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