Reference soil Finland 06: Gleysol

FI006

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)

WRB 2006:

WRB 1998:

Fluvic Gleysol(Epidystric Siltic)
Epidystric Gleysol
  gleyic colour pattern
  reducing conditions
  fluvic material
0-20 cm ochric horizon
  fluvic soil material
  gleyic properties

FAO-UNESCO-ISRIC 1988:

FAO-UNESCO 1974:

Silti- Dystric Gleysol
Dystric Gleysol
0-20 cm ochric A horizon
  gleyic properties
0-20 cm ochric A horizon
  hydromorphic properties

Other classification

USDA-NRCS (1999)

Endoaquent

USDA-SCS (1975)

Haplaquent fine-silty mixed frigid
Location: 

20km E of Tampere near Kangasala