Reference soil Uruguay 04: Regosol

UY004

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 UY004: Regosols

DRAINAGE PATTERN: coarse dendrite DOMINANT SPECIES: trachypogon montufari, paspalum notatum, andropogon ternatus, richardia humistrata, cyperus spp., axonopus affinis, axonopus argentinus spp. MORPHOLOGY: C Weathered rock, banded with alterated black minerals on the surface of which clay (10YR6/3) is found (unlcear whether the clay is formed in situ or illuviated). Probably biotite is alterated to vermiculite. Colours (dry) also 7.5YR5/8 and 10YR7/6

 

Classification

WRB 2006WRB 1998
Epileptic- Regosol (Humic Eutric)Humi-Epileptic- Regosol (Eutric)
-continuous rock
0-28 cmochric horizon
-continuous hard rock
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Dystric Regosol lithicDystric Regosol lithic
0-28 cmochric A horizon
-continuous hard rock
0-28 cmochric A horizon

 

Local classification:Brunosol subéutrico háplico