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Definition
thick, dark colored, high base saturation, strong structure. Does not become hard and massive when dry. soft, high pH and OM |
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Thick and dark, but too low in base saturation to be mollic. Otherwise, shares all other characteristics with a mollic epipedon |
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too light colored, low organic content or thin to be mollic, may become massive and hard when dry. light colored surface layer. Probably the dominant epipedon on 90% of Virginia. |
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Definition
has 20 to 40 cm of saturated cm of organic soil materials. wet during some part of year usually in marshes and swamps. |
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Definition
thick, black, high in organic matter, common in volcanic ash soils |
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Definition
Highly leached and weathered, light colored, clay and Fe and Al oxides mostly removed |
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Definition
Illuvial high charge clay, most common subsoil, silicate clay accumulation |
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Definition
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Definition
Weak color/structure B, second most common, clay accumulation, changed or altered by physical movement or by chemical reactions, generally non illuvial |
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Definition
Illuvial Fe/Al+humus, organic matter |
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Definition
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Definition
Completely weathered down to Fe + Al oxy-hydroxides – tropical, non sticky type silicate clays |
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Definition
dominantly dense, brittle, root- and waterlimiting layers that are common in many different geomorphic settings of transported material. Water and roots flow/grow only in a few vertical macropores between prism structures, usually loam textured, course prisms |
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Term
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Definition
Cold soils with shallow permafrost; or deep permafrost plus frequent frost churning (cryoturbation). |
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Definition
Soils with a thick (40 cm or more of the top 80 cm) layer of organic soil materials. Requires high OM inputs and generally cold or wet to inhibit OM decomposition. No andic properties. |
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Definition
Coniferous/ericaceous acidic forest soils in sandy parent materials with Spodic horizons (Bh or Bhs). Can also be wet sandy soils in coastal regions. No andic properties. Fe, Al osides and humus accumulation |
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Definition
Soils formed from volcanic ash. High in allophane and CEC, low in density. Must have andic soil properties. Allophane fixes high amounts of P. |
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Definition
Highly weathered tropical soils dominated by Fe+Al oxides and virtually no weatherable minerals left |
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Definition
Soils with high shrink/swell clay content in the upper 50 cm and that crack open regularly to form slickensides. |
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Term
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Definition
Dry soils with a dry moisture regime (< 90 days moist) and accumulation of a secondary mineral. |
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Definition
Highly weathered forest soils with an argillic/kandic horizons (Bt) and low subsoil pH and Base Sat. (< 35%) |
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Term
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Definition
Soils of the prairies with high > 50% base saturation throughout. |
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Definition
Moderately weathered forest soils with an argillic horizon (Bt) but moderate subsoil pH and Base Saturation (high Ca + Mg and Low in Al) |
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Term
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Definition
Soils with a weak diagnostic B horizon (such as a Bw [Cambic]) or a diagnostic epipedon other than Ochric, or other weak diagnostic characteristics. |
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Term
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Definition
Soils without diagnostic B horizons or characteristics and without any epipedon except Ochric. Development is limited by the soil forming factors such as time, climate, P.M., etc. |
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Term
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Definition
Wet at surface in growing season |
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Definition
Moist most of growing season |
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Term
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Definition
Signficant periods of drought |
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Definition
Dry in the growing season |
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Definition
Prounounced wet/dry Mediterranean type climate |
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Definition
rare freezes, can grow citrus |
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Definition
Long growing season, can grow cotton, loblolly but not citrus commercially |
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Definition
Moderate growing season, can grow corn but not those crops listed above |
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Definition
Short growing season, can grow wheat |
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Definition
Too cold for commercial crops |
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