The soil formed in residuum from cherty limestone, interbedded with small amounts of sandstone, siltstone, and shale. The mean annual temperature is about 60 to 65 degrees F, and the mean annual precipitation is about 45 to 55 inches.

The Clarksville series consists of very deep, somewhat excessively drained soils formed in hillslope sediments and the underlying clayey residuum from cherty dolomite or cherty limestone on steep side slopes and narrow ridgetops. Slopes range from 1 to 70 percent. Mean annual precipitation is 43 inches, and mean annual temperature is 55 degrees F.

Depth to Seasonal High Water Table: more than 180 cm (6 feet). SERIES ESTABLISHED: Cherokee County, Alabama, 1924. This edit adopts the semitabular format, updates the typical pedon location, range in characteristics (BE and BA horizons), geographic setting, competing series (editorial change), and associated soils.

2004年10月9日 · cherty silt loam surface layer and a cherty silt loam to a cherty silty clay loam subsoil. These soils occur on slopes ranging from 35 to 60 percent. The site class for loblolly pine is 70. These soils have severe management problems for erosion hazards and equipment limitations while seedling mortality is moderate.

Aggregate lab data for the FULLERTON soil series. This aggregation is based on all pedons with a current taxon name of FULLERTON, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles.

2004年11月13日 · Cedargap soils are formed from silty alluvium that has a high content of chert fragments and occur on bottom land in stream valleys. The surface water runoff class is very low and the natural drainage condition of the soil is somewhat excessively drained. The slowest permeability is moderately rapid.

2017年1月30日 · Soil hydraulic properties at eight depths in a Fullerton cherty silt loam (a clayey, kaolinitic, thermic Typic Paleudult) profile were derived from measurements of water content with a calibrated neutron probe and of matric potential with tensiometers during drainage of a flooded 2- by 2- by 3-m deep soil plot.

The Dellrose series consists of very deep, well drained soils that formed in medium textured, cherty colluvium on foot slopes and steep hillsides. These soils have moderately rapid permeability. Slopes range from 2 to 60 percent. Near the type location, mean annual temperature is 58.5 degrees F. and mean annual precipitation is 52.9 inches.

These soils formed in colluvium or residuum weathered from cherty limestone. They are on sharply dissected uplands. Slopes range from 5 to 70 percent. TAXONOMIC CLASS: Loamy-skeletal, siliceous, semiactive, thermic Typic Paleudults. TYPICAL PEDON: Bodine gravelly silt loam -- hardwood and second growth pine.

The Stemley series consists of deep, moderately well drained, slowly permeable soils that formed in loamy cherty limestone. These soils are on nearly level to strongly sloping toeslopes and sideslopes near drainageways.