Soil classification and soil maps Why a classification

Soil classification and soil maps

Why a classification system for soils? -mapping -taxation -inventory -management/use

Pedon – basic unit of soil classification

Classification system must be: 1. based on quantifiable characteristics of soils 2. open-ended (we do not know about every soil…) 3. hierarchical (like biological systems) Also – use new names (avoid old meanings and baggage)

The “old” (1938) system of soil classification -based on interpretation and assumed genesis -grouped soils based on climate/vegetation assemblages

Three ORDERS in old system 1. Zonal or “normal” soils -climate inputs dominate a soil’s genesis -soil is in equilibrium with the climate/veg 2. Intrazonal soils -salts, wetness or limestone bedrock overwhelm the soil’s genesis 3. Azonal soils -too young, dry or sandy to have developed into Zonal soils

Zonal soils – examples Podzols – cool climates, coniferous forest Brunizems – tallgrass prairies Sierozems – desert soils Laterite soils – red tropical soils

Intrazonal soils – examples Rendzinas – shallow to limestone bedrock Gley soils – wet soils Peat soils

Azonal soils – examples Dry, sandy soils Shallow-to-bedrock soils Alluvial soils (young parent materials)

The new system of SOIL TAXONOMY -adopted in 1975, revisions ever since

Order – highest level (12) Suborder – (>60) Great Group – (about 300) Subgroup – (about 1600) Family – (>8000) Series – (>14, 000)

The 12 soil orders • • • Gelisols – cold soils, permafrost (-el) Histosols – organic soils, usually Very PD (-ist) Spodosols – podzolization, cool, moist forested areas (-od) Andisols – volcanic ash parent materials (-and) Oxisols – old, weathered soils of the humid tropics, oxide clays (-ox) Vertisols – shrink-swell clays, wet-dry climate, deep cracks (-ert) Aridisols – desert soils, some evidence of B horizon formation (-id) Ultisols – 1: 1 clays dominate, red, weathered soils but not like Oxisols (-ult) Mollisols – thick, dark A horizon, grassland soils (-oll) Alfisols – minimally weathered soils, lessivage, not highly acidic (-alf) Inceptisols – weak B horizon development, some pedogenesis (-ept) Entisols – most weakly developed soils, no diagnostic B horizon (-ent)

Xeric Argidurid subgroup Fine, smectitic, mesic Xeric Argidurids Family Aridisol order Series: Reno Durid suborder Argidurid Great Group

More about families Cation exchange class (sometimes) e. g. , active, semiactive, superactive Sandy, mixed, frigid Typic Haplorthods Depth class (sometimes) Texture Mineralogy (Particle size family) Soil temperature regime (Table 7. 13 in your book) Soil MOISTURE REGIME – can be determined from the taxonomic name (we’ve done this already)

The soil TEMPERATURE REGIME is all based on the MAST at 50 cm depth Four most common ones MAST Cryic <8 C (but no permafrost)…like central Canada Frigid <8 C (but warm in summer)…like da UP Mesic 8 – 15 C………………like Ohio Thermic 15 – 22 C……………like Georgia Hyperthermic >22 C………………. like Cuba

Cryic Frigid Mesic Thermic Hyperthemic

Frigid ic es M Mesic

“Iso-” minimal seasonal variation in soil temperature islands, and the tropics

It’s usually possible to estimate the drainage class of a soil, knowing only it’s taxonomic subgroup. Here’s how: Drainage class Well drained or drier Moderately well drained Somewhat poorly drained Poorly drained Very poorly drained subgroup designation -------------Aquic Aeric -----------------------aqu----------ist

Drainage class More practice… Well drained or drier Moderately well drained Somewhat poorly drained Poorly drained Very poorly drained subgroup designation -------------Aquic Aeric -----------------------aqu----------ist Fine-silty, siliceous, active, thermic Aeric Albaqualfs Loamy, mixed, active, mesic Aquic Arenic Hapludults Clayey, smectitic, shallow Typic Haplocryolls Coarse-loamy, mixed, active, mesic Aquic Fragiudepts Loamy-skeletal, mixed, superactive, thermic Cambidic Haplodurids Coarse-loamy, mixed, superactive, calcareous, mesic Aquic Torriorthents

More about subgroups… Three kinds: 1. Central concept – the “Typics” Typic Haplorthods Typic Dystrudepts Typic Eutrustox

More about subgroups… Three kinds: 1. Central concept 2. Intergrades – trending toward another ORDER Alfic Haplorthods Spodic Dystrudepts Ultic Eutrustox

