Reference soil Belgium 02: Albeluvisol

BE002

Albeluvisols occur mainly in the moist and cool temperate regions (dominantly regions with a cool continental climate), particularly in Eastern Europe and central USA/Canada.

Characteristics

Soils having an argic horizon (a subsurface horizon with distinct higher clay content than the overlying horizon) within 100 cm from the soil surface. The argic horizon has an irregular upper boundary resulting from "albeluvic tonguing".

Distribution of Albeluvisols (rough estimation supplied by soilgrids)

 

Reference soil BE002: Albeluvisols

REFERENCE: Mitteilungen de Deutschen Bodenkundlichen Gesellschaft, Band 3, Göttingen 1965, pp. 105-107 (profile 9)

 

Classification

WRB 2006WRB 1998
Stagnic-Gleyic-Fragic- Albeluvisol (Ruptic Hyperdystric Siltic)Fragi-Gleyic- Albeluvisol (Siltic Hyperdystric)
20-43 cmalbic horizon
43-106 cmargic horizon
59-106 cmfragic horizon
-reducing conditions
-albeluvic tonguing
-gleyic colour pattern
0-20 cmochric horizon
20-43 cmalbic horizon
43-106 cmargic horizon
53-106 cmfragic horizon
-gleyic
-albeluvic tonguing
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Dystri-Gleyic Podzoluvisol fragipanDystric Podzoluvisol fragipan
0-12 cmochric A horizon
20-43 cmalbic E horizon
43-106 cmargic B horizon
-gleyic
-tonguing
0-20 cmochric A horizon
20-43 cmalbic E horizon
43-106 cmargillic B horizon
-hydromorphic
-tonguing

 

Local classification:Sol lessivé très fortement gleyifié