- •Foreword
- •Preface
- •Acknowledgements
- •Preamble
- •Contents
- •About the Authors
- •List of Figures
- •Abstract
- •1.1 Introduction
- •1.2 History of Soil Classification Systems
- •1.2.1 Soil Classification Systems
- •1.2.1.1 Australian Soil Classification System (2016)
- •1.2.1.2 Canadian Soil Classification System
- •1.2.1.3 Chinese Soil Taxonomy
- •1.2.1.4 England and Wales Soil Classification System
- •1.2.1.5 France Soil Classification System
- •1.2.1.6 Kuwait Soil Taxonomy Hierarchy
- •1.2.1.7 Norway Soil Classification System
- •1.2.1.8 Russian Soil Classification System
- •1.2.1.9 South African Soil Classification System
- •1.2.1.10 United Arab Emirates Keys to Soil Taxonomy
- •1.2.1.11 USDA-NRCS Keys to Soil Taxonomy
- •1.2.1.12 World Reference Base for Soil Resources (WRB Classification)
- •References
- •Abstract
- •2.1 Introduction
- •2.2 The Soil That We Classify
- •2.3 Lower Boundary of Soil
- •2.4 Nonsoil Materials
- •2.5 Buried Soils
- •References
- •Abstract
- •3.1 Introduction
- •3.2 Basic System of Horizon and Layer Designations
- •3.2.1 Master Horizons and Layers
- •3.2.2 Suffix Symbols
- •3.2.3 Conventions for Using Horizon Designation Symbols
- •3.2.4 Vertical Subdivisions
- •3.2.5 Discontinuities
- •3.2.6 The Prime Symbol
- •3.2.7 The Caret Symbol
- •3.3 Diagnostic Surface and Subsurface Horizons
- •3.3.1 The Epipedon
- •3.3.1.1 Ochric Epipedon
- •3.3.2 Diagnostic Subsurface Horizons
- •3.3.2.1 Anhydritic Horizon
- •3.3.2.2 Argillic Horizon
- •3.3.2.3 Calcic Horizon
- •3.3.2.4 Cambic Horizon
- •3.3.2.5 Gypsic Horizon
- •3.3.2.6 Petrocalcic Horizon
- •3.3.2.7 Petrogypsic Horizon
- •3.3.2.8 Salic Horizon
- •3.4 Diagnostic Soil Characteristics
- •3.4.1 Free Carbonates
- •3.4.2 Identifiable Secondary Carbonates
- •3.4.3 Aquic Conditions
- •3.4.4 Lithic Contact
- •3.4.5 Soil Moisture Regimes
- •3.4.5.1 Soil Moisture Control Section
- •3.4.5.2 Classes Soil Moisture Regimes
- •3.4.6 Soil Temperature Regimes
- •References
- •4 Families and Series Differentiae
- •Abstract
- •4.1 Introduction
- •4.2.1 Control Section for Particle-Size Classes
- •4.2.1.1 Root-Limiting Layers
- •4.2.1.3 Key to the Particle-Size and Substitute Classes
- •4.3 Mineralogy Classes
- •4.3.1 Control Section for Mineralogy Classes
- •4.3.2 Key to Mineralogy Classes
- •4.4.1 Use of the Cation-Exchange Activity Classes
- •4.4.3 Key to Cation-Exchange Activity Classes
- •4.5 Soil Temperature Class
- •4.5.1 Control Section for Soil Temperature
- •4.5.2 Key to Soil Temperature Class
- •4.6 Soil Depth Classes
- •4.6.1 Key to Soil Depth Classes
- •4.7 Series Differentiae Within a Family
- •4.7.1 Control Section for the Differentiation of Series
- •4.7.1.1 Key to the Control Section for the Differentiation of Series
- •References
- •Abstract
- •5.1 Introduction
- •5.2 Soil Orders Identified in Kuwait
- •5.2.1 Aridisols
- •5.2.2 Entisols
- •5.3 Understanding Soil Taxonomic Classes
- •5.4 Key to Soil Orders
- •5.5 Key to Suborders of Aridisols
