Reference soil Nicaragua 02: Phaeozem

NI002

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 NI002: Phaeozems

Formerly agricultural exploitation, mainly sorghum (verbal comm.). Now six years of secondary forest, dominant species: Lonchocarpus minimifloras (Chaperno), Acacia costaricensis (Cornizuelo), Stemnadenia spp. (Cachito). The B horizon has occasionally pockets of grey clay (10 YR 5/2). The CB horizon has pockets of light grey clay (10 YR 5/1). Short description: Moderately deep, well drained, very dark grey clay; roots penetrates easily the weathered rock C horizon, therefore effective soil depth > 80 cm

 

Classification

WRB 2006WRB 1998
Vertic-Endoleptic- Phaeozem (Clayic)Endoleptic- Phaeozem
0-40 cmmollic horizon
-vertic
0-40 cmmollic horizon
5-50 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Verti-Haplic PhaeozemHaplic Phaeozem
0-40 cmmollic A horizon
5-50 cmcambic B horizon
-vertic
0-40 cmmollic A horizon
5-50 cmcambic B horizon

 

Local classification:Chocolito