Unit 4: Soil Taxonomy Chapter 7. Objectives Understand categories of the U.S. taxonomic system How...
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Transcript of Unit 4: Soil Taxonomy Chapter 7. Objectives Understand categories of the U.S. taxonomic system How...
Objectives
Understand categories of the U.S. taxonomic system
How soil properties help distinguish soil families
Knowledge of locations of various soil orders Investigate how soil temps and moistures are
categorized
U. S. System of Soil TaxonomySoils are named, mapped as a geologic entity
or individual
1st taxonomic system began in 1938
NRCS began extensive use of the system in 1965
12 orders separate all soils Pedons are identified to help separate soil orders
(minimum 3.3 ft2, & as deep as roots grow)
U. S. System of Soil Taxonomy
Order Most general category Histosols
Organic soils Entisols
Undeveloped soils Inceptisols
Slightly developed Andisols
Volcanic material Vertisols
Swelling-clay
U. S. System of Soil Taxonomy
Gellisols Must have permafrost in the top 6’
Mollisols Most extensive soils in the U.S. Naturally fertile, slightly leached Can be semiarid to subhumid climates
Alfisols Fertile in favorable moisture conditions Usually very productive
Ultisols Leached, acidic Moderate to low fertility
U. S. System of Soil Taxonomy
Aridisols Arid-region soils Can be very productive
Oxisols Hot, wet tropics Conducive to year-round plant growth
Spodosols Found mostly in cool climates Poorest soils for cultivation Must have lime & fertilization to grow crops
U. S. System of Soil Taxonomy
Suborder Differentiated based on soil properties & horizons Soil moisture, soil temp, dominating effects of chemical
or textural features Great Groups
Differentiated by soil horizons & soil features Accumulated clay, iron, humus, hard pans/cement layers
Subgroup Three kinds of subgroups
Represent the central (typic) concept of the soil group Properties that intergrade towards other groups, etc.
U. S. System of Soil Taxonomy
Properties that prevent its classification as typic or an intergrade to another category
Family Soil properties important to the growth of plants Behavior of soils when used for engineering Important soil properties: texture, mineralogy, pH, avg.
soil temp, moisture, permeability, thickness of horizons, structure, consistency
Series 18,000 soil series identified Typically named after something local Differentiated on the basis of observable & mappable
soil characteristics
U. S. System of Soil Taxonomy
Must have similar color, texture, structure, consistency, thickness, pH, similar horizon arrangements, similar chemical & mineralogy properties
Phase Not considered to be an official category, but being used
to further differentiate, if needed Further delineates soils w/in a series
Soil Moisture & Temperature Regimes Soil Moisture Regimes
Attempt to indicate the extent of naturally available water in the soil depth of maximum root proliferation
Aquic Wet w/ anaerobic saturation long enough to produce
visual evidence of poor aeration Peraquic
Tidal marsh or inland depression where groundwater is always at or near the surface
Soil Moisture & Temperature Regimes
Udic Usually has adequate water throughout the yr
Perudic Extremely wet, percolation in all months when not frozen
Ustic Moisture is limited but is present during the growing
season Xeric
Deficient in water & w/ a dry cropping season Most precipitation in the winter
Soil Moisture & Temperature Regimes
Aridic Very water deficient Long dry periods, short wet periods
Soil Temperature Regimes Based on the mean annual soil temp (MAST) Mean summer soil temp Mean winter soil temp Determined at ~2’ depth Cryic
MAST 46° F
Soil Moisture & Temperature Regimes
Frigid MAST 46° F Mean summer temp >11° F higher than mean winter
temp Mesic
MAST 46 - 59° F Mean summer temp >43° than mean winter temp
Thermic MAST 59 - 72° F Mean summer temp >11° than mean winter temp
Soil Moisture & Temperature Regimes
Hyperthermic MAST >72° F Mean summer temp >11° than mean winter temp
Add iso prefix to the classification if the mean summer & winter temps vary <11° F
Additional Terminology for Family Groupings Particle-size Classes
Fragmental Mostly stones, cobbles, gravel, etc. Fine-earth component <10% of soil volume
Sandy skeletal >35% rock fragments Fine-earth fraction is sand, sandy loam
Loamy skeletal >35% rock fragments Fine-earth fraction loamy
Additional Terminology for Family Groupings
Clayey skeletal >35% rock fragments Fine-earth fraction >35% clay
