Reference soil Spain 09: Cambisol
Cambisols occur mainly in the temperate and boreal regions of the world, where the soil’s parent material is still young or where low temperatures slow down the processes of soil formation.
Characteristics
Soils having either a cambic horizon (a horizon showing evidence of alteration with respect to the underlying material), or a mollic horizon overlying a subsoil, which has a base saturation of less than 50 percent in some part within 100 cm from the soil surface, or one of the following diagnostic horizons within the specified depth: an andic, vertic, or vitric horizon starting between 25 and 100 cm; a (petro-)plinthic or salic horizon starting between 50 and 100 cm, in absence of loamy sand or coarser textures above these horizons.
Reference soil ES009: Cambisols
Short profile descripion: A moderately deep well drained yellowish-red fine loamy profile; The structure is moderate strong, and B-horizon shows well developed clayskins. Parent material: solifluction material derived from weathered spillite.
Classification
WRB 2014 | |||||||||||
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Cambisol | |||||||||||
FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||
Chromic Cambisol | Eutric Cambisol | ||||||||||
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