Reference soil China 07: Ferralsol

CN007

Ferralsols occur in tropical and subtropical regions of the world, mainly on old and stable land surfaces.

Characteristics

Soils having a ferralic horizon (strongly weathered horizon with low-activity clays and very low amounts of weatherable minerals) between 25 and 200 cm from the soil surface. They lack a nitic horizon (a horizon with strongly developed, nut-shaped structure) and do not have a layer which fulfils the requirements of an argic horizon and which has, in the upper 30 cm, 10 percent or more water-dispersible clay.

Distribution of Ferralsols (rough estimation supplied by soilgrids)

 

Reference soil CN007: Ferralsols

PROFILE DESCRIPTION : Very deep, well drained red sandy clay loam derived from granite. The brownish coloured topsoil is low in organic carbon and very low in bases. The uniformly coloured red subsoil has only weakly developed subangular blocky structures or appears as porous massive. The soil reaction is acid througout. GEOLOGY: medium grained Mesozoic granite / HYDROLOGY: coarse dendritic surface drainage; infiltration is estimated at 25-50 cm/day / SOIL FAUNA: few ants and worms / HUMAN INFLUENCES: reforestation as anti-erosion measure, sometimes taking place by air seeding of pine. Slide nos. of the ISRIC collection: 5980-5986 (profile, landscape, vegetation). Thin section nos. of the ISRIC collection: 2714-2720.

 

Classification

WRB 2006WRB 1998
Vetic- Ferralsol (Alumic Epidystric)Alumi-Vetic- Ferralsol
5-150 cmferralic horizon
0-19 cmochric horizon
5-150 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Ferralic CambisolOrthic Ferralsol
0-19 cmochric A horizon
- cmcambic B horizon
- cmochric A horizon
-ferralic
0-19 cmochric A horizon
5-115 cmoxic B horizon

 

Local classification:Eutrophic latored soil; Hapli-Udic Ferralosol
Common name:Red floury clay