To begin, we define soil as the weathered and fragmented outer layer of the earth’s terrestrial surface. It is formed initially through disintegration, decomposition, and recomposition of mineral material contained in exposed rocks by physical, chemical, and biological processes. The material thus modified is further conditioned by the activity and accumulated residues of numerous microscopic and macroscopic organisms (plants and animals). In a series of processes that may require hundreds or even thousands of years and that is called soil genesis, the loose debris of rock fragments is transmuted into a more or less stable, internally ordered, actively functioning natural body. Ultimately, this culminates in the formation of a characteristic soil profile, which resembles a layer cake. We can visualize the soil profile as a composite living body, in the same way that we think of the human body as a distinct organism, even though in reality it is an ensemble of numerous interdependent and symbiotically coordinated groups of organelles, cells, organs, and colonies of myriad organisms. <...>

Soils are a valuable resource and a critical component in many of the environmental and economic issues facing society today. Understanding soil properties and soil behaviour and interpreting soil data are especially relevant for many environmental and land management issues facing the community. These issues include urban development, control of salinity, clearing of native vegetation, prevention of land degradation, control of water and wind erosion, irrigation development, the management of effluent disposal, contamination and the management of acid sulfate soils.

This special issue of Geoderma is the result of the work of members of the “International Working-Group on Submicroscopy of Undisturbed Soil Materials (IWGSUSM)”. The papers are from the second workshop of IWGSUSM, organized in 1981 by J. Ducloux at the University of Poitiers, France; the symposium on “Submicroscopy of Undisturbed Soil Materials” organized in 1981 by M.L. Thompson in Atlanta, Georgia, U.S.A. during the annual meeting of the Soil Science Society of America, and work done in 1982. The papers mainly concern in situ electron microscopic studies of materials in thin sections of soils and of unimpregnated soil constituents in peds. Ion microscopy is discussed in one paper.

Handbook of Soil Sciences is the second edition of a comprehensive reference work on the discipline of soil science as practiced today. The new edition has been completely revised and rewritten to reflect the current state of knowledge. It contains definitive descriptions of each major area in the discipline, including its fundamental principles, appropriate methods to measure each property, many examples of the variations in properties in different soils throughout the world, and guidelines for the interpretation of the data for various applications (agricultural, engineering, and environmental).

This book is the third in a series of three, intended primarily to provide a working manual for laboratory technicians and others engaged in the testing of soils for building and engineering purposes. It is not meant in any way to be used as a substitute for the Standards referred to therein, but to augment their requirements by the provision of step by step procedures. This third edition has been revised to take account of the current requirements of BS 1377: 1990,

Information on soil and land resources is a prerequisite for informed decisions on land use and management. Procedures for acquiring and using this information are introduced and  emphasis is given to a balanced approach with elements of mapping, modelling and monitoring within the broader context of environmental change. The conceptual basis for a range of approaches to survey is introduced along with an assessment of strengths and weaknesses. A framework for dealing with scale in measurement and prediction is then introduced.

Laboratory data are critical to the understanding of the properties and genesis of a single pedon, as well as to the understanding of fundamental soil relationships based on many observations of a large number of soils. The development of laboratory methods, the analytical database, and the soil relationships based on those data are the cumulative effort of several generations of scientists.

The word “clays” was assigned early to fine grained material in geological formations (Agricola 1546) or soils (de Serres 1600). Clays have been identified as mineral species in the begining of the 19th century in the production of ceramic materials (Brongniart 1844). Then Ebelmen (1847) carefully analyzed the decomposition of rocks under chemical attack and the way that porcelain can be commonly made. Since this pionner works, the definition of clays has varied.

В учебном пособии в интерактивной форме представлены современные представления о теории и методах геостатистики и их применении в почвоведении и экологии для решения актуальных экологических и агроэкологических проблем. Основное внимание уделено вопросам построения семивариограмм и расчета их основных характеристики подбору моделей. Рассматривается понятие кригинга и дается описание некоторых его разновидностей.

This entry explains the use of emergy analysis to evaluate systems and compare resource use, environmental loading, and sustainability. This method allows the free contributions of the environment to be compared directly with the purchased inputs from the economy. Results summarized from agriculture and forestry systems indicate that extensive amounts of indirect energy were dissipated to yield agricultural and forest products and that timber typically requires less indirect energy than crops.