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New Trends in Soil Micromorphology - Selim Kapur
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Selim Kapur:
New Trends in Soil Micromorphology - neues Buch

2004, ISBN: 9783540791348

ID: 9783540791348

The soil water retention curve, the saturated hydraulic conductivity and the unsaturated hydraulic conductivity function are basic soil hydraulic functions and parameters. Ample apprehension of the soil hydraulic functions and parameters is required for a successful formulation of the principles leading to sustainable soil management, agricultural production and environmental protection. From these, all the other parameters, required in the solution of the practical tasks, are derived. The basic soil hydraulic functions are strongly dependent upon the soil porous system. The development of models is characteristic by the gradual transition from the simplest concepts up to the sophisticated approaches, which should correspond to the visual reality studied by soil micromorphology. 2 Soil Porous System and Soil Micromorphometry 2.1 An Overview on the Quantification of the Soil Porous System Quanti cation of the soil porous system consists of classi cation of soil pores, ch- acterization of the soil pores shapes and the estimation of the pore size distribution function. When the hydraulic functions of the soil pores are considered, the following laws of hydrostatics and hydrodynamics are applied as best tting to the classi cation criteria of the size of the pores (Kutilek and Nielsen 1994, p. 20, Kutilek 2004): A. Submicroscopic pores that are so small that they preclude clusters of water molecules from forming uid particles or continuous water ow paths. New Trends in Soil Micromorphology: The soil water retention curve, the saturated hydraulic conductivity and the unsaturated hydraulic conductivity function are basic soil hydraulic functions and parameters. Ample apprehension of the soil hydraulic functions and parameters is required for a successful formulation of the principles leading to sustainable soil management, agricultural production and environmental protection. From these, all the other parameters, required in the solution of the practical tasks, are derived. The basic soil hydraulic functions are strongly dependent upon the soil porous system. The development of models is characteristic by the gradual transition from the simplest concepts up to the sophisticated approaches, which should correspond to the visual reality studied by soil micromorphology. 2 Soil Porous System and Soil Micromorphometry 2.1 An Overview on the Quantification of the Soil Porous System Quanti cation of the soil porous system consists of classi cation of soil pores, ch- acterization of the soil pores shapes and the estimation of the pore size distribution function. When the hydraulic functions of the soil pores are considered, the following laws of hydrostatics and hydrodynamics are applied as best tting to the classi cation criteria of the size of the pores (Kutilek and Nielsen 1994, p. 20, Kutilek 2004): A. Submicroscopic pores that are so small that they preclude clusters of water molecules from forming uid particles or continuous water ow paths. Archeology Humus Rock magnetism Sediment Soil Science Soil microscopy chemistry classification ecology environment evolution fabric forest geology soil C Biogeosciences Environmental Monitoring/Analysis Soil Science & Conservation Earth, Springer Berlin

Neues Buch Rheinberg-Buch.de
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New Trends in Soil Micromorphology - Selim Kapur; Georges Stoops
Vergriffenes Buch, derzeit bei uns nicht verfügbar.
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Selim Kapur; Georges Stoops:
New Trends in Soil Micromorphology - neues Buch

ISBN: 9783540791348

ID: 9783540791348

Earth Sciences; Biogeosciences; Soil Science & Conservation; Monitoring/Environmental Analysis Archeology, Humus, Rock magnetism, Sediment, Soil Science, Soil microscopy, chemistry, classification, ecology, environment, evolution, fabric, forest, geology, soil Books eBook, Springer Science+Business Media

Neues Buch Springer.com
The book contains state-of-the-art new research results in micromorphology and other disciplines of soil science. It provides information for researchers, educators, and graduate students interested in microscopic and submicroscopic studies of soils. Versandkosten: EUR 0.00
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(*) Derzeit vergriffen bedeutet, dass dieser Titel momentan auf keiner der angeschlossenen Plattform verfügbar ist.
New Trends in Soil Micromorphology - Selim Kapur; Georges Stoops
Vergriffenes Buch, derzeit bei uns nicht verfügbar.
(*)
Selim Kapur; Georges Stoops:
New Trends in Soil Micromorphology - neues Buch

ISBN: 9783540791348

ID: 9783540791348

Earth Sciences; Biogeosciences; Soil Science & Conservation; Monitoring/Environmental Analysis Archeology, Humus, Rock magnetism, Sediment, Soil Science, Soil microscopy, chemistry, classification, ecology, environment, evolution, fabric, forest, geology, soil Books eBook, Springer Nature

Neues Buch Springer.com
The book contains state-of-the-art new research results in micromorphology and other disciplines of soil science. It provides information for researchers, educators, and graduate students interested in microscopic and submicroscopic studies of soils. Versandkosten:zzgl. Versandkosten.
Details...
(*) Derzeit vergriffen bedeutet, dass dieser Titel momentan auf keiner der angeschlossenen Plattform verfügbar ist.
New Trends in Soil Micromorphology - Selim Kapur;  Selim Kapur;  Georges Stoops;  Ahmet Mermut;  Georges Stoops
Vergriffenes Buch, derzeit bei uns nicht verfügbar.
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Selim Kapur; Selim Kapur; Georges Stoops; Ahmet Mermut; Georges Stoops:
New Trends in Soil Micromorphology - Erstausgabe

2008, ISBN: 9783540791348

ID: 21666634

[ED: 1], Auflage, eBook Download (PDF), eBooks, [PU: Springer-Verlag]

Neues Buch Lehmanns.de
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New Trends in Soil Micromorphology
Vergriffenes Buch, derzeit bei uns nicht verfügbar.
(*)
New Trends in Soil Micromorphology - neues Buch

2008, ISBN: 9783540791348

ID: 105493665

2008. Auflage 2008. Auflage eBooks > Fachthemen Wissenschaft > Natur Umwelt, [PU: Springer, Berlin/Heidelberg]

Neues Buch eBook.de
No. 11341535 Versandkosten:zzgl., Versandkosten, DE (EUR 0.00)
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