Reference soil Peru 21: Fluvisol

PE021

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 PE021: Fluvisols

Short field description A very deep, well drained, dark brown loam to sandy loam. Soil profile located in a recent fluvial deposit (low terrace). Soil profile development is in its initial stage and the incipient structure is partly due to parent material.

 

Classification

WRB 2006WRB 1998
Haplic- Fluvisol (Calcaric Sodic)Sodi-Calcaric- Fluvisol
-fluvic
-calcaric
0-53 cmochric horizon
-calcaric
-fluvic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Sodi-Calcaric FluvisolCalcaric Fluvisol sodic
0-53 cmochric A horizon
- cmochric A horizon
-fluvic
-sodic
0-53 cmochric A horizon

 

Local classification:Suelo Moquegua