Reference soil Sri Lanka 04: Acrisol

LK004

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 LK004: Acrisol

CLASSIFICATION: 1. Classification by collectors: Udult or Humult. 2. FAO-UNESCO: Nitosol (Nitisol 1988) or Acrisol depending on clay distribution within profile; probably Acrisol because the horizon >104 cm is named B? indicating a lower clay content ( probably more than 20% less than maximum). 3. USDA: Difference between Udult and Humult depends on organic matter content; between Tropudult and Paleudult see point 2. FAO-UNESCO: Humic Nitisol or Humic Acrisol USDA: Tropudult or Sombrihumult (sombric horizon), Paleudult PARENT MATERIAL: Highland series; hard dark basic rocks. GEOLOGICAL FORMATION: Metamorphic rocks of precambrian age. MINERALOGY: Quartz. Watertable: Highest >6 m. Surface drainage: Dendritic, medium textured. Vegetation type: Tropical mountain (small extent of left natural vegetation). Land use: Tea in adjoining crest. Human influence: Burning. Soil fauna: Worm casts. Additional notes on profile description: Ah: Few coarse roots. Bth: Clay/humus and clay/iron cutans. Climate data: Relative humidity = maximal relative humidity below = minimal relative humidity

 

Classification

WRB 2014 
Acrisol