Reference soil Netherlands 19: Fluvisol

NL019

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 NL019: Fluvisols

An imperfectly drained soil, derived from holocene river sediments, situated on a flood plain with "escarpment" (about 2m) to river bed. The site is an eroded river bank that is flooded in winter, connected with deposition of sandy-clayey material. Therefore, the profile is a mixture of changing sandy and clayey sedimentary layers. The C2 is coloured 10 YR 5/3 (sand and 10 YR 4/2 (clay); the C4 10 YR 6/3 (sand) and 10 YR 4/2 (clay). (authors: Breimer/van Reuler/Van Kekem//de Sitter)

 

Classification

WRB 1998 
Calcaric- Fluvisol 
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Calcaric FluvisolCalcaric Fluvisol

 

Local classification:Poldervaaggrond