Reference soil Spain 06: Leptosol

ES006

Leptosols are by far the most extensive group of soils in the world. They are found mainly in mountainous regions and in areas where soil has been eroded to the extent that hard rock comes near to the surface. Other (minor) occurrences are along rivers where gravely deposits have accumulated without substantial admixture of fine earth material.

Characteristics

Soils which are either limited in depth by continuous hard rock within 25 cm from the soil surface, or overly mayerial with a calcium carbonate equivalent of more than 40 percent within 25 cm from the soil surface, or contain less than 10 percent (by weight) fine earth (mineral soil material with a diameter of 2 mm or less) to a depth of 75 cm from the soil surface. Leptosols have no diagnostic horizons other than a mollic, ochric, umbric, vertic or yermic horizon.

Distribution of Leptosols (rough estimation supplied by soilgrids)

 

Reference soil ES006: Leptosols

Short field description: A very shallow somewhat excessively drained yellowish-red gravelly sandy loam, underlain by weathered schistic rock. The structure is moderate very fine subangular blocky. There is lithic contact at 14 cm depth.

 

Classification

WRB 2014 
Leptosol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Calci-Eutric LeptosolEutric Cambisol lithic
- cmochric A horizon
-continuous hard rock
- cmochric A horizon
-lithic contact

 

Local classification:xeroranker