Reference soil China 15: Arenosol

CN015

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 CN015: Arenosols

Very deep, somewhat excessively drained, very pale brown fine sand. Strongly tilted stratification is clearly visible from about 15 cm and deeper; thin layers are differentiated from each other by colour and granulometric differences. About 10-20% of the sand grains consist of dark coloured grains. HYDROLOGY: depth of ground water level is more than 10 m / VEGETATION: the semi-fixed sand dunes have a 10% (or less) vegetational coverage consisting mainly of Aristida, Haloxylon, Calligonum, Echinopsilon and Alhagia

 

Classification

WRB 2006WRB 1998
Protic- Arenosol (Eutric Aridic)Proti-Aridic- Arenosol (Eutric)
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Proto-Haplic ArenosolEutric Regosol

 

Local classification:Haplic blown sand soil; Aridi-Sandic Primosol
Common name:Dune sand