Reference soil: Nicaragua 03

NI003

Distribution of Phaeozems (rough estimation supplied by soilgrids)

Very deep, (mod) well drained, yellowish brown clay; with a very dark brown topsoil, well rooted throughout At the limit Bt --> BC is a thin layer of rounded stones (not weathered resistent). It may be an indication of colluvium as parent material [micromorphology!]. The BC and CB horizons are charatcerized by whitish spots, the abundance increasing with depth. The cutans in the Bt have been described as patchy and broken, faint and distinct. Dry forest, major species: Quebrado ( ); Jinocuabo ( ) Espino negro ( ); Cornizuelo( ) The permeability of the soil is probably not sufficient to transmit the excess of rainwater. Run-off is a common feature, res ulting in natural gullies/dissecting streamlines throughout the landscape (high natural erosion).

Classification

 
WRB 2006 WRB 1998
Vertic Phaeozems (Clayic ) Haplic Phaeozem
0-43 cm mollic horizon 0-43 cm mollic horizon
43-102 cambic horizon 43-102 cm cambic horizon
  vertic horizon    
  FAO-UNESCO-ISRIC 1974
  Haplic Phaeozem
    0-43 cm mollic A horizon
    43-102 cm cambic B horizon
-   - argillic B horizon
    - ochric A horizon
Other classification
USDA-SCS (1975) Haplustalf clayey
Location: 

Department of Caraco, Biological Station Chacocente