- •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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Torripsamments that lack all other diagnostic characteristics. These are the soils that represent the central concept of the great group. They are deep and have a texture of sand or loamy sand throughout the top 100 cm of the profile. They are nonsaline and are always calcareous to various degrees but do not have enough pedogenic carbonate accumulation to form a calcic horizon. Torripsamments (27.3%) are the second most extensive soils in Kuwait (Fig. 5.10) after petrogypsids (33.4%).
Typic Torripsamments
References
Dubai Municipality (DM) (2005) Satellite imagery and thematic mapping project, 221p. Executed jointly by Global Scan Technologies (Dubai) and National Remote Sensing Agency, India
EAD (2009a) Soil survey of Abu Dhabi Emirate-extensive survey, vol 1, pp xx+506. Environment Agency–Abu Dhabi, UAE
EAD (2009b) Soil survey of Abu Dhabi emirate, Intensive survey, vol III, pp xviii+435. Environment Agency, Abu Dhabi
EAD-MOEW (2012) Soil survey of the Northern Emirates. Soil Report, vol 1, pp xxvi+410. Environment Agency–Abu Dhabi, UAE
Eswaran H, Reich PF (2005) Aridisols–an overview. In: Encyclopedia of Soils in the Environment
KISR (1999a) Soil survey for the State of Kuwait. Reconnaissance survey, vol II. Kuwait Institute for Scientific Research, Kuwait
KISR (1999b) Soil survey for the State of Kuwait. Semi-detailed survey, vol IV. Kuwait Institute for Scientific Research, Kuwait
Schoeneberger PJ, Wysocki DA, Benham EC, Soil Survey Staff (2012) Field book for describing and sampling soils, version 3.0. Natural Resources Conservation Service, National Soil Survey Center
Shahid SA, Abdelfattah MA, Wilson MA, Kelley JA, Chiaretti JV (2014) United Arab emirates keys to soil taxonomy, 108p. Springer
Soil Science Division Staff (2017) Soil survey manual. U.S. Department of Agriculture Handbook 18. Soil Conservation Service
References |
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Soil Survey Staff (1999) Soil taxonomy: a basic system of soil classification for making and interpreting soil surveys, 2nd edn. US Department of Agriculture Handbook 436. Natural Resources Conservation Service
Soil Survey Staff (2014) Keys to soil taxonomy, 12th edn. US Department of Agriculture, Natural Resources Conservation Service, US Government Printing Office, Washington, DC
Silene villosa grows on sandy soils (Entisols)
Kuwait Soil Taxonomy Hierarchy |
6 |
Soil Families and Soil Series |
Abstract
The soil taxonomy hierarchy of Kuwait is based on two soil surveys, (i) Fourth order Reconnaissance soil survey of Kuwait completed at 1:100,000 scale at the fifth hierarchy level (soil family) of US Soil Taxonomy; and (ii) Second order Semi-detained soil survey of 200,000 ha at scale 1:25,000 scale (with the potential for irrigated agriculture) completed at the sixth level (soil series) of US Soil taxonomy hierarchy. Based on the reconnaissance survey, 2 soil orders, 7 suborders, 8 great groups, 14 subgroups and 24 soil families were mapped. In the semi-detailed survey 39 soil series were mapped. Mixed, carbonatic, gypsic and hypergypsic mineralogy classes are identified. Sandy, sandy-skeletal, coarse-loamy, fine-loamy and coarse-gypseous family textural classes are identified. In this book the terminologies and the standards have been upgraded to the latest USDA protocols.
Keywords
Taxonomy Hierarchy Mineralogy class Particle size class Soil family
Soil series Kuwait
6.1Introduction
The US Soil Taxonomy was used to establish soil families (reconnaissance survey) and soil series (semi-detailed survey). The US Soil Taxonomy (Soil Survey Staff 2014) hierarchy constitutes six levels.
© The Author(s), under exclusive license to Springer Nature |
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Switzerland AG 2022
S. A. Shahid and S. A. S. Omar, Kuwait Soil Taxonomy, https://doi.org/10.1007/978-3-030-95297-6_6
