TSV

WRB Reference Soil Groups - TSV

The WRB Reference Soil Groups represent the highest hierarchical level in the World Reference Base for Soil Resources (WRB), established by the International Union of Soil Sciences (IUSS). The fourth edition of 2022 defines 32 Reference Soil Groups (RSGs), systematically classified based on soil-forming processes and characteristics. This classification system is widely used as a standard reference for creating soil maps and facilitating international soil information exchange.

soil classification WRB IUSS Reference Soil Groups soil science pedology
code	slug	name	description	category
HS	histosol	Histosol	Soils with thick organic layers.	Soils with thick organic layers
AT	anthrosol	Anthrosol	Soils with long and intensive agricultural use, often altered to enhance fertility.	Soils with strong human influence
TC	technosol	Technosol	Soils containing significant amounts of artefacts.	Soils with strong human influence
CR	cryosol	Cryosol	Permafrost-affected soils.	Soils with limitations to root growth
LP	leptosol	Leptosol	Thin soils or soils with many coarse fragments.	Soils with limitations to root growth
SN	solonetz	Solonetz	Soils with a clay-enriched subsoil with high concentrations of exchangeable Na.	Soils with limitations to root growth
VR	vertisol	Vertisol	Soils with high contents of shrink-swell clays, alternating wet-dry conditions.	Soils with limitations to root growth
SC	solonchak	Solonchak	Soils with high concentrations of soluble salts.	Soils with limitations to root growth
GL	gleysol	Gleysol	Groundwater-dominated soils, underwater or in tidal areas.	Soils distinguished by Fe/Al chemistry
AN	andosol	Andosol	Soils with allophanes and/or complexes of Al and organic matter.	Soils distinguished by Fe/Al chemistry
PZ	podzol	Podzol	Soils with subsoil accumulation of organic matter and/or oxides.	Soils distinguished by Fe/Al chemistry
PT	plinthosol	Plinthosol	Soils with accumulation and redistribution of Fe.	Soils distinguished by Fe/Al chemistry
PL	planosol	Planosol	Soils with stagnant water and abrupt textural difference.	Soils distinguished by Fe/Al chemistry
ST	stagnosol	Stagnosol	Soils with stagnant water and no or only moderate textural difference.	Soils distinguished by Fe/Al chemistry
NT	nitisol	Nitisol	Soils with low-activity clays, P fixation, many Fe oxides, strongly structured.	Soils distinguished by Fe/Al chemistry
FR	ferralsol	Ferralsol	Soils with dominance of kaolinite and oxides.	Soils distinguished by Fe/Al chemistry
CH	chernozem	Chernozem	Soils with very dark and well-structured topsoil and secondary carbonates.	Pronounced accumulation of organic matter in the mineral topsoil
KS	kastanozem	Kastanozem	Soils with dark topsoil and secondary carbonates.	Pronounced accumulation of organic matter in the mineral topsoil
PH	phaeozem	Phaeozem	Soils with dark topsoil, no secondary carbonates (unless very deep), and high base status.	Pronounced accumulation of organic matter in the mineral topsoil
UM	umbrisol	Umbrisol	Soils with dark topsoil and low base status.	Pronounced accumulation of organic matter in the mineral topsoil
DU	durisol	Durisol	Soils with accumulation of, and cementation by, secondary silica.	Accumulation of moderately soluble salts or non-saline substances
GY	gypsisol	Gypsisol	Soils with accumulation of secondary gypsum.	Accumulation of moderately soluble salts or non-saline substances
CL	calcisol	Calcisol	Soils with accumulation of secondary carbonates.	Accumulation of moderately soluble salts or non-saline substances
RT	retisol	Retisol	Soils with interfingering of coarser-textured, lighter-coloured material into a finer-textured, stronger-coloured layer.	Soils with clay-enriched subsoil
AC	acrisol	Acrisol	Soils with low-activity clays and exchangeable Al greater than exchangeable base cations.	Soils with clay-enriched subsoil
LX	lixisol	Lixisol	Soils with low-activity clays and exchangeable base cations equal to or greater than exchangeable Al.	Soils with clay-enriched subsoil
AL	alisol	Alisol	Soils with high-activity clays and exchangeable Al greater than exchangeable base cations.	Soils with clay-enriched subsoil
LV	luvisol	Luvisol	Soils with high-activity clays and exchangeable base cations equal to or greater than exchangeable Al.	Soils with clay-enriched subsoil
CM	cambisol	Cambisol	Moderately developed soils.	Soils with little or no profile differentiation
FL	fluvisol	Fluvisol	Soils with stratified fluviatile, marine or lacustrine sediments.	Soils with little or no profile differentiation
AR	arenosol	Arenosol	Very sandy soils.	Soils with little or no profile differentiation
RG	regosol	Regosol	Soils with no significant profile development.	Soils with little or no profile differentiation