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ویرایش: سری: ISBN (شابک) : 9783031206672 ناشر: Springer International Publishing سال نشر: 2023 تعداد صفحات: 572 زبان: English فرمت فایل : PDF (درصورت درخواست کاربر به PDF، EPUB یا AZW3 تبدیل می شود) حجم فایل: 26 مگابایت
در صورت تبدیل فایل کتاب Geopedology: An Integration of Geomorphology and Pedology for Soil and Landscape Studies به فرمت های PDF، EPUB، AZW3، MOBI و یا DJVU می توانید به پشتیبان اطلاع دهید تا فایل مورد نظر را تبدیل نمایند.
توجه داشته باشید کتاب ژئوپدولوژی: تلفیقی از ژئومورفولوژی و پدولوژی برای مطالعات خاک و منظر نسخه زبان اصلی می باشد و کتاب ترجمه شده به فارسی نمی باشد. وبسایت اینترنشنال لایبرری ارائه دهنده کتاب های زبان اصلی می باشد و هیچ گونه کتاب ترجمه شده یا نوشته شده به فارسی را ارائه نمی دهد.
In Memoriam Foreword Bringing Geopedology to a New Generation References Contents Part I: Foundations of Geopedology Chapter 1: Introduction References Chapter 2: Theoretical Framework References Chapter 3: Relationships Between Geomorphology and Pedology: Brief Review 3.1 Introduction 3.2 Definitions and Approaches 3.2.1 Academic Stream 3.2.2 Applied Stream 3.3 Nature of the Relationships and Fields of Convergence 3.3.1 Evolution of the Relationships 3.3.2 Mutual Contributions 3.3.3 Trend Towards Greater Integration 3.4 Conclusion References Chapter 4: The Geopedologic Approach 4.1 Introduction: Definition, Origin, Development 4.2 Conceptual Relationships 4.2.1 Common Forming Factors 4.2.2 The Geopedologic Landscape 4.2.2.1 Flat Areas 4.2.2.2 Sloping Areas 4.3 Methodological Relationships 4.3.1 Geopedologic Integration: A Structural Model 4.3.2 Geopedologic Integration: Soil Geography, Genesis, and Stratigraphy 4.3.2.1 Soil Geography 4.3.2.2 Soil Genesis and Stratigraphy 4.3.3 Geopedologic Integration: A Test of Numerical Validation 4.3.3.1 Materials and Method 4.3.3.2 Results 4.3.3.3 Conclusion 4.4 Operational Relationships 4.4.1 Introduction 4.4.2 The Structure of the Soil Survey 4.4.3 The Functioning of the Soil Survey 4.4.4 The Contribution of Geomorphology to Soil Survey 4.5 Conclusions References Chapter 5: The Pedologic Landscape: Organization of the Soil Material 5.1 Introduction 5.2 Nano-level 5.2.1 Chemical Reactions 5.2.2 Mechanical Reactions 5.2.2.1 Types of Packing 5.2.2.2 Types of Fabric 5.2.3 Physico-Chemical Reactions 5.2.4 Relationship with Geopedology 5.3 Micro-level 5.3.1 The Micromorphologic Components 5.3.1.1 Skeleton Grains 5.3.1.2 Plasma 5.3.1.3 Pores 5.3.1.4 Pedologic Features 5.3.2 Relationship with Geopedology 5.4 Meso-level 5.4.1 Horizon Definition and Designation 5.4.1.1 Primary Divisions: The Master Horizons 5.4.1.2 Secondary Divisions: Specific Genetic Features 5.4.1.3 Tertiary Divisions 5.4.2 Relationship with Geopedology 5.5 Macro-level 5.5.1 Definition 5.5.2 Related Concepts 5.5.3 Relationship with Geopedology 5.6 Mega-level 5.6.1 Definition 5.6.2 Relationship with Geopedology 5.7 Conclusion References Chapter 6: The Geomorphic Landscape: Criteria for Classifying Geoforms 6.1 Introduction 6.2 Examples of Geomorphic Classification 6.2.1 Classification by Order of Magnitude 6.2.2 Genetic and Genetic-Chorologic Classifications 6.2.3 Morphometric Classification 6.2.4 Ethnogeomorphic Classification 6.3 Bases for a Taxonomic Classification System of the Geoforms 6.3.1 Premises and Basic Statements 6.3.2 Prior Information Sources 6.3.3 Searching for Structure: An Inductive Example 6.4 Structure and Elements for Building a Taxonomic System of the Geoforms 6.4.1 Structure 6.4.2 Elements 6.4.2.1 Category 6.4.2.2 Class 6.4.2.3 Taxon 6.4.2.4 Attribute 6.5 Levels of Perception: