Reference soil Finland 05: Fluvisol

FI005

Fluvisols typically are young soils in alluvial, deltaic, lacustrine, or marine deposits, and occur all over the world.

Characteristics

Soils having fluvic soil material starting within 25 cm from the soil surface and continuing to a depth of at least 50 cm from the soil surface. They have no diagnostic horizons other than a histic, mollic, ochric, takyric, umbric, yermic, salic, or sulfuric horizon.

Distribution of Fluvisols (rough estimation supplied by soilgrids)

 

Reference soil FI005: Fluvisols

Land has been empoldered in 1958

 

Classification

WRB 2006WRB 1998
Gleyic- Fluvisol (Thionic Dystric Clayic)Gleyi-Orthithionic- Fluvisol
30-45 cmthionic horizon
-sulphidic
0-20 cmochric horizon
30-45 cmsulfuric horizon
-sulfidic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Gleyi-Thionic Fluvisol salicThionic Fluvisol saline
0-20 cmochric A horizon
30-45 cmsulfuric horizon
-sulfidic materials
0-20 cmochric A horizon
30-45 cmsulfuric horizon

 

Local classification:Recently reclaimed soil in silty marine deposits