Reference soil Brazil 19: Podzol
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.
Reference soil BR019: Podzols
Deep, moderately well drained sandy soil derived from Tertiary sediments; having a strongly cemented impermeable iron layer in the deeper subsoil. Brazilian classification: Podzol com duripan or Podzol hidromorfico. *Geomorphology: dissected plain ("Tabuleiro") developed in Tertiary sediments of the "Barreiras" group. The genesis of these sediments is not yet understood. Lateral groundwater flow over impermeable iron pan. Seepage zones on lower slope. Imperfectly to moderately well Drained. Major crops: roots like 'inhame' (Dioscoreaceae), cassava, sweet potato. Additional information: Boletim Tecnico no 35 (ISRIC-library), slides 9821-9826. Classification: the iron & duripan is situated at a depth than 100cm, it therefore does not classify as Placorthord or Durorthod.