Reference soil Australia 25: Acrisol

AU025

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 AU025: Acrisols

Classification

WRB 1998 
Acrisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Stagni-Humic AcrisolGleyic Acrisol

Local classification:

HAS: Grey-brown Podzolic Soil, Springton light sandy loam; FK: Dy3.22