Reference soil Finland 01: Gleysol

FI001

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 FI001: Gleysols

Classification

WRB 2006WRB 1998
Haplic- Gleysol (Hypereutric Clayic)Hapli-Hypereutric- Gleysol
15-55 cmcambic horizon
-reducing conditions
-gleyic colour pattern
0-15 cmochric horizon
15-55 cmcambic horizon
-gleyic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Eutric GleysolEutric Gleysol
0-15 cmochric A horizon
15-55 cmcambic B horizon
-gleyic
0-15 cmochric A horizon
15-55 cmcambic B horizon
-hydromorphic

 

Local classification:Heavy clay soil