Reference soil Belgium 04: Podzol

BE004

Podzols mainly occur in cool temperate and moist regions on coarse textured materials. Areas of Podzols have also been recorded from wet, tropical regions, notably the Amazon basin, southern central Africa and southeast Asia.

Characteristics

Soils having a spodic horizon (a dark coloured subsurface horizon with illuvial amorphous alumino-organic substances) within 200 cm from the soil surface, underlying an albic, histic, umbric or ochric horizon, or an anthropedogenic horizon less than 50 cm thick. Podzols are probably the most extensively researched group of soils.

Distribution of Podzols (rough estimation supplied by soilgrids)

 

Reference soil BE004: Podzols

REFERENCE: Mokma D.L. and P. Buurman. 1982. Podzols and podzolization in temperate regions. ISM Monograph 1. International Soil Museum, Wageningen. Profile B-101.

 

Classification

WRB 1998 
Haplic- Podzol 
0-13 cmochric horizon
13-23 cmalbic horizon
23-45 cmspodic horizon
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Haplic PodzolOrthic Podzol
0-13 cmochric A horizon
13-23 cmalbic E horizon
23-45 cmspodic B horizon