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Soil classification and soil maps

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

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Soil classification and soil maps

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  1. Soil classification and soil maps

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

  3. Pedon – basic unit of soil classification

  4. 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)

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

  6. Three ORDERS in old system • Zonal or “normal” soils • -climate inputs dominate a soil’s genesis • -soil is in equilibrium with the climate/veg • 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

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

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

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

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

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

  12. 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)

  13. Xeric Argiduridsubgroup Fine, smectitic, mesic Xeric Argidurids Family Aridisolorder Series: Reno Duridsuborder ArgiduridGreat Group

  14. More about families Cation exchange class (sometimes) e.g., active, semiactive, superactive Sandy, mixed, frigid Typic Haplorthods Depth class (sometimes) Mineralogy Texture (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)

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

  16. Cryic Frigid Mesic Thermic Hyperthemic

  17. Frigid Mesic Mesic Mesic

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

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

  20. Drainage class subgroup designation Well drained or drier ------- -------------- Moderately well drained Aquic ---------------- Somewhat poorly drained Aeric --------aqu----- Poorly drained ------- --------aqu----- Very poorly drained ------- -------------ist More practice… 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

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

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

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

  24. 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, one, or several

  25. 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

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

  27. 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

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

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

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

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

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

  33. 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

  34. 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

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

  36. 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

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

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

  39. 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

  40. 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

  41. 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

  42. Diagnostic subsurface horizons Calcic - accumulation of secondary CaCO3 If cemented – Petrocalcic Ifplugged - Bkk Bk, Bkm

  43. 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

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

  45. Diagnostic subsurface horizons Sulfuric - pH < 3.5, yellow (jarosite) mottles - toxic to plants - in tidal marshes

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

  47. 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

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