Reference soil France 10: Podzol

FR010

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 FR010: Podzols

PARENT MATERIAL: Sand is locally alternated by clays. Geology: Upper(Bartonian) and middle(Lutetian) Eocene. VEGETATION AND LAND USE: coverage(%) trees 70 herbs & grasses 95 ADDITIONAL NOTES ON PROFILE DESCRIPTION: Bh - streaks of dark reddish brown (5YR3/3) sand. Bs - inclusions: consist of somewhat lighter coloured, coherent sand. 2C1 - color: also 10YR7/3. 2C2 - color: also 5YR5/8. - mottled and horizontally streaked. - with pockets of sandy clay. 3C - yellow, coherent sand.

 

Classification

WRB 2006WRB 1998
Albic- Podzol (Ruptic)Haplic- Podzol
16-39 cmalbic horizon
39-67 cmspodic horizon
-lithological discontinuity
1-16 cmochric horizon
16-39 cmalbic horizon
39-67 cmspodic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic PodzolOrthic Podzol
1-16 cmochric A horizon
16-39 cmalbic E horizon
39-67 cmspodic B horizon
1-16 cmochric A horizon
16-39 cmalbic E horizon
39-67 cmspodic B horizon

 

Local classification:Podzol humo-ferrique