Reference soil Brazil 28: Gleysol-old

BR028

Gleysols occur throughout the world where groundwater comes near to the surface, causing soils to become wet for a prolonged part of the year. They are particularly abundant in the low-lying river basins.

Characteristics

Soils having gleyic properties (properties associated with prolonged wetness) within 50 cm from the soil surface. They have no diagnostic horizons other than an anthraquic, histic, mollic, ochric, takyric, or umbric horizon at the surface, or an andic, calcic, cambic, gypsic, plinthic, salic, sulfuric, or vitric horizon within 100 cm from the soil surface.

Distribution of Gleysols (rough estimation supplied by soilgrids)

 

Reference soil BR028: Gleysols

Very deep, imperfectly drained silty loam with a thin dark grey topsoil and a strongly mottled subsoil. Effective soil depth depends on fluctuating water table, determined by water level of the river. Porosity and permeability of whole soil profile is very high. Deep augering shows different strata due to variation in mottling. The profile show some river-sedimemtation strtification. The soil classifies as Gleysol bordering to Fluvisol. Brazilian classification: Plintossolo Eutrofico Tbtextura media. Slides no 9904-9909.

 

Classification

WRB 2006WRB 1998
Fluvic- Gleysol (Eutric)Eutric- Gleysol
10-135 cmcambic horizon
-fluvic
-gleyic colour pattern
-reducing conditions
0-22 cmochric horizon
22-135 cmcambic horizon
-fluvic
-gleyic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Eutric GleysolEutric Gleysol cerrado
0-22 cmochric A horizon
22-135 cmcambic B horizon
- cmumbric A horizon
-gleyic
0-22 cmochric A horizon
22-135 cmcambic B horizon
-hydromorphic

 

Local classification:Plintossolo eutrófico Tb textura media