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Hint
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Soil Group
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Has at least 40cm of organic matter starting within 40cm from the soil surface.
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Histosol
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Has been formed or heavily modified due to long-term human influences, such as irrigation.
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Anthrosol
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Contains a significant amount of artifacts in the soil (something that is made or extracted from earth by humans).
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Technosol
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Contains permafrost within 1m of soil surface.
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Cryosol
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Continiuous rock starting within 25cm of the soil surface.
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Leptosol
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Has a high concentration of exchangable sodium.
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Solonetz
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Clay-rich soil that shows cracks on the surface.
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Vertisol
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Has a high concentration of soluble salts.
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Solonchak
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Groundwater-dominated soil, showing reducing and oxidating conditions.
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Gleysol
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Soil that is dominated by volcanic ash materials.
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Andosol
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Has a ash-grey E-horizon formed by intense leaching.
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Podzol
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Has a high concentration of plinthite in the soil.
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Plinthosol
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Has a textural discontinuity, causing seasonal waterlogging.
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Planosol
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Water stagnates in the upper soil layer above a slowly permeable layer.
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Stagnosol
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Deep, well-structured nitic horizon with shiny ped faces and stable aggregates.
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Nitisol
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Very deeply weathered, iron- and aluminum-rich, low-activity clays.
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Ferralsol
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Deep, dark humus-rich topsoil with high base saturation and a mollic horizon.
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Chernozem
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Has a brownish, humus-rich surface horizon typical of steppe climates.
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Kastanozem
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Humus-rich surface horizon, but more leached and with moderate rainfall
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Phaeozem
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Has a thick, dark, humus-rich surface layer.
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Umbrisol
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A soil that has a lot of accumulated silica.
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Durisol
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A soil that has a lot of accumulated gypsum.
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Gypsisol
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A soil that has a lot of accumulated carbonates.
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Calcisol
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Has a distinctive net-like pattern of pale, clay-poor layers within a darker, clay-rich layer.
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Retisol
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Strongly weathered soil with a clay-rich subsurface horizon and low base saturation
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Acrisol
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Has an argic horizon with low base saturation and low-activity clays
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Lixisol
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Has an argic horizon with low base saturation and high-activity clays.
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Alisol
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Has an argic horizon with high base saturation.
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Luvisol
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Weakly developed soils showing initial alteration but no major accumulation.
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Cambisol
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Young soils formed in recent alluvial deposits with stratification.
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Fluvisol
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Very sandy soils with little profile development.
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Arenosol
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Has no significant profile development.
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Regosol
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