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Hydrostructural Pedology [Kõva köide]

  • Formaat: Hardback, 184 pages, kõrgus x laius x paksus: 241x165x15 mm, kaal: 431 g
  • Ilmumisaeg: 17-Jun-2016
  • Kirjastus: ISTE Ltd and John Wiley & Sons Inc
  • ISBN-10: 1848219946
  • ISBN-13: 9781848219946
Teised raamatud teemal:
  • Formaat: Hardback, 184 pages, kõrgus x laius x paksus: 241x165x15 mm, kaal: 431 g
  • Ilmumisaeg: 17-Jun-2016
  • Kirjastus: ISTE Ltd and John Wiley & Sons Inc
  • ISBN-10: 1848219946
  • ISBN-13: 9781848219946
Teised raamatud teemal:
This book presents an in-depth guide to the subject matter and main points of hydrostructural pedology, as theorized for the first time. The authors focus on the underlying concepts, the purpose and role this field plays within agroenvironmental sciences.

It is divided into two parts:

Part 1 presents the theory behind hydrostructural pedology. The systemic approach applied to the soil is presented, showing how this leads to the thermodynamic formulation of water in the soil's organized medium and to the systemic modeling of soilwater-coupling in natural or anthropic organizations.

Part 2 presents the methodology to complement the first part. In it, the authors determine the hydrostructural characteristics of the pedostructure, characteristic parameters of equilibrium state equations and the hydrostructural functioning of the soil.
Preface ix
Part 1 Theory of Systemic Modeling of the Pedostructure within the Hierarchal Hydrofunctional Organization of the Natural Environment 1(94)
Chapter 1 Introduction to Part 1
5(4)
Chapter 2 Inherent Problems of Soil Science
9(8)
2.1 History of pedology
9(2)
2.2 Modeling of water transfers in the soil: supremacy of pedotransfer functions
11(1)
2.3 Absence of a unitary theory of the description of soil
12(5)
Chapter 3 The Systemic Approach Applied to Pedology
17(42)
3.1 The Bertalanffy project and Le Moigne's general system model
17(8)
3.1.1 The general system theory and Cartesian precepts
17(5)
3.1.2 Systemic representation: Le Moigne's two great ideas
22(3)
3.2 The systemic description of the soil organization
25(14)
3.2.1 Physical definition of a "system"
25(3)
3.2.2 Graduation of spatial axes: the systemic description of soil
28(4)
3.2.3 Systemic modeling of the operating system (OS) on axis III
32(3)
3.2.4 The "Structural Representative Elementary Volume" (SREV) concept required for the systemic description of the pedon
35(4)
3.3 Systemic physics of the organized soil medium defined on axis III
39(15)
3.3.1 The thermodynamic system of the pedostructure
39(2)
3.3.2 Equations of the hydrostructural equilibrium of the pedostructure
41(3)
3.3.3 Determining hydrostructural soil parameters
44(1)
3.3.4 Equations of the hydrodynamic functioning of the pedostructure
45(5)
3.3.5 The Kamel® model of the hydrostructural functioning of a pedon
50(4)
3.4 Systemic mapping of soil in the landscape
54(5)
3.4.1 Hierarchical hydrofunctional mapping units of the landscape
54(3)
3.4.2 The SIRS-Soils
57(2)
Chapter 4 The General System (GS): General Model of Scientific Disciplines Related to the Study and Management of Natural Areas
59(8)
4.1 The human system, system of study or management of a natural area, isomorphic to the general system
59(2)
4.2 Natural systems, OSs of the GS
61(1)
4.3 Information systems of human systems implemented for the study or management of natural systems
62(2)
4.4 Hydrostructural pedology and its own spatial reference information system: the SIRS-Soils
64(3)
Chapter 5 Emergence of a New Scientific Discipline: Hydrostructural Pedology
67(8)
5.1 Where hydrostructural pedology fits into the natural sciences
67(3)
5.2 Specificity of the hydrostructural pedology laboratory
70(5)
5.2.1 Hydrostructural characterization of the pedostructure
70(2)
5.2.2 Experimental analysis of the bio-soil association in the soil column
72(1)
5.2.3 Simulation of processes at the scale of the pedon using a lysimeter
72(3)
Chapter 6 Implications for Agro-environmental Sciences
75(20)
6.1 A unitary theory on the systemic and thermodynamic approaches within the natural environment
75(17)
6.1.1 Modeling in the natural environment and Cartesian precepts
75(4)
6.1.2 Systematization, theoretical basis of the systemic approach
79(2)
6.1.3 Theoretical and applied systemology
81(5)
6.1.4 General Systems theory of the agro-environmental disciplines
86(2)
6.1.5 Systemic thermodynamics
88(4)
6.2 The new challenge to agro-environmental modeling
92(3)
Part 2 Hydrostructural Characterization of Soil Pedostructure 95(62)
Chapter 7 Introduction to Part 2
99(4)
Chapter 8 Theoretical Recall
103(20)
8.1 Pinpointing the problem
103(1)
8.2 Modeling micro- and macro-water types by the shrinkage curve
104(3)
8.3 New principle for determining the micro-and macro-water types using the retention curve
107(16)
8.3.1 Micro/macro thermodynamic and hydrostructural equilibrium
107(1)
8.3.2 Equations for the retention curve
108(4)
8.3.3 Equations for the pF curve
112(2)
8.3.4 Equations for the shrinkage curve
114(3)
8.3.5 Equations for hydric conductivity
117(6)
Chapter 9 Methods for Determining the Characteristic Parameters
123(34)
9.1 Soil water retention curve "WRC"
123(12)
9.1.1 Measured using the tensiometer (suction-based method)
123(8)
9.1.2 Measured under air pressure on the porous plate press (pressure-based method), extending the WRC measurement beyond the 1,000 hPa tensiometric limit
131(4)
9.2 The shrinkage curve
135(14)
9.2.1 Case of non-sigmoidal shrinkage curves
135(9)
9.2.2 Case of the sigmoidal shrinkage curves
144(5)
9.3 The hydric conductivity curve of the pedostructure
149(8)
9.3.1 Description of the Excel sheets
149(3)
9.3.2 Procedure
152(1)
9.3.3 Results
153(4)
Conclusion 157(2)
Bibliography 159(6)
Index 165
Erik Braudeau is a Senior Scientist in Pedology and Soil Water Physics at the Institute of Research for Development in Marseille, France.

Amjad T. Assi is Assistant Research Scientist at the Texas A&M University in Texas, USA.

Rabi H. Mohtar is Professor in the Department of Biological and Agricultural Engineering at the Texas A&M University in Texas, USA.