Reference soil Brazil 29: Planosol

BR029

Planosols occur in level landscapes throughout the world often associated with broad river valleys.

Characteristics

Soils having an eluvial horizon, the lower boundary of which is marked. within 100 cm from the soil surface, by an abrupt textural change associated with stagnic properties above that boundary. The feature of albeluvic tonguing, however, is lacking.

Distribution of Planosols (rough estimation supplied by soilgrids)

Reference soil BR029: Planosols

Classification

WRB 2006WRB 1998
Umbric-Acric-Endogleyic- Planosol (Albic Ruptic Alumic)Umbri-Gleyic- Planosol (Albic Alumic)
0-35 cmumbric horizon
35-65 cmalbic horizon
65-143 cmargic horizon
-gleyic colour pattern
-lithological discontinuity
-abrupt textural change
0-35 cmumbric horizon
35-65 cmalbic horizon
65-143 cmargic horizon
-gleyic
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Albi-Umbric PlanosolHumic Planosol
0-35 cmumbric A horizon
35-65 cmalbic E horizon
65-143 cmargic B horizon
-abrupt textural change
-stagnic
0-35 cmumbric A horizon
35-65 cmalbic E horizon
65-143 cmargillic B horizon
-abrupt textural change
-hydromorphic

 

Local classification:Planossolo Tb álico a moderado textura média/argilosa fase floresta tropical subcaducifólia relvo plano