- •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
6.6 Soil Families |
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6.6Soil Families
At the fifth level of soil taxonomy hierarchy, 22 soil families in the soil order Aridisols and only two in the soil order Entisols have been mapped in Kuwait. These are briefly described below.
6.6.1 Families in the Soil Order Aridisols
Gypsic Aquisalids, sandy, mixed, hyperthermic—hypersaline, sandy, gypsic, mixed mineralogy soil with water table within 1 m from soil surface.
Typic Aquisalids, sandy, mixed, hyperthermic—hypersaline, sandy, mixed mineralogy soil with water table within 1 m from soil surface.
Petrocalcic Petrogypsids, sandy, mixed, hyperthermic—Petrocalcic and petrogypsic hard pan within 1 m from soil surface, sandy soil with mixed mineralogy.
Petrocalcic Salidic Petrogypsids, sandy, mixed, hyperthermic (shallow)—
Petrocalcic and petrogypsic hard pan within 25 to less than 50 cm from soil surface, sandy soil with mixed mineralogy and ECe of more than 8 to less than 30 dS m−1 in a layer 10 cm or more thick, within 100 cm of the soil surface.
Petrocalcic Salidic Petrogypsids, coarse-loamy, mixed, active, hyperther- mic—Petrocalcic and petrogypsic hard pan within 1 m from soil surface, coarse-loamy soil with mixed mineralogy and ECe of more than 8 to less than 30 dS m−1 in a layer 10 cm or more thick, within 100 cm of the soil surface.
Calcic Salidic Petrogypsids, sandy, mixed, hyperthermic—calcic horizon above the petrogypsic horizon within upper 1 m from soil surface, sandy soil with mixed mineralogy and ECe of more than 8 to less than 30 dS m−1 in a layer 10 cm or more thick, within 100 cm of the soil surface.
Typic Petrogypsids, coarse-gypseous, hypergypsic, hyperthermic—petro- gypsic horizon within upper 1 m from soil surface, coarse-gypseous soil with hypergypsic mineralogy.
Typic Petrogypsids, coarse-gypseous, hypergypsic, hyperthermic (shallow)
—petrogypsic horizon within 25 to less than 50 cm from soil surface, coarse-gypseous soil with hypergypsic mineralogy.
Typic Calcigypsids, sandy, mixed, hyperthermic—both calcic and gypsic horizons within the upper 1 m from soil surface, sandy soil with mixed mineralogy.
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6 Kuwait Soil Taxonomy Hierarchy Soil Families and Soil Series |
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Typic Calcigypsids, coarse-gypseous, hypergypsic, hyperthermic—both calcic and gypsic horizons within the upper 1 m from soil surface, coarse-gypseous sandy soil with hypergypsic mineralogy.
Typic Calcigypsids, coarse-loamy, mixed, semiactive, hyperthermic —both calcic and gypsic horizons within the upper 1 m from soil surface, coarse-loamy soil with mixed mineralogy.
Typic Haplocalcids, sandy, mixed, hyperthermic—calcic horizon within upper 1 m from soil surface, sandy soil with mixed mineralogy.
Typic Haplocalcids, coarse-loamy, mixed, semiactive, hyperthermic—calcic horizon within upper 1 m from soil surface, coarse-loamy soil with mixed mineralogy.
Leptic Haplogypsids, coarse-gypseous, hypergypsic, hyperthermic—gypsic horizon within 18 cm from soil surface, coarse-gypseous soil with hypergypsic mineralogy.
Typic Haplogypsids, sandy, mixed, hyperthermic—gypsic horizon between 18 and 100 cm from soil surface, sandy soil with mixed mineralogy.
Typic Haplogypsids, coarse-gypseous, hypergypsic, hyperthermic—gypsic horizon between 18 and 100 cm from soil surface, coarse-gypseous soil with gypsic mineralogy.
Typic Haplogypsids, coarse-loamy, mixed, semiactive, hyperthermic— gypsic horizon between 18 and 100 cm from soil surface, coarse loamy soil with mixed mineralogy.
Calcic Petrocalcids, sandy, mixed, hyperthermic—a calcic horizon above the petrocalcic horizon within 1 m from soil surface, sandy soil with mixed mineralogy.
Calcic Petrocalcids, sandy, mixed, hyperthermic (shallow)—calcic horizon above the petrocalcic horizon within 25 to less than 50 cm from soil surface, sandy soil with mixed mineralogy.
Calcic Petrocalcids, coarse-loamy, mixed, subactive, hyperthermic—a calcic horizon above the petrocalcic horizon within 1 m from soil surface, coarse loamy soil with mixed mineralogy.
Typic Petrocalcids, sandy, mixed, hyperthermic—a petrocalcic horizon within 1 m from soil surface, sandy soil with mixed mineralogy.
Typic Petrocalcids, sandy, mixed, hyperthermic (shallow)—a petrocalcic horizon within 25 to less than 50 cm from soil surface, sandy soil with mixed mineralogy.
6.6 Soil Families |
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6.6.2 Families in the Soil Order Entisols
Typic Torripsamments, mixed, hyperthermic—deep sandy soil, with mixed mineralogy.
Salidic Torriorthents, sandy-skeletal, carbonatic, hyperthermic—gravely (>35% by volume) sandy deep soil, with carbonatic mineralogy and ECe of more than 8 to less than 30 dS m−1 in a layer 10 cm or more thick, within 100 cm of the soil surface.
6.7Important Definitions (Soil Survey Staff 2014) to Understand Soil Families Characteristics Recognized in Kuwait
6.7.1 Hypergypsic Mineralogy
The soils with horizons in the mineralogy control section that have a substitute class that replaces the particle-size class, other than fragmental, and that have 40 percent or more (by weight) gypsum either in the fine-earth fraction or in the fraction less than 20 mm in diameter, whichever has a higher percentage of gypsum.
6.7.2 Gypsic Mineralogy
Any particle-size class and 15 percent or more (by weight) gypsum, either in the fine-earth fraction (<2 mm soil) or in the fraction less than 20 mm in diameter, whichever has a higher percentage of gypsum.
6.7.3 Carbonatic Mineralogy
Any particle-size class and more than 40 percent (by weight) carbonates (expressed as CaCO3) plus gypsum, either in the fine-earth fraction (< 2 mm soil) or in the fraction less than 20 mm in diameter, whichever has a higher percentage of carbonates plus gypsum.
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6.7.4 Mixed Mineralogy
No specific dominance of minerals, but mixture of minerals presence in soil.
6.7.5 Shallow
The soil where root restricting layer occurs within 25 to less than 50 cm depth.
6.7.6 Coarse-Gypseous
Less than 35 percent (by volume) rock fragments and 50 percent or more (by weight) particles with diameters of 0.1 to 2.0 mm.
6.7.7 Sandy-Skeletal
Have a total content of rock fragments, plus any artifacts 2 mm or larger in diameter which are both cohesive and persistent, of 35 percent or more (by volume) and a texture class of coarse sand, sand, fine sand, loamy coarse sand, loamy sand, or loamy fine sand in the fine-earth fraction (<2 mm).
6.7.8 Sandy
Have a texture class of coarse sand, sand, fine sand, loamy coarse sand, loamy sand, or loamy fine sand in the fine-earth fraction.
6.7.9 Loamy
Have a texture class of loamy very fine sand, very fine sand, or finer, including less than 35 percent (by weight) clay in the fine-earth fraction (< 2 mm), and are in a shallow family or in a Lithic subgroup, or the layer is a part in a strongly contrasting particle-size class.