Sandy Texture is sand, loamy sand
Loamy Finer than sand or loamy, <35% clay
Clayey >35% clay
Very fine >60% clay
Additional Terminology for Family Groupings Soil Mineralogy Classes
Ferritic: >40% iron oxide in fine-earth fraction Kaolinitic: >50% kaolinite & other 1:1 or
nonexpanding clay Carbonatic: >40% carbonates plus gypsum Magnesic: >40% magnesium-silicate minerals Smectitic: clayey soil w/ more smectite than any
other clay Siliceous: >90% silica minerals Mixed: not dominated by any mineral type
Distribution of Soil Orders
Soil orders diverse & unevenly distributed Some land areas don’t correspond to any
order See inside front & back covers for
distributions of soil orders
Gellisols
Occur in tundra regions Cold & relatively barren May have exposed rock intermixed Yukon & Northwest Territories of Canada,
northern 2/3 of Alaska
Histisols
Organic soils formed in cold or wet regions Can occur almost anywhere Found in FL, LA, GA, some in the Great
Lakes states Large area found in Canada
Entisols
Lack horizons due to being a young soil, or weathering is ineffective
Widely distributed in the U.S. Include river floodplains, rocky soils,
mountainous areas, barren islands of East & Gulf coasts, beach sands
Found on all continents Can be excellent ag soil, but may be very
unproductive
Inceptisols
Weakly developed soils More development than Entisols Mostly found in Middle Atlantic & Pacific
states, northern Rockies Develop in many climates Largest area globally found in China
Andisols
Weakly to moderately developed Most from volcanic materials Extensively found in the Pacific Ocean &
Hawaii Some also in the northwestern U.S.
Aridisols
Long dry periods, short periods of wetness Found in the U.S. primarily in the western
mountain states & Pacific states Low rainfall, scattered grasses, desert shrubs Rank second worldwide in area to Entisols
Mollisols
Dark-colored soils of grasslands & some hardwood forests
Deep, dark-colored, fertile A horizon (mollic epipedon) Mollic epipedon extends from surface to ~2’ depth
Properties & Classification of Mollisols Large number of suborders Naturally fertile Easily managed
Mollisols
Management of Mollisols Formed under grasses, forests Tend to be most fertile soil High humus content High concentration of N In wetter climates don’t need irrigation, but in
dryer areas can produce highly May become acidic Black soil colors to depth of 2-3’
Mollisols
1/5 of the U.S. soils Can withstand much variation in cropping Limited leaching Quite fertile, even w/out fertilization Little to no lime needed Only Alfisols may have high natural productivity Texture, depth, climate make it ideal for cropping
and highly valuable
Mollisols
Distribution of Mollisols Found in the Great Plains region of the U.S.
extending north into Canada, south to Gulf of Mexico
Most extensive of U.S. soil orders
Vertisols
Self-mixing soils, >30% shrink/swell clays Found mostly in central & southeastern TX &
along lower Mississippi River
Alfisols
Usually enough precipitation to move clays downward & form an argillic (clay accumulation) horizon
Generally have high CEC’s, usually fairly fertile
Properties & Classification of Alfisols Medium to high supply of basic cations
Evidence of mild leaching Water is adequate for plant growth for 3+ warm
season mos.
Alfisols
Management of Alfisols If topography & climate are favorable; alfisols can
be very productive Most are leached of lime, and can have an acidic
zone If leached enough, forms an E horizon
Erosion exposing clays at the surface not favorable for plant growth
Most naturally productive soils w/out fertilization or irrigation
Alfisols
Usually will require lime amendments Alfisols & Mollisols generally located in a region’s
breadbasket Distribution of Alfisols
North-central states & mountain states Occur on all continents Corn belt of IN, OH, MI, WI, IL Woodland soils in TX, CO
Spodosols
High sand content High rainfall w/ easy leaching
Humus, colloids leached Cold, wet climates are common Mostly found in Cascade Mountains in WA,
OR, New England, & Great Lakes states Also found in FL
Ultisols
Warm, humid regions Usually too acidic to be classified as a
Mollisol/Alfisol, not weathered enough to be an Oxisol
Located in southern Atlantic states, eastern south-central states, Pacific sates
Oxisols
Most extensively weathered soils Typically found on old landforms in tropical,
subtropical climates Found only in HA, Puerto Rico, Guam Extensive in South America, Africa