Reference soil Indonesia 38: Acrisol

ID038

Acrisols occur dominantly in the wetter parts of the tropics and subtropics and the warm temperate regions in relatively young landscapes.

Characteristics

Soils having an argic horizon (a subsurface horizon with 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 100 cm from the soil surface, or within 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 less than 50 percent in the major part between 25 and 100 cm from the soil surface

Distribution of Acrisols (rough estimation supplied by soilgrids)

 

Reference soil ID038: Acrisols

ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ah2 - Friable to firm. Bw - Multicoloured: 2.5Y6/2 (60%), 10YR3.5/1 (40%); friable to firm. Bt1 - Multicoloured: 2.5Y6/4 (50%), 10YR6/6 (50%); mottles: irregular, unspecified iron mottles; colour cutans: 2.5Y6/2. Bt2 - mottles: irregular, unspecified iron mottles. III - mottles: very coarse, irregular, unspecified iron mottles.

 

Classification

WRB 2006 
Endogleyic-Cutanic- Acrisol (Alumic Humic) 
32-89 cmargic horizon
-reducing conditions
-gleyic colour pattern
 
32-89 cmargic horizon
-reducing conditions
-gleyic colour pattern
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Gleyic AcrisolFerric Acrisol
0-22 cmochric A horizon
32-89 cmargic B horizon
0-22 cmochric A horizon
32-89 cmargillic B horizon
-ferric

 

Local classification:Podsolik Haplik