An introduction to soil mineralogy; Surface chemistry of soil minerals; An introduction to organic matter in mineral soils; Mineral equilibria and the soil system; Mineral occurrence in soil environments; Carboonate, halide, sulfate, and sulfide minerals; Aluminum oxides and oxyhydroxides; Iron oxides; Manganese oxides ands hydroxides; Kaolin and serpentine group minerals; The pyrophyllite-talc group; Micas; Vermiculites; Chlorites and hydroxy-interlayered vermiculite and smectite; Interstratification in layer silicates; Palygorskite and sepiolite group minerals; Zeolites in soils; Silica in soils: quartz and disordered silica polymorphs; Feldpars, olivines, pyroxenes, and amphiboles; Allophane and imogolite; Phosphate minerals; Titanium and zirconium minerals.

An introduction to soil mineralogy. Surface chemistry of soil minerals. An introduction to organic matter in mineral soils. Mineral equilibria and the soil system. Mineral occurrence in soil environments. Carbonate, halide, sulfate, and sulfide minerals. Aluminum oxides and oxyhydroxides. Iron oxides. Manganese oxides and hydroxides. Kaolin and serpentine group minerals. The pyrophyllite-talc group. Micas. Vermiculites. Smectites. Chlorites and hydroxy-interlayered vermiculite and smectite. Interstratification in layer silicates. Palygorskite and sepiolite group minerals. Zoolites in soils. Silica in soils: quartz and disordered silica polymorphs. Feldspars, olivines, pyroxenes, and amphiboles. Allophane and imogolite. Phosphate minerals. Titanium and zirconium minerals.

An introduction to soil mineralogy. Surface chemistry of soil minerals. An introduction to organic matter in mineral soils. Mineral equilibria and the soil system. Mineral occurrence in soil environments. Carbonate, halide, sulfate, and sulfide minerals. Aluminum oxides and oxyhydroxides. Iron oxides. Manganese oxides and hydroxides. Kaolin and serpentine group minerals. The pyrophyllite-talc group. Micas. Vermiculites. Smectites. Chlorites and hydroxy-interlayered vermiculite and smectite. Interstratification in layer silicates. Palygorskite and sepiolite group minerals. Zoolites in soils. Silica in soils: quartz and disordered silica polymorphs. Feldspars, olivines, pyroxenes, and amphiboles. Allophane and imogolite. Phosphate minerals. Titanium and zirconium minerals.

Few books achieve a connection between scientifc theory and real world environmental problems, but this one does. Generous use of color images, exercises, and case studies make it friendly for the classroom or non-mineralogist. Discover crystallography, surface chemistry, mineral-solution equilibria, organic matter, and soil mineral analysis. The book includes a lengthy exploration of world-wide applications of mineralogy in soil taxonomy, tectonics, radionuclides, pesticides, enzymes, and more.

Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles.

The latest installment in the well-received Methods of Soil Analysis series, Methods of Soil Analysis. Part 5. Mineralogical Methods, presents valuable techniques that will enable researchers to analyze mineralogy for a wide variety of applications. An understanding of mineralogical composition provides crucial insight into the fundamental behavior of soils and their response to environmental conditions and management. Highlights include extensive coverage of new techniques, such as X-ray absorption and diffuse reflectance spectroscopy, and updated chapters on thermal analysis and selective dissolution methodologies. Each chapter provides the basic principles of the method, guides the reader through the method itself, and finally assists in the interpretation and analysis of results collected.

Probably more than any other element, iron markedly influences the chemical and physical properties of soils and sediments in the earth. Considering its transition metal status, with potential variation in electronic configuration, ionic radius, and magnetic moment, combined with its abundance and relatively large mass, little wonder that one sees its unique influence on every hand. Pre sentations at the NATO Advanced Study Institute (NATO AS!) on Iron in Soils and Clay Minerals reviewed and discussed the occurrence, behavior, and properties of Fe-bearing minerals found in soils and in the clay mineral groups kaolinite, smectite, and mica. Also discussed at the NATO AS! were the basic chemical properties of Fe, methods for separating and identifying Fe in minerals, and the role of Fe minerals in weathering and other soil-forming processes. The present publication is the reviewed and edited proceedings of that Advanced Study Institute. The sequence of chapters follows the general pattern beginning with introductory chapters which overview the general occurrence of Fe in the earth and its chemistry, both generally and in mineral environments, followed by identification and characterization methods for Fe and Fe phases in minerals. The properties and behavior of Fe oxides, Fe-bearing clay minerals, and other Fe minerals in soils are then described, and the text ends with a summary of the role of Fe in soil-forming processes. A Table of Contents and subject index are provided to assist the reader in finding specific topics within the text.