Exploring the Structure of a Geomorphic Space 6.6 Structure of a Taxonomic System of the Geoforms 6.7 Conclusion References Chapter 7: The Geomorphic Landscape: Classification of Geoforms 7.1 Introduction 7.2 The Taxonomy: Categories and Main Classes of Geotaxa 7.2.1 Geostructure 7.2.2 Morphogenic Environment 7.2.3 Geomorphic Landscape 7.2.3.1 Definition 7.2.3.2 Taxa 7.2.4 Relief/Molding 7.2.4.1 Definition 7.2.4.2 Taxa 7.2.5 Lithology/Facies 7.2.5.1 Definition 7.2.5.2 Taxa 7.2.6 Terrain Form/Landform 7.2.6.1 Definition 7.2.6.2 Taxa 7.3 Classification of the Geoforms at the Lower Levels 7.3.1 Introduction 7.3.2 Geoforms Mainly Controlled by the Geologic Structure 7.3.2.1 Structural Geoforms Proper 7.3.2.2 Volcanic Geoforms 7.3.2.3 Karstic Geoforms 7.3.3 Geoforms Mainly Controlled by the Morphogenic Agents 7.3.3.1 Nival, Glacial, and Periglacial Geoforms 7.3.3.2 Eolian Geoforms 7.3.3.3 Alluvial and Colluvial Geoforms 7.3.3.4 Lacustrine Geoforms 7.3.3.5 Gravity and Mass Movement Geoforms 7.3.3.6 Coastal Geoforms 7.3.4 Banal Hillside Geoforms 7.3.4.1 Main Characteristics 7.3.4.2 Classes of Banal Hillside Geoforms 7.4 Conclusion References Chapter 8: The Geomorphic Landscape: The Attributes of Geoforms 8.1 Introduction 8.2 Morphographic Attributes: The Geometry of Geoforms 8.2.1 Topography 8.2.2 Planimetry 8.2.2.1 Configuration of the Geoforms 8.2.2.2 Contour Design of the Geoforms 8.2.2.3 Drainage Pattern 8.2.2.4 Neighboring Units and Surrounding Conditions 8.2.3 Morphography and Landscape Ecology 8.3 Morphometric Attributes: The Dimension of Geoforms 8.3.1 Relative Elevation (Relief Amplitude, Internal Relief) 8.3.2 Drainage Density 8.3.3 Relief Slope 8.3.4 Terrain and Soil Surface Features 8.3.5 Contribution of Digital Morphometry 8.4 Morphogenic Attributes: The Dynamics of Geoforms 8.4.1 Particle Size Distribution 8.4.1.1 Relevance 8.4.1.2 The Information 8.4.1.3 Examples of Inference and Interpretation 8.4.2 Structure 8.4.2.1 Geogenic Structure 8.4.2.2 Pedogenic Structure 8.4.3 Consistence 8.4.4 Mineralogy 8.4.5 Morphoscopy 8.5 Morphochronologic Attributes: The History of Geoforms 8.5.1 Reference Scheme for the Geochronology of the Quaternary 8.5.2 Dating Techniques 8.5.3 Relative Geochronology: The Contribution of Pedostratigraphy 8.5.3.1 Definition 8.5.3.2 Indicators 8.5.3.3 Combining Indicators 8.6 Relative Importance of the Geomorphic Attributes 8.6.1 Attribute Classes 8.6.1.1 Differentiating Attributes 8.6.1.2 Accessory Attributes 8.6.1.3 Accidental Attributes 8.6.2 Attribute Weight 8.6.2.1 Morphographic Attributes 8.6.2.2 Morphometric Attributes 8.6.2.3 Morphogenic Attributes 8.6.2.4 Morphochronologic Attributes 8.6.3 Attribute Hierarchization 8.6.3.1 Upper Levels 8.6.3.2 Lower Levels 8.7 General Conclusion on Geopsedology References Part II: Approaches to Soil-Landscape Pattern Analysis Chapter 9: Knowledge Is Power: Where Digital Soil Mapping Needs Geopedology 9.1 Introduction 9.2 Example 1: Exhumed Paleosols 9.3 Example 2: Depositional Low-Relief Environments 9.4 Example 3: Inverted Landscapes 9.5 Example 4: Young Post-Glacial Landscapes 9.6 Discussion 9.6.1 What Could Be the Contribution of the Geopedologic Approach to DSM? 9.7 Conclusion References Chapter 10: Geodiversity and Geopedology in a Logarithmic Universe 10.1 Introduction 10.2 The Concept of Diversity 10.3 Biodiversity, Pedodiversity, Landform Diversity, and Lithological Diversity Patterns 10.4 Geopedologic and Bioclimatic Approaches 10.5 Geographical Analysis, Taxonomies, Maps and Soil Surveys: Fractal Structures 10.5.1 Paretian Thinking in a Logarithmic World 10.5.2 Paretian Thinking, Natural