Reference soil China 30: Ferralsol

CN030

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 CN030: Ferralsols

PROFILE DESCRIPTION : Deep, well drained, yellowish red clay derived from Quaternary red clay deposits. The topsoil has weakly to moderately developed (sub-)angular blocky structures while the subsoil is strong to very strong angular blocky. Organic carbon content is low and the soil reaction is strongly acid throughout. Dry soil breaks into enormous angular elements. PARENT MATERIAL: on a 20m higher plateau (distance 1km from site) 2-3m red Quaternary clay lies over an unconsolidated conglomerate. Slide nos. of the ISRIC collection: 13922-13928 (landscape, profile, profile details, vegetation, erosion features).

 

Classification

WRB 2006WRB 1998
Haplic- Ferralsol (Hyperdystric Clayic Xanthic)Hyperdystric- Ferralsol
0-200 cmferralic horizon
0-18 cmochric horizon
0-200 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Ferralic CambisolFerralic Cambisol
0-18 cmochric A horizon
- cmcambic B horizon
- cmochric A horizon
-ferralic
0-18 cmochric A horizon
18-225 cmcambic B horizon
-ferralic

 

Local classification:Yellowic para-red soil; Hiweatheri-Udic Ferrosol
Common name:Acid red clay