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Titlebook: Arid Zone Irrigation; Bruno Yaron,Erik Danfors,Yoash Vaadia Book 1973 Springer-Verlag Berlin · Heidelberg 1973 agriculture.ecosystem.irrig

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期刊全称Arid Zone Irrigation
影响因子2023Bruno Yaron,Erik Danfors,Yoash Vaadia
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学科分类Ecological Studies
图书封面Titlebook: Arid Zone Irrigation;  Bruno Yaron,Erik Danfors,Yoash Vaadia Book 1973 Springer-Verlag Berlin · Heidelberg 1973 agriculture.ecosystem.irrig
影响因子A book previously published within the framework of the Ecological Studies Series, entitled "Physical Aspects of Soil Water and Salts in Ecosystems" included awidespectrum of research papers devoted to new findings in the field of soil-plant-water relationships. "Arid Zone Irrigation" has been written specifically as a textbook for agronomists, soil scientists, agrometeorologists, water engineers and plant physiologists who want a clear presentation of irrigation fundamentals in arid and semi-arid zones. It was our intention to provide an understanding of the basic principles governing irrigation technology and to help overcome the problem of water shortage in arid zone agriculture. This book, written by a large number of specialists and covering a broad spectrum of different disciplines, is based on general up-to-date information, as well as on the results of the authors‘ own research. The idea of preparing such a textbook was conceived during a series of international advanced courses on irrigation held annually at the Institute of Soils and Water, Agricul­ tural Research Organization, Volcani Center, Bet Dagan, Israel. The final organization of the material has been influenced b
Pindex Book 1973
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https://doi.org/10.1007/978-3-540-33795-9o the total atmospheric losses of water from soil and plant surfaces. However, as used in this chapter the word evaporation will mean all water losses in vapor form, regardless of the nature of the surface.
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Interferenz, Beugung und Streuung,und surface, leaving only about 4.4 × 10. m. that could be used each year for the benefit of mankind. The available amount is divided between surface water (rivers, streams, freshwater lakes), groundwater (to a depth of 800 m below the ground surface), and atmospheric water (atmospheric moisture, clouds, etc.) as follows:
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Elektromagnetische Wellen in Materie,ories, the soil is considered to be a continuous porous medium, and the governing equations are derived for a representative elementary volume that is large enough so that its properties can be expressed in terms of statistical averages.
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Hydrologic Fundamentalsund surface, leaving only about 4.4 × 10. m. that could be used each year for the benefit of mankind. The available amount is divided between surface water (rivers, streams, freshwater lakes), groundwater (to a depth of 800 m below the ground surface), and atmospheric water (atmospheric moisture, clouds, etc.) as follows:
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