Reference soil Indonesia 37: Phaeozem

ID037

Phaeozems occur all over the world, but especially on the more moist side of the steppe regions, bordering Chernozems.

Characteristics

Soils having a mollic horizon (deep, brownish or blackish surface horizon with a significant accumulation of organic matter and high base saturation); a base saturation of 50 percent or more between 25 and 100 cm from the soil surface; a calcium carbonate-free soil matrix at least to a depth of 100 cm from the soil surface, or to a contrasting layer between 25 and 100 cm; no diagnostic horizons other than an albic, argic, cambic or vertic horizon, or a petrocalcic horizon in the substratum.

Distribution of Phaeozems (rough estimation supplied by soilgrids)

 

Reference soil ID037: Phaeozems

Subangular to angular blocky structure with shiny pedfaces.

 

Classification

WRB 2006 
Luvic- Phaeozem (Pachic Clayic) 
0-70 cmmollic horizon
30-150 cmargic horizon
 
0-70 cmmollic horizon
30-150 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Niti-Luvic PhaeozemLuvic Phaeozem
0-70 cmmollic A horizon
30-150 cmargic B horizon
-nitic
0-70 cmmollic A horizon
30-150 cmargillic B horizon

 

Local classification:Mediteran