable properties inherent in these soils, the productivity is generally low. Proper utilization and melioration of these soils remain an important problem in agricultural production. Besides agriculture, soil pollution is becoming an increasingly important problem following the industrialization in these regions. Since "Red Earths" are generally low in their buffering capacity against acid precipitation and other pollutants, the problem presents a series of special features. From a scientific standpoint, just as most of the characteristics of paddy soils are related to "water," red earths' characteristic features are closely related to "red," a visible indication of the presence of the large amounts of iron oxides. These iron oxides, together with the large amounts of aluminum oxides, cause the surface charge carried by the clay to become markedly variable. This is the reason for the name variable charge soils. Because of this feature, the soils possess certain properties different from those of the constant charge soils in temperate regions. It would be helpful to have a comprehensive understanding of the chemical properties of these soils, and the results from research on these soils can enrich our present knowledge that comes primarily from research on constant charge soils. Beginning in 1962 when establishing its electrochemical research, the Department of Soil Electrochemistry in the Institute of Soil Science of the Chinese Academy of Sciences chose "Red Earths" as the principal subject of study. In particular, after the completion of the monograph Physical Chemistry of Paddy Soils (Yu, 1985; Science Press/Springer-Verlag) in 1982, the department has concentrated most of its efforts on systematic research of the chemical properties of variable charge soils. During the research it was realized that in order to thoroughly study the chemical phenomena of these soils it was necessary to develop appropriate research techniques. Therefore, focusing on the characteristics of variable charge soils, we developed a series of new electrochemical methods that were described in the monograph, Electrochemical Methods in Soil and VI Water Research (Yu and Ji, 1993; Pergamon Press). In retrospect it is clear that the application of these methods played an important role in helping us to explore new research fields and to study certain chemical phenomena not understood previously. This book summarizes the experience of our research during the past 30 years. The materials cited in the book, except for those referred to in the literature at the end of each chapter, are previously unpublished data from our research. In this book, emphasis is placed on the interactions among charged particles (clay, ions, protons and electrons) and their chemical consequences in soils. This is the essence of soil chemistry. Actually, the topics cover most areas of modern soil chemistry. It is my hope that this book may help the reader to understand the basic characteristics of variable charge soils and the fundamental difference between this kind of soil and constant charge soils. Such an understanding, when applied to research, may be helpful for further development in this field. I wish to express my sincere thanks to Prof. G. Sposito of University of California at Berkeley and Prof. M. E. Sumner of the University of Georgia for their help in facilitating the publication of this book. I am thankful to my colleagues in the Department of Soil Electrochemistry, particularly Prof. G. L. Ji, currently the head of the department, for their painstaking work in assisting me to complete the manuscript. I am also grateful to my wife, Prof. B. H. Li of Nanjing Medical University, for her help in preparing the typescript. The research was supported by the National Natural Science Foundation of China. T. R. Yu ACKNOWLEDGMENTS Permission from the following publishers to reproduce copyrighted material is gratefully acknowledged: American Chemical Society for Table 3.1, which appeared in