Principles of Soil and Plant Water RelationsPrinciples of Soil and Plant Water Relations combines biology and physics to show how water moves through the soil-plant-atmosphere continuum. This text explores the instrumentation and the methods used to measure the status of water in soil and plants. Principles are clearly presented with the aid of diagrams, anatomical figures, and images of instrumentation. The methods on instrumentation can be used by researchers, consultants, and the military to monitor soil degradation, including measurements of soil compaction, repellency, oxygen diffusion rate, and unsaturated hydraulic conductivity. Intended for graduate students in plant and soil science programs, this book also serves as a useful reference for agronomists, plant ecologists, and agricultural engineers. * Principles are presented in an easy-to-understand style * Heavily illustrated with more than 200 figures; diagrams are professionally drawn * Anatomical figures show root, stem, leaf, and stomata * Figures of instruments show how they work * Book is carefully referenced, giving sources for all information * Struggles and accomplishments of scientists who developed the theories are given in short biographies. |
Contents
1 | |
15 | |
27 | |
Chapter 4 Tensiometers | 41 |
Chapter 5 SoilWater Terminology and Applications | 55 |
Chapter 6 Static Water in Soil | 67 |
Chapter 7 Water Movement in Saturated Soil | 85 |
Chapter 8 Field Capacity Wilting Point Available Water and the NonLimiting Water Range | 101 |
Chapter 16 Measurement of Water Potential with Thermocouple Psychrometers | 241 |
Chapter 17 Measurement of Water Potential with Pressure Chambers | 263 |
Chapter 18 Stem Anatomy and Measurement of Osmotic Potential and Turgor Potential Using PressureVolume Curves | 281 |
Chapter 19 The Ascent of Water in Plants | 315 |
Chapter 20 Electrical Analogues for Water Movement through the SoilPlantAtmosphere Continuum | 341 |
Chapter 21 Leaf Anatomy and Leaf Elasticity | 357 |
Chapter 22 Stomata and Measurement of Stomatal Resistance | 379 |
Chapter 23 Solar Radiation Black Bodies Heat Budget and Radiation Balance | 403 |
Chapter 9 Penetrometer Measurements | 117 |
Chapter 10 Measurement of Oxygen Diffusion Rate | 129 |
Chapter 11 Infiltration | 145 |
Chapter 12 Pore Volume | 173 |
Chapter 13 Time Domain Reflectometry to Measure Volumetric Soil Water Content | 187 |
Chapter 14 Root Anatomy and Poiseuilles Law for Water Flow in Roots | 207 |
Chapter 15 Gardners Equation for Water Movement to Plant Roots | 229 |
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Advanced Soil Physics Agricultural Agronomy American Society Appendix bars biography Clothier cohesion theory crop curve determine diameter diffusion disc permeameter electrical energy Equation Esau evapotranspiration field capacity flow Gardner guard cells heat hydraulic conductivity hygrometer Idso infiltration infiltrometer infrared thermometers irrigation John Wiley Kirkham Kirkham and Powers Kramer leaf water potential matric potential measure method moisture Nobel osmotic potential penetrometer permanent wilting point permission of John physicist Plant Physiology pore volume porometer pressure chamber probe psychrometer radiation relative water content Reprinted by permission Research resistance root Schaum Scholander Sci Soc Amer Section Society of Agronomy Society of America Soil Physics Soil Sci Soc Soil Science Soil Science Society soil water content solution stomata surface tension Tanner temperature tensiometer tension infiltrometer thermocouple thermocouple psychrometer tion tissue transpiration tube University vapor pressure vascular water potential Water Relations Wiley & Sons wilting point xylem York
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Page 20 - Units length meter' (m) mass* kilogram (kg) time second (s) electric current ampere (A) thermodynamic temperature* kelvin (K) amount of substance mole (mol) luminous intensity candela (cd) Supplementary Units plane angle radian (rad) solid angle steradian (sr) The spellings "metre" and "litre" are preferred by ASTM; however, "-er
Page 6 - The logarithm of any power of a number is equal to the logarithm of the number multiplied by the exponent of the power.
Page 6 - The logarithm of a quotient is equal to the logarithm of the dividend minus the logarithm of the divisor. , M , ,• , . logi — = log