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Understanding the U.S. Soil Taxonomy: Categories, Properties, and Regimes, Slides of Biology

An overview of the u.s. Soil taxonomy system, including its history, categories of soils, and how soil properties help distinguish different soil families. It covers the 12 orders of soil, their properties, and the suborders, great groups, families, and series within each order. Additionally, it discusses soil moisture and temperature regimes.

Typology: Slides

2012/2013

Uploaded on 01/17/2013

parameshwari
parameshwari 🇮🇳

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Download Understanding the U.S. Soil Taxonomy: Categories, Properties, and Regimes and more Slides Biology in PDF only on Docsity! Unit 4: Soil Taxonomy Docsity.com 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 Docsity.com 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 Docsity.com 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 Docsity.com 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. Docsity.com 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 Docsity.com 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 Docsity.com 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 Docsity.com 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 Docsity.com 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 Docsity.com 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 Docsity.com Docsity.com 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 Docsity.com Ee 9 ° > — iQ © ° a Docsity.com DOMINANT SUBORDERS (ES Aquents (I Orthents WM Arents (2) Psamments Aiea Fluvents Docsity.com 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 Docsity.com Docsity.com DOMINANT SUBORDERS GS Aquands (MM Udands (1) xerands (EE cryands (BD ustands (MS torrands (MMM Vitrands Doesity.com 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 Docsity.com 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 Docsity.com 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’ Docsity.com 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 Docsity.com DOMINANT SUBORDERS MM Albolils MBB) Rendolls ME) Xerolls BY Aquolls HBB Udolls z= Cryolls BS Ustalls Docsity.com Vertisols • Self-mixing soils, >30% shrink/swell clays • Found mostly in central & southeastern TX & along lower Mississippi River Docsity.com Ee = Vera 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 Docsity.com 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 Docsity.com Docsity.com ot i lil ae = eat aii Doesity.com _ Docsity.com 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 Docsity.com 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 Docsity.com Do€sity com PUERTO RICO DOMINANT SUBORDERS ey Aquox = Udox [0 Perox HR Ustox i Torrox — US. VI. —_ Docsity.com
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