Reference soil: Nicaragua 03
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 |
USDA-SCS (1975) | Haplustalf clayey |
Department of Caraco, Biological Station Chacocente