Resources Inventories, and Mapping 10.5.3 Human Cognition, Logarithmic Thinking and Miller’s Law 10.6 Pedodiversity, Geodiversity and the Preservation of Geoforms as Part of Natural Heritage 10.7 Conclusions References Chapter 11: Algorithms for Quantitative Pedology 11.1 Introduction 11.1.1 Example Data: Clarksville Soil Series (Fig. 11.1) 11.2 Representing Collections of Soil Profiles in R 11.2.1 Subsetting 11.2.2 Data Quality and Repairs 11.3 Soil Morphology 11.3.1 Soil Color 11.3.1.1 Color Conversion 11.3.1.2 Color Contrast 11.3.2 Soil Profile Sketches 11.3.3 Functional Horizon Aggregation 11.3.4 Change of Depth Support 11.4 Numerical Classification of Soils 11.5 Water Balance 11.6 Conclusions References Chapter 12: Interaction of Geological and Pedological Processes in the Genesis of Soils with Gypsum, Northern Patagonia, Argentina 12.1 Introduction 12.2 Distribution of Gypsum Soils and Its Relationship with the Calcium Sulfate Source 12.2.1 Gypsum Soils of Geological Origin 12.2.2 Gypsum Soils of Pedogenic Origin 12.3 Processes Affecting the Soil. Soil Uses 12.4 Conclusions References Chapter 13: Use of Soil Maps to Interpret Soil-Landform Assemblages and Soil-Landscape Evolution 13.1 Introduction 13.2 Methodological Approach 13.3 Example 1: A Detailed Surficial Geology Map of Iowa, USA 13.4 Example 2: The Loess-Covered Landscapes of Western Wisconsin, USA 13.5 Example 3: The Recently Deglaciated Landscape of Northeastern Lower Michigan, USA 13.6 Example 4: An Enigmatic Soil Parent Material on the Outwash Plains of Southwestern Michigan, USA 13.7 Example 5: A Watershed with a Complex Geology in the Western Grand-Duchy of Luxembourg 13.8 Example 6: Improving the Precision of Delineations for Large Extent Maps in the Glaciated Central Lowlands, USA 13.9 Summary and Conclusions References Part III: Methods and Techniques Applied to Pattern Recognition and Mapping Chapter 14: Digital Soil Texture Maps of Argentina and Their Relationship to Soil-Forming Factors and Processes 14.1 Introduction 14.2 Materials and Methods 14.2.1 Study Area 14.2.2 Soil Profile Data 14.2.3 Environmental Covariates 14.2.4 Processing 14.2.5 Modelling and Accuracy Assessment 14.2.6 Generation of Textural Class Maps 14.3 Results and Discussion 14.3.1 Predicted Maps and Accuracy Assessment 14.3.2 Maps of Textural Classes 14.4 Conclusions References Chapter 15: Synergistic Use of Radar and Optical Image Data for Improved Land Use and Land Cover Assessment: A Case Study in the North of Entre Rios Province (Argentina) 15.1 Introduction 15.2 Materials and Methods 15.2.1 Subset Selection 15.2.2 Land Use and Land Cover Classes 15.2.3 Synthetic Aperture Radar Data 15.2.4 Optical Data 15.2.5 Methodology 15.2.5.1 SAR Data Processing 15.2.5.2 Statistical Analysis 15.2.5.3 Change Detection: Log-Ratio Scaling 15.2.5.4 Radar Vegetation Index 15.2.5.5 S2 Derived Indices 15.2.5.6 Radar and Optical Integration 15.2.5.7 Feature Extraction and Classification 15.3 Results and Discussion 15.3.1 Backscattering Behavior 15.3.2 SAR Log-Ratio Operator 15.3.3 Radar Vegetation Index 15.3.4 Soil and Vegetation Radiometric Indices 15.3.5 Integration of S1 and S2 Bands 15.4 Concluding Remark References Chapter 16: Landslide Susceptibility Mapping Using Supervised Learning Methods – Case Study: Southwestern Colombia 16.1 Introduction 16.2 Materials and Method 16.2.1 Study Area 16.2.2 Data Collection 16.2.3 Method 16.3 Results and Discussion 16.3.1 SRTM DEM Accuracy Assessment 16.3.2 Landslide Inventory 16.3.3 Landslide Conditioning Factors 16.3.4 LR Model for Landslide Probability Occurrence 16.3.4.1 Training