Reference soil Netherlands 10: Fluvisol

NL010

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 NL010: Fluvisol

LAND USE AND DRAINAGE: controlled polder water in ditches spaced 80-100m apart. The fields have a ridge-and-furrow system, spaced 10-15m. REFERENCE: "Soil excursion in the vicinity of Wageningen", soil B-NL10.

 

Classification

WRB 1998 
Humi-Gleyic- Fluvisol (Eutric) 
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
GleyiEutric FluvisolEutric Fluvisol

 

Local classification:Poldervaaggrond