Reference soil Peru 01: Podzol

PE001

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 PE001: Podzols

Short field description Deep, excessively drained pale brown sand. At a depth of 115 cm starts a thick, mainly by organic matter, cemented hard, water stagnating layer, the Spodic horizon. Soil classification: samples of horizons 6 and 7 turn pale red upon ignition, indicating the presence of iron, and therefore excluding a Carbid Podzol classification. The site is situated in an erosion gully. 1) The soil is formed in the Iquitos formation, and consist, after the podzolisation process, of deep homogenous white quartz sands. 2) The original vegetation is a dense rain-forest, cleared for agriculture and abandonned as a forest fallow, locally known as "purma". " X " in the climate data refers to cloud cover in eights.

 

Classification

WRB 2006WRB 1998
Albic- PodzolHaplic- Podzol
108-167 cmspodic horizon
27-68 cmalbic horizon
0-27 cmochric horizon
108-167 cmspodic horizon
27-68 cmalbic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic PodzolOrthic Podzol
0-27 cmochric A horizon
101-186 cmspodic B horizon
- cmalbic E horizon
0-27 cmochric A horizon
108-167 cmspodic B horizon