Soil great group

Palexeralf

Of the Xeralf suborder; it is very old and evolved: very thick clay horizon, or a petrocalcic horizon (calcareous hardpan) indicating a long time of formation.

What the name says

Soil Taxonomy names are built from parts, and each part says something about the soil. From general to specific:

Taxonomic orderAlfisolSoil with a clay accumulation horizon (argillic or natric) and good base saturation, but without the thick, dark surface of a Molisol.
SuborderXeralfAlfisol with a Mediterranean climate (xeric moisture regime).
Great groupPalexeralfWithin the Xeralf suborder, it is very old and evolved: very thick clay horizon, or a petrocalcic horizon (calcareous hardpan) indicating a long time of formation.

What it means for farming

Acceptable fertility, but the surface layer is thinner and poor in organic matter. In the Pampas region many Alfisoles are sodic or floodable (Natracualfes) and are left for livestock.

Most common surface texture
Sandy loam
Most common drainage
Moderate
Typical effective depth
140 cm

Where it is found

According to the 1:500.000 national map, it covers about 10.750 ha, spread over 1 districts.

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National map units that list it. The scale is 1:500.000: good for seeing the region, not a single property.

ProvinceArea
Neuquén10.750 ha

Districts where it is most common

Subgroups on the maps

  • Palexeralf mólico

The definitions are a plain-language summary of the USDA Keys to Soil Taxonomy. The formal definition includes thickness, color and percentage thresholds that are left out here.

Sources