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Cataula soil series

The Cataula series consists of very deep, moderately well drained soils formed in material weathered from metamorphic and igneous rocks of the Piedmont. They contain a layer that is dense and partially brittle. Permeability is slow. Slopes range from 2 to 25 percent.

 

TAXONOMIC CLASS: Fine, kaolinitic, thermic Oxyaquic Kanhapludults

 

Depth to the dense, partially brittle layer ranges from 15 to 40 inches. Depth to bedrock is more than 5 feet. The solum ranges from 40 to more than 60 inches thick. Content of rock fragments ranges from 0 to about 7 percent by volume. These consist of angular fragments of quartz often occurring as quartz stringers. The A horizon is very strongly acid to slightly acid, and all of the other horizons are very strongly acid to moderately acid.

 

Most areas had been cleared and used for growing cotton, corn, small grain, and pasture, but now about 75 percent of the total acreage is in shortleaf and loblolly pine.

 

These soils are moderately extensive in the Piedmont of South Carolina, Alabama and Georgia.

 

For a detailed description, visit:

soilseries.sc.egov.usda.gov/OSD_Docs/C/CATAULA.html

 

For acreage and geographic distribution, visit:

casoilresource.lawr.ucdavis.edu/see/#cataula

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Uploaded on December 21, 2010
Taken in December 2020