Reference soil China 25: Lixisol

CN025

Lixisols occur dominantly in the drier parts of the tropics and subtropics. Their high base status is partly due to less leaching, partly to admixture from airborne dust from adjacent desert regions.

Characteristics

Soils having an argic horizon (a subsurface horizon with a distinct higher clay content than the overlying horizon), which has a cation exchange capacity of less than 24 cmolc per kg in some part, either starting within either: 100 cm from the soil surface, or 200 cm from the soil surface if the argic horizon is overlain by loamy sand or coarser textures throughout. They have a base saturation (total amount of Ca, Mg, K and Na with respect to the cation exchange capacity) of 50 percent or more in the major part between 25 and 100 cm from the soil surface.

Distribution of Lixisols (rough estimation supplied by soilgrids)

 

Reference soil CN025: Lixisols

PROFILE DESCRIPTION : Very deep, moderately well drained, dark red to red clay derived from Quaternary red clayey deposits. The topsoil is only 11 cm hick and consists of reworked B material. Organic carbon content is low. The subsoil has very strongly developed angular blocky structures. Soil reaction is acid in the surface layers and strongly acid in the subsoil below 50 cm depth. LAND USE AND HUMAN INFLUENCES: the Bt horizon is now only 11 cm from the surface because of terracing. Slide nos. of the ISRIC colection: 13891-13896 (landscape, profile, profile details).

 

Classification

WRB 2006WRB 1998
Cutanic- Lixisol (Profondic Rhodic)Rhodi-Profondic- Lixisol
11-200 cmargic horizon
0-11 cmochric horizon
5-65 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Niti-Haplic LixisolFerric Acrisol
0-11 cmochric A horizon
11-200 cmargic B horizon
- cmargic B horizon
- cmochric A horizon
0-11 cmochric A horizon
11-200 cmargillic B horizon
-weatherable minerals

 

Local classification:Haplic red soil; Argi-Udic Ferrosol
Common name:Red claypan soil