Reference soil Brazil 20: Arenosol

BR020

Arenosols occur over large areas in Africa, central and western Australia, the Middle East and central China. Smaller areas are found along coastlines all over the world.

Characteristics

Soils with a loamy sand or coarser texture either to a depth of at least 100 cm from the soil surface, or to a (petro-)plinthic or salic horizon between 50 and 100 cm from the soil surface. They contain less than 35 percent (by volume) rock fragments or other coarse fragments within 100 cm from the soil surface and have no diagnostic horizons other than an ochric, yermic or albic horizon, a (petro-)plinthic or salic horizon below 50 cm from the soil surface, or an argic or spodic horizon below 200 cm below the soil surface.

Distribution of Arenosols (rough estimation supplied by soilgrids)

 

Reference soil BR020: Arenosols

Very deep, excessively drained, light yellowish brown sand derived from Tertiary sediments. Parent material: Tertiary sediments of the "Barreiras-group", the genesis of the barreiras sediments is not yet understood. Climate of site is considered to be in between station Guarabira and Joao Pessoa (see bra19). Year sum precipitation of Mamanguape is: 1245mm. At a depth of 175cm is present an iron fibre, irregular, wavy, with a thickness of a few mm. See Boletim tecnico no35 (ISRIC-library), slides no. 9827-9831

 

Classification

WRB 2006WRB 1998
Ferralic-Brunic- Arenosol (Eutric)Eutri-Ferralic- Arenosol
-ferralic
0-50 cmochric horizon
-ferralic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Ferralic ArenosolFerralic Arenosol
0-50 cmochric A horizon
-ferralic
0-50 cmochric A horizon
-ferralic

 

Local classification:Areia Quartzosa distrófica