Reference soil China 46: Stagnosol
Stagnosols are often related to Luvisols and occur for the greater part in humid and perhumid temperate regions in West and Central Europe, North America, Australia and Argentina.
Characteristics
Soils having within 50 cm of the soil surface reducing conditions (soil conditions with low redox potential (negative logarithm of the hydrogen potential (rH) and presence of free iron (Fe2+) on freshly broken surfaces) and in 50% of the layer a stagnic colour pattern (strong mottling of soils in such a pattern that peds surfaces are lighter (at least one Munsell value) and paler (at least one chroma) than ped interiors, which are more reddish and brighter (at least one chroma)). The stagnic color pattern develops under temporarily saturation of a perched water table from surface water, long enough to allow reducing conditions to arise. The topsoil can be bleached and concretions can occur in the subsoil. They develop often in slowly permeable, unconsolidated materials of various origins.
Reference soil CN046: Stagnosols
PROFILE DESCRIPTION : Shallow, moderately well drained, reddish brown sandy clay loam to silty clay developed from solid rock derived from sandstone. The soil has between 28 and 46 cm depth a slowly permeable layer as reflected by common low chroma mottles. It is uncertain if the topsoil is original or aggradated.