- •5.5.1 Argids
- •5.5.2 Calcids
- •5.5.3 Cambids
- •5.5.4 Gypsids
- •5.5.5 Salids
- •5.6 Key to Suborders of Entisols
- •5.6.1 Orthents
- •5.6.2 Psamments
- •References
- •Abstract
- •6.1 Introduction
- •6.2 Soil Orders
- •6.2.1 Entisols
- •6.2.2 Aridisols
- •6.3 Soil Suborders
- •6.4 Soil Great Groups
- •6.5 Soil Subgroups
- •6.6 Soil Families
- •6.6.1 Families in the Soil Order Aridisols
- •6.6.2 Families in the Soil Order Entisols
- •6.7.1 Hypergypsic Mineralogy
- •6.7.2 Gypsic Mineralogy
- •6.7.3 Carbonatic Mineralogy
- •6.7.4 Mixed Mineralogy
- •6.7.5 Shallow
- •6.7.6 Coarse-Gypseous
- •6.7.7 Sandy-Skeletal
- •6.7.8 Sandy
- •6.7.9 Loamy
- •6.7.10 Coarse-Loamy
- •6.7.11 Fine-Loamy
- •6.7.12 Hyperthermic
- •References
- •Abstract
- •7.1 Introduction
- •7.2 Soil Samples Collection, Preparation and Processing
- •7.4 Coarse Fragments
- •7.5 Moisture Content
- •7.6 Loss on Acid Treatment (LAT)
- •7.9 Extractable Cations
- •7.11 Exchangeable Sodium Percentage (ESP)
- •7.12 Saturation Percentage (SP)
- •7.13 Preparation of Saturated Soil Paste
- •7.14 Saturation Extract Analysis
- •7.15 Electrical Conductivity of Soil Saturation Extract (ECe)
- •7.16 Osmotic Potential (OP)
- •7.17 Soil Reaction or Hydrogen Ion Activity (pH)
- •7.18 Sodium Adsorption Ratio (SAR)
- •7.19 Water Retention
- •7.20 Bulk Density (BD)
- •7.21 Particle Density (PD)
- •7.22 Porosity
- •7.23 Soil Organic Matter and Organic Carbon
- •7.24 Engineering Data
- •7.24.1 Atterberg Limits
- •7.24.1.1 Liquid Limit (LL)
- •7.24.1.2 Plastic Limit (PL)
- •7.24.1.3 Plasticity Index (PI)
- •7.24.2 Percent Passing Sieves
- •7.24.3 Unified Soil Classification System (USCS)
- •7.24.4 AASHTO Group Classification
- •7.25 Soil Mineralogy
- •7.26 Clay Mineralogy
- •7.26.1 X-Ray Diffraction Criteria
- •References
- •Author Index
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5 Identification of the Taxonomic Class of a Soil |
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Fig. 5.2 A view of sandy desert landscape presenting Entisols soil order covering 30% of surveyed area in Kuwait
5.2.2 Entisols
In US Soil Taxonomy (Soil Survey Staff 2014), Entisols is one of the twelve soil orders, defined as soils that do not show any profile development other than an A horizon. All deep sandy soils (sand sheets, sand dunes) without any development are classified under Entisols. The Entisols has no diagnostic horizons (calcic, gypsic, salic, petrocalcic, petrogypsic etc.), and the parent material is unaltered. The Entisols are the most abundant soil order, occupying about 16% of the global ice-free land area (Fig. 5.2).
5.3Understanding Soil Taxonomic Classes
It is mandatory that the user of this chapter for the identification of soil taxa to be well familiar with the definitions of master horizons, diagnostic horizons, and the terms defined in the Soil Survey Manual (Soil Science Division Staff 2017) and the Field Book for Describing and Sampling Soils (Schoeneberger et al. 2012).
