Reference soil Cuba 1 Vertisol
CU001
Distribution of Vertisols (rough estimation supplied by soilgrids)
Deep, poorly to imperfectly drained, grayish brown clay. The subsoil is strongly mottled, a wedge-shaped angular blocky structure and slickensides. Water table is present during the rainy season at a depth of about 50 to 100 cm (verbal communications). Geology: Quaternary Era, Pleistocene; Guevarra Formation: Clays and sandy clay. Geomorphology: marine plain and terrace, abrasive and accumulative abrasive, slightly ondulating. The poor drainage is somewhat compensated by the cultivation of sugarcane on machine prepared large ridges with a height of 40 to 50 cm
WRB 2006 | WRB 1998 | ||
---|---|---|---|
Gleyic Vertisols (Hyposodic Chromic ) | Chromic Hyposodi Vertisols | ||
18-45 cm | cambic horizon | 18-45 cm | cambic horizon |
- | gleyic colour pattern horizon | 105-200 cm | ferric horizon |
- | reducing conditions horizon | 0-18 cm | ochric horizon |
45-200 | vertic horizon | - | gleyic horizon |
105-200 | ferric horizon | 45-200 cm | vertic horizon |
FAO-UNESCO-ISRIC 1974 | |||
Chromic Vertisols phreatic |
|||
- | hydromorphic horizon | ||
- | slickensides horizon | ||
0-18 cm | ochric A horizon | ||
18-45 cm | cambic B horizon |
Local classification
Classification information | Gley Ferralítico Típico |
Other classification
USDA-NRCS (1999) | Ustic Endoaquert |
USDA-SCS (1975) | Ustic Tropaquept aquic clayey montmorillonitic isohyperthermic |
Location:
Provincia Habana, Municipio Melena del Sur, CAI "Gregorio Arlee Mañalich", Bloque 41, Campo 4006