Reference soil Peru 19: Regosol

PE019

Regosols are found in areas where soil has been eroded to the extent that the underlying unconsolidated materials come near to the surface, or where soil formation has not played an important role, e.g. in desert regions. The name comes from the greek 'rhegos' :blanket meaning young soils on weathering materials.

Characteristics

Soils in medium and fine textured materials, having no distinctive horizons other than an ochric horizon at the surface.

Distribution of Regosols (rough estimation supplied by soilgrids)

 

Reference soil PE019: Regosols

Short field description A deep, well drained, dark brown sandy loam to loamy sand. On the transition from fifth to sixth horizon is a sandy lens with a ligth gray color. Bulk density is too high for Andisols, andic subgroup possible. The soil profile located in a fan of volcanic material. The land has been shaped by man, constructing terraces which have been cultivated for about 100 years. " X " in the climate data refers to the cloud in eighths.

 

Classification

WRB 2006WRB 1998
Haplic- Regosol (Calcaric Tephric Humic)Hyposodi-Humic- Regosol (Calcaric Tephric)
-tephric
-calcaric
0-59 cmochric horizon
-tephric
-calcaric
-strongly humic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Calcaric RegosolVitric Andosol
0-59 cmochric A horizon
- cmmollic A horizon
-strongly humic
0-36 cmochric A horizon