More about subgroups… Three kinds: 1. Central concept 2. Intergrades 3. Extragrades – with some other important or limiting attribute Lamellic Haplorthods Lithic Dystrudepts Aquic Eutrustox

Soil Taxonomy a quantitative system of soil classification, largely based on diagnostic horizons Diagnostic horizons at the surface – epipedons (all soils have one, and only one) Diagnostic subsurface horizons – soils may have none, or several

Epipedons – the major ones Mollic – mandatory for Mollisols Ca++ ions common, base saturation >50% value <3. 5 moist, <5. 5 dry chroma <3. 5 moist OC > 0. 6% Generally >25 cm thick moist for 3+ months at a time thru the year

Epipedons – the major ones Anthropic: resembles mollic, but can be dry high in phosphorous (due to long-term agriculture or human occupation)

Epipedons – the major ones Umbric: same as mollic, but base sat. <50% mountainous or hilly regions moist, acidic soils where OM decomposition is slowed due to high water table or cold temps

Epipedons – the major ones Histic – mandatory for Histosols water saturated for 30+ consecutive days (most years) organic materials dominate

Epipedons – the major ones Plaggen and Melanic – minor ones, we won’t discuss

Epipedons – the major ones Ochric: all others usually light colored, thin forested and dry soils

Diagnostic subsurface horizons -can be E or B horizons Entisols, by definition, lack a diagnostic B horizon

Diagnostic subsurface horizons Albic – E horizons (must meet thickness and color requirements)

Diagnostic subsurface horizons Argillic – clay-enriched Bt horizons - illuvial silicate clays (NOT formed in place) indicates a stable surface, because illuviation is slow, and therefore it must exceed rate of argillan destruction if argillans are to be present in sands, clay bridging is acceptable Required for Alfisols, Ultisols

Diagnostic subsurface horizons Glossic -degradation of an argillic (or kandic or natric) horizon -E/Bt or Bt/E -tongues of E material penetrating B material

Diagnostic subsurface horizons Natric: same as argillic, but has either: (1) prisms/columns in upper part, or (2) high Na content Bn or Btn

The poop on Na+ At low electrolyte concentrations, Na+ favors dispersion, just like other +1 cations (Na in upper profile can favor lessivage) At high electrolyte concentrations, as is typical of most desert and dryland soils, Na enhances flocculation. Btn becomes very clay-rich, and is virtually impermeable when wet. Biscuit tops Btn

Diagnostic subsurface horizons Kandic – like argillic, but low CEC clays dominate has lots of kaolinite and many oxide clays Bt Only in Ultisols Kandiudult

Illuvial clay ARGILLIC Degraded - Glossic Na-rich - Natric Oxide clays – Kandic

Diagnostic subsurface horizons Spodic - amorphous Al and humus, with or without Fe - sandy soils, little clay to inhibit podzolization - rapidly forming, under forest or heath veg. Required for Spodosols Bh, Bs, Bhs, Bsm, Bhsm

Diagnostic subsurface horizons Placic - thin pan, dark, cemented by Fe, Mn, and/or OC - 2 -10 mm thick, brittle Has many similarities to Spodic horizon

Diagnostic subsurface horizons Oxic - mineral horizon in advanced stage of weathering - clay minerals are 1: 1 or oxides - residual accumulation of Al, Ti, Fe and Mn - very old, stable surfaces - tropical/subtropical, wet/dry climates Required for Oxisols Bo

Diagnostic subsurface horizons Calcic - accumulation of secondary Ca. CO 3 If cemented – Petrocalcic Ifplugged - Bkk Bk, Bkm

Diagnostic subsurface horizons Gypsic - rich in secondary gypsum/sulfates - sea spray and gypsic parent materials are sources - difficult to differentiate from Bk If cemented - petrogypsic By, Bym

Diagnostic subsurface horizons Salic - soluble salts (more soluble than gypsum) Bz

Diagnostic subsurface horizons Sulfuric - p. H < 3. 5, yellow (jarosite) mottles - toxic to plants - in tidal marshes

Diagnostic subsurface horizons Fragipan – Btx, Bx, Ex Duripan – silica cementation - Xeric soil moisture regimes - Bqm

Diagnostic subsurface horizons When all else fails…. Cambic weak "color" B horizon Bw horizon (some Bg horizons) must lack geologic structure or have soil structure not sandy (Bw forms too quickly in sands) Having a Cambic horizon kicks the soil OUT of Entisols and (usually) into Inceptisols Bw