J. Phys. Chem., 63:1831-1837 (1959). Blackwell Scientific Publications for Figs. 6.3, 6.10, 6.13, 6.15, 6.16, 13.6, 13.7, which appeared in Journal of Soil Science, 35:471 (Fig. 3), 474 (Fig. 8) (1984); 38:31 (Figs. 1, 2), 32 (Fig. 3), 33 (Figs. 4, 5) (1987). Elsevier Science Publishers for Figs. 2.17, 11.21, 13.20, 13.21, 13.22, 13.23, 13.24, 13.25, which appeared in Geoderma, 32:290 (Figs. 1, 2), 291 (Fig. 3), 292 (Fig. 4), 293 (Fig. 5), 294 (Fig. 6) (1984) ; 44:282 (Fig. 5), 283 (Fig. 6) (1989). International Society of Soil Science for Figs. 3.23, 13.13, 13.15, 13.16, 13.17, 13.18, 13.19, which appeared in Transactions of 14th International Congress of Soil Science, pp. II-64 (Fig. 1), II-65 ( Figs. 2A, 2B), II-66 (Fig. 3), II-72 (Fig. 2) (1990). Springer-Verlag for Figs. 11.23, 11.29, 13.2, 13.8, 13.10, 13.11, 13.12, 14.1, 14.4, 14.6, 14.7, 14.10, which appeared in Physical Chemistry of Paddy Soils (Yu Tian-ren, ed.) (1985), pp. 14 (Fig. 1.9), 15 (Fig. 1.10), 29 (Fig. 2.2), 31 (Fig. 2.3), 35 (Fig. 2.8), 39 (Fig. 2.14), 76 (Fig. 4.1), 78 (Fig. 4.2), 81 (Fig. 4.5), 88 (Fig. 4.8), 149 (Fig. 7.17), 152 (Fig. 7.19). VCH Verlagsgesellschaft mbH for Figs. 5.1, 5.4, 5.5, 12.1, 12.2, 12.3, 12.4, 12.5, 12.10, 12.15, which appeared in Z. fur Pflanzenemahrung und Bodenkunde, 144:518 (Fig. 1), 519 (Fig. 2) (1981); 149:602 (Fig. 4) , 603 (Fig. 5), 604 (Fig. Fig. 7) (1986); 150:19 (Figs. 1, 2) (1986). Williams & Wilkins for Figs. 8.17, 8.18, 8.24, 8.25, 8.26, 9.1, 9.2, 9.3, 9.4, 9.5, 9.6, 9.7, 9.8, 9.9, 9.10, 9.11, 9.12, 9.13, 10.1, 10.2, 10.3, 10.4, 10.5, 10.6, 10.7, 10.9, 10.10, 10.11, 10.12, 10.13, 10.14, 10.15, 10.16, 10.17, 10.18, 11.20, which appeared in Soil Science 139:169 (Fig. 7) (1985); 144:405 (Fig. 3) (1987); 147:38 (Figs. 4, 5), 92 (Figs. 1, 2, 3), 93 (Fig. 4), 175 (Fig. 1), 176 (Fig. 2) (1989); 150:832 (Fig. 2), 833 (Fig. 3) (1990); 151:438 (Figs. 1, 2), 439 (Figs. 3, 4), 440 (Figs. 5, 6, 7) (1991); 152:27 (Fig. 1), 28 (Fig. 2), 29 (Figs. 3, 4, 5), 30 (Figs. 6, 7, 8, 9), 31 (Fig. 10) (1991). This page intentionally left blank CONTENTS Chapter 1 Introduction 3 T. R. Yu 1.1 Scope of Soil Chemistry 3 1.2 Characteristics of Variable Charge Soils 6 1.3 Types of Variable Charge Soils 8 1.4 Significance of Chemistry of Variable Charge Soils 14 Bibliography 15 Chapter 2 Surface Charge 17 X. N. Zhang and A. Z. Zhao 2.1 Charged Surface 17 2.2 Contribution of Soil Components to Surface Charge 29 2.3 Influence of Environmental Factors on Surface Charge 40 2.4 Surface Charge and Soil Type 51 Bibliography 60 Chapter 3 Electrostatic Adsorption of Cations 64 G. L. Ji and H. Y. Li 3.1 Mechanism of Electrostatic Adsorption of Cations 64 3.2 Factors Affecting adsorption 70 3.3 Dissociation of Adsorbed Cations 80 3.4 Competitive Adsorption of Potassium Ions with Sodium Ions 86 3.5 Competitive Adsorption of Potassium Ions with Calcium Ions 95 3.6 Concluding Remarks 107 Bibliography 109 Chapter 4 Electrostatic Adsorption of Anions 112 G. L. Ji 4.1 Properties of Anions Relating to Electrostatic Adsorption 112 4.2 Factors Affecting Electrostatic Adsorption of Anions 115 4.3 Negative Adsorption 124 4.4 Mechanisms of Adsorption of Anions 127 Bibliography 137 Chapter 5 Specific Adsorption of Cations 140 T. R. Yu, H. Y. Sun, and H. Zhang 5.1 Principles of Specific Adsorption of Cations 140 5.2 Factors Affecting Adsorption by Soils 146 5.3 Consequences of Specific Adsorption 160 Bibliography 170 Chapter 6 Coordination Adsorption of Anions 175 G. Y. Zhang and T. R. Yu 6.1 Principles of Coordination Adsorption of Anions 176 6.2 Coordination Adsorption by Soil Components 180

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This book, based on research carried out at the Academia Sinica over the past 30 years, explains the basic difference between the variable charge soils of tropical and subtropical regions, and the constant charge soils of temperate regions. It will focus on the chemical properties of the variable ch
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