Reference soil Jamaica 01: Acrisol

JM001

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 JM001: Acrisols

pH in field measured with Truog Soil Reaction Field kit.

 

Classification

WRB 2006WRB 1998
Cutanic- Acrisol (Alumic Humic Hyperdystric)Alumi-Humic- Acrisol (Hyperdystric Chromic)
23-109 cmargic horizon
0-23 cmochric horizon
23-109 cmargic horizon
-strongly humic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Humic AcrisolHumic Acrisol
0-23 cmochric A horizon
23-109 cmargic B horizon
-strongly humic
0-23 cmochric A horizon
23-109 cmargillic B horizon
-ferric
-high organic matter content in B horizon
-high organic matter content in the B horizon

 

Local classification:Chudleigh clay loam