Model 16.3.4.2 Performance of the LR Model 16.3.5 Landslide Susceptibility Zoning Based on RF Analysis 16.3.5.1 Training Model 16.3.5.2 Mean Decrease Accuracy (MDA) 16.3.5.3 Accuracy of the Landslide Classification by the RF Method 16.4 Conclusions References Chapter 17: Polygenic Vertisols and “Hidden” Vertisols of the Paraná River Basin, Argentina 17.1 Introduction 17.2 Polygenic Vertisols of the Mesopotamian Pampa 17.2.1 Setting the Subject 17.2.2 The Study Cases 17.2.2.1 The Soils and Their Environment 17.2.2.2 Clay Mineralogy 17.2.2.3 Mineralogy of the Sand and Silt Fractions 17.2.2.4 Micromorphology 17.2.2.5 Discussion and Conclusions 17.3 “Hidden” Vertisols of the Undulating Pampa 17.3.1 Setting the Subject 17.3.2 The Study Cases 17.3.2.1 Morphology of a Soil Profile in the INTA Fields 17.3.2.2 Chemical and Physical Parameters 17.3.2.3 Magnetic Susceptibility 17.3.2.4 Clay Mineralogy 17.3.2.5 Application of the Pedogenetic Model to the Classification and Mapping of Vertic Argiudolls 17.3.2.6 Discussion and Conclusions 17.4 General Conclusions and Prospect References Chapter 18: Mapping Gilgai Micro-relief and Its Impact on Dryland Agricultural Landscapes Using Time Series of NDVI Derived from Sentinel-2 Imagery 18.1 Introduction 18.2 Materials and Methods 18.2.1 Study Area. The COALA Project 18.2.2 Sentinel 2 Images and Its Processing Chain 18.2.3 Methodology for Mapping Management Zones Map, MZM, in Australian Paddocks on the Study Area 18.2.4 Gilgai Soil Structure 18.3 Results 18.3.1 Management Zones Map 18.3.1.1 How MZM Picks Up the Crop Growth Through Sentinel2 Time Series 18.3.2 Detection of Granular Structure in Paddocks by Using RGB from Sentinel2 18.3.3 Detection of Granular Structure by Using Other Imagery: Landsat, Google Earth 18.4 Discussion and Conclusions References Part IV: Applications in Land Degradation and Geohazard Studies Chapter 19: Gully Erosion Analysis. Why Geopedology Matters? 19.1 Introduction 19.2 Research on Gully Erosion: Detection, Monitoring, and Modeling 19.2.1 Gully Erosion Processes and Modeling 19.2.2 Remote Sensing, GIS and Gully Mapping 19.3 Using Geopedology in Gully Erosion Research 19.3.1 Why Is It Important? 19.3.2 Why Geopedology Matters? 19.4 Conclusions References Chapter 20: Soil Erosion Assessment and Mitigation Scenarios Based on Geopedology in Northwestern Patagonia, Argentina 20.1 Introduction 20.2 Materials and Method 20.2.1 Study Area 20.2.2 Survey Approach 20.2.3 Soil Erosion Mapping 20.3 Results and Discussion 20.3.1 Soil Types 20.3.2 Current Erosion and Active Processes 20.3.3 Soil Erosion Hazard 20.3.4 Soil Erosion Hazard with a Simulated Silvopastoral System 20.4 Final Considerations References Chapter 21: Adequacy of Soil Information Resulting from Geopedology-Based Predictive Soil Mapping for Assessing Land Degradation: Case Studies in Thailand and Iran 21.1 Introduction 21.2 Materials and Methods 21.3 Soilscape Mapping for Assessing Soil Erosion in Thailand 21.3.1 Study Area 21.3.2 Soil Studies 21.3.3 Results 21.4 Soilscape Mapping for Flood Hazard Assessment in Central Thailand 21.4.1 Study Area 21.4.2 Soil Studies in Sample Areas and Transects 21.4.3 Results 21.5 Soilscape Mapping for Soil Salinity Trend Assessment 21.5.1 Salinity Hazard Assessment in North-Eastern Thailand 21.5.1.1 Soil Sampling and Data Analysis 21.5.1.2 Results 21.5.2 Soil Salinity Risk Assessment in Iran 21.5.2.1 Study Area 21.5.2.2 Soilscape and Hydropedology 21.5.2.3 Results 21.6 Discussion 21.7 Conclusion References Chapter 22: Exploring the Contribution of Geopedology to the Implementation of National Frameworks for Land