Environmental Soil Physics: Fundamentals, Applications, and Environmental ConsiderationsElsevier, 1998 M09 9 - 771 páginas Environmental Soil Physics is a completely updated and modified edition of the Daniel Hillels previous, successful books, Introduction to Soil Physics and Fundamentals of Soil Physics. Hillel is a Pulitzer Prize-winning author, one of the true leaders in the field of environmental sciences. The new version includes a chapter and problems on computational techniques, addresses current environmental concerns and trends. - Updates and expands the scope of Hillel's prior works, Fundamentals of Soil Physics (1980)and Applications of Soil Physics (1980) - Explores the wide range of interactions among the phases in the soil and the dynamic interconnections of the soil with the subterranean and atmospheric domains - Draws attention to historical and contemporary issues concerning the human management of soil and water resources - Directs readers toward solution of practical problems in terrestrial ecology, field-scale hydrology, agronomy, and civil engineering - Incorporates contributions by leading scientists in the areas of spatial variability, soil remediation, and the inclusion of land-surface processes in global climate models |
Contenido
| 57 | |
THE LIQUID PHASE | 127 |
THE GASEOUS PHASE | 275 |
COMPOSITE PHENOMENA | 307 |
THE FIELD WATER CYCLE | 383 |
SOILPLANTWATER RELATIONS | 545 |
APPENDICES | 653 |
| 707 | |
| 757 | |
Otras ediciones - Ver todas
Environmental Soil Physics: Fundamentals, Applications, and Environmental ... Daniel Hillel Sin vista previa disponible - 1998 |
Términos y frases comunes
adsorbed adsorption aggregates aquifer atmosphere bulk density calculate capillary cations clay concentration constant crop curves Darcy's law decrease depends depth diffusion distribution drainage drains effect energy equation equilibrium erosion evaporation rate evapotranspiration field field capacity flow fluid flux fraction function gradient gravity groundwater heat hence Hillel hydraulic conductivity hydraulic head hysteresis increase infiltration rate initial ions irrigation kaolinite kg/m³ layer liquid mass matric suction measured minerals mm/day molecules montmorillonite organic matter osmotic oxygen particles permeability phase piezometers plant pores porosity porous properties radiation rainfall resistance root zone runoff salinity salt sample sand saturated shear soil moisture soil physics soil profile Soil Sci soil surface soil water soil wetness soil-water soil's stress structure temperature tend tensiometer thermal tion transpiration tube unit unsaturated values variable velocity vertical volumetric volumetric heat capacity water content water table wetting front
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Página 59 - All these things being considered, it seems probable to me that God in the beginning formed matter in solid, massy, hard, impenetrable, movable particles, of such sizes and figures, and with such other properties and in such proportion to space as most conduced to the end for which he formed them...
