Reference soil Uruguay 09: Planosol

UY009

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 UY009: Planosols

Duran, A. (1973) Caracterizacion y genesis de algunas Praderas Arenosas de Tacuarembo y Rivera. Ministerio de Ganaderia y Agricultura. Direccion de Suelos y Fertilizantes. Montevideo, Uruguay. Technical Bulletin No. 2. (profile with name 25-24)

 

Classification

WRB 2006WRB 1998
Umbric-Alic- Planosol (Alumic)Profondi-Endostagnic- Luvisol (Hyperdystric)
0-53 cmumbric horizon
53-160 cmargic horizon
-stagnic colour pattern
-reducing conditions
0-53 cmumbric horizon
53-160 cmargic horizon
-stagnic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Umbri-Stagnic AlisolHumic Acrisol
0-53 cmumbric A horizon
53-160 cmargic B horizon
-stagnic
0-53 cmumbric A horizon
53-160 cmargillic B horizon
-ferric
-hydromorphic

 

Local classification:Luvisol ocrico abrúptico Ar, hm