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Overview
This book is a unified, condensed, and simplified version of the recently issued twin volumes, Fundamentals of Soil Physics and Applications of Soil Physics. Nonessential topics and complexities have been deleted, and little prior knowledge of the subject is assumed. An effort has been made to provide an elementary, readable, and self-sustaining description of the soil's physical properties and of the manner in which these properties govern the processes taking place in the field. Consideration is given to the ways in which the soil's processes can be influenced, for better or for worse, by man. Sample problems are provided in an attempt to illustrate how the abstract principles embodied in mathematical equations can be applied in practice. The author hope that the present version will be more accessible to students than its precursors and that it might serve to arouse their interest in the vital science of soil physics.Audience: Undergraduate students in the agronomic, horticultural, silvicultural, environmental, and engineering sciences.
Synopsis
This book demonstrates applications of the basic principles of soil physics and illustrates how they can be used systematically to define—and eventually control—existing phenomena.
The first section of the book provides comprehensive treatment of the field water cycle and its management. Topics covered are: the sequential processes if infiltration and runoff; redistribution and storage of soil moisture; groundwater drainage; evaporation from bare soil and soil salinization; uptake of water by plants and transpiration as determined by climate, soil properties, and rooting habit; field water balance and energy balance; crop water requirements and water use efficiency; tillage mechanics and soild structure management.
The second section extends these principles further and introduces the reader to the contributions of several leading authorities on topics of vital contemporary interest. The topics discussed include; crop canopy effects on evapotranspiration; freezing phenomena in soils; similitude and scaling; spatial heterogeneity of soil physical properties; and the movement of solutes during infiltration.