Degradation Neutrality 22.1 Land Degradation Neutrality and Geopedology: Foundations 22.2 Entry Points of Geopedology in Planning for LDN 22.3 Worked Example Using the Cochabamba Valleys (Bolivia) 22.4 Final Remarks References Part V: Applications in Land Use Planning and Policy Chapter 23: Geo-Pedological Approach for Land Use Planning-Case Studies from India 23.1 Introduction 23.2 Materials and Methods 23.2.1 Details of Study Area 23.2.1.1 Case Study 1: Meghalaya Plateau 23.2.1.2 Case Study 2: Yavatmal District, Maharashtra State, India 23.2.1.3 Case Study 3: Pulivendala 23.2.2 Geo-Pedological Survey 23.2.3 Land Evaluation 23.3 Results and Discussion 23.3.1 Case Study-1: Meghalaya Plateau 23.3.1.1 Landforms and Soils 23.3.1.2 Soil Site Suitability for Potato 23.3.2 Case Study-2-Yavatmal District 23.3.2.1 Soil mapping Units in Relation Landforms 23.3.2.2 Soil Site Suitability Analysis 23.3.3 Case Study-1: Pulivendula 23.3.3.1 Landforms and Soils 23.3.3.2 Soil Site Suitability Analysis 23.4 Conclusions and Recommendations References Chapter 24: Geopedologic Information, Foundation for Soil Conservation: Land Evaluation, Land Use Allocation and Associated Conservation Practices 24.1 Introduction 24.2 Methodology 24.3 Study Area Location and Characteristics 24.4 Study Case 1 24.5 Study Case 2 24.6 New Trends in Precision Sustainable Land Management 24.7 General Conclusion References Chapter 25: The Relevance of Geopedology for Policy Making and Soil Security 25.1 Introduction 25.2 Geopedology and Soil Security 25.3 Capability 25.4 Condition 25.5 Capital 25.6 Connectivity 25.7 Codification 25.8 Conclusions References Chapter 26: Significance of Land Cover Change for Soil Regulating Ecosystem Services Using Maine’s Climate Action Plan as a Case Study 26.1 Introduction 26.2 Materials and Methods 26.2.1 The Ecosystem Services Accounting Framework 26.3 Results 26.3.1 Value of SOC by Soil Order and County for Maine 26.3.2 Value of SIC by Soil Order and County for Maine 26.3.3 Value of TSC (SOC + SIC) by Soil Order and County for Maine 26.3.4 Land Use/Land Cover Change by Soil Order in Maine from 2001 to 2016 26.4 Discussion 26.4.1 The Role of Pedodiversity (Soil Diversity) in Carbon Regulating ES/ED in Maine 26.4.2 The Role of Land Cover Change in Soil Carbon Regulating ES/ED in Maine 26.4.3 The Role of Land Cover and Pedodiversity (Soil Diversity) Concepts in Sustainable Management of Soil C Regulating ES/ED 26.4.4 Significance of Results for Maine’s Climate Action Plan 26.5 Summary and Conclusions References Chapter 27: Upscaling the Integrated Terroir Zoning Through Digital Soil Mapping Disaggregation: A Case Study in the Designation of Origin Campo de Borja 27.1 Introduction 27.2 Material and Methods 27.2.1 Study Area Characterisation 27.2.2 Data Sources 27.2.2.1 Original Soil Zoning: A Conventional Soil Map with Phases 27.2.2.2 Revised Soil Zoning: A Disaggregated Soil Map 27.2.2.3 Legacy Soil Observations 27.2.2.4 Climate Zoning 27.2.2.5 Landscape Zoning 27.2.2.6 Vineyard Register and Geographical Information System for Agricultural Plots 27.2.2.7 Data Management, GIS, and Statistical Software 27.2.3 Procedure 27.2.3.1 New Homogeneous Terroir Units 27.2.3.2 Quality Index 27.2.3.3 Occupation Index 27.2.3.4 Clustering: HTU Classes by Index 27.2.3.5 Modelling: OI vs. QI 27.3 Results and Discussion 27.3.1 New HTUs from the Disaggregated Soil Map 27.3.2 Quality Index 27.3.3 Occupation Index 27.4 Conclusions References Part VI: Synthesis Chapter 28: Concluding Remarks and Outlook 28.1 Introduction 28.2 What We Know and the Challenges Ahead 28.3 Outlook References Index