Reference soil Peru 06: Acrisol

PE006
Distribution of Acrisols (rough estimation supplied by soilgrids)

 

Reference soil PE006: Acrisol

Short field description A very deep, well drained, brown clay. The topsoil has a loamy texture. The soil site is located in an old alluvium plain, not any more flooded ('Tierra Firme'), with a nearly level to gently undulating relief. In the surrounding area at a distance of about 5 km starts a dissected higher hilly area. The site is comparable to soil profile Yurimaguas 17 in the thesis " Genesis of the soils within a detailed soil survey area in the upper Amazon basin, Yurimaguas, Peru" by E.J. Tyler (North Carolineat Raleigh, 1975). Many experiments of the Tropsoils programme (P.Sanchez) are realized on this soil type. Slight sheet erosion is manifest. The textural increase is sufficient for the recognition of an argic B horizon in FAO (1988) classification system and classifies as Haplic Acrisol. However, because no cutans were observed in the field no argillic horizon can be recognized in FAO (1974) and therefore the soil is classified as Ferralic Cambisol. A similar remark can be made for the USDA classification: if no clay skins are detected in thin sections, the soil is classified as Oxic Dystropept.

 

Classification

WRB 2006WRB 1998
Haplic- Acrisol (Alumic Chromic)Chromi-Alumic- Acrisol
8-114 cmargic horizon
0-8 cmochric horizon
8-114 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
AlumiHaplic AcrisolOrthic Acrisol
0-8 cmochric A horizon
8-114 cmargic B horizon
- cmochric A horizon
0-8 cmochric A horizon
8-114 cmargillic B horizon

 

Local classification:Suelo Yurimaguas