Natchez silt loam
Encyclopedia
In 1988, the Professional Soil Classifiers Association of Mississippi selected Natchez silt loam soil to represent the soil resources of the State. These soils exist on 171,559 acres (0.56% of state) of landscape in Mississippi.

Mississippi state soil

The Natchez Silt Loam as the official state soil, designated by the Mississippi Legislature
Mississippi Legislature
The Mississippi Legislature is the state legislature of the U.S. state of Mississippi. The bicameral Legislature is composed of the lower Mississippi House of Representatives, with 122 members, and the upper Mississippi Senate, with 52 members. Both Representatives and Senators serve four-year...

 in 2003.

Description

The Natchez soils formed in very deep loess
Loess
Loess is an aeolian sediment formed by the accumulation of wind-blown silt, typically in the 20–50 micrometre size range, twenty percent or less clay and the balance equal parts sand and silt that are loosely cemented by calcium carbonate...

 material under a woodland environment and a climate that was warm and humid. These soils have natural fertility and desirable tilth
Tilth
Tilth can refer to two things:Tillage and a measure of the health of soil.Good tilth is a term referring to soil that has the proper structure and nutrients to grow healthy crops. Soil in good tilth is loamy, nutrient-rich soil that can also be said to be friable because optimal soil has a mixture...

 but usually occur on slopes that limit their use to trees. In areas where slopes are less, pasture
Pasture
Pasture is land used for grazing. Pasture lands in the narrow sense are enclosed tracts of farmland, grazed by domesticated livestock, such as horses, cattle, sheep or swine. The vegetation of tended pasture, forage, consists mainly of grasses, with an interspersion of legumes and other forbs...

 and row crops are grown and the soil is very productive when good management is applied.

A typical Natchez soil profile consists of a 3 inch top soil of dark grayish brown silt loam and to 8 inches, a subsurface of brown silt loam, a yellowish brown and dark yellowish brown silt loam subsoil to 36 inches and a substratum that is yellowish brown, and dark yellowish brown silt loam down to 80 inches.

Soil family classification

Classified as coarse-silty, mixed, superactive, thermic typic eutrudepts:

Natchez soils are in the Inceptisols soil order. Inceptisols soils have developed in relatively young material that have an Ochric epipedon is rich in weatherable minerals. The term coarse-silty indicates that the subsoil has less than 18 percent clay with less than 15 percent sand coarser than very fine. The term mixed suggests that no one mineral is over 60 percent. Thermic refers to an average annual soil temperature between 15 and 22 degrees Celsius (59 to 72 degrees Fahrenheit) and differs more than 5 degrees Celsius (9 °F) between winter and summer at 50 cm (20 inches) below the surface.

Natchez soils are on strongly sloping to very steep hillsides in the highly dissected parts of the bluff hills that border the Mississippi Delta floodplains. They formed in silty loess material that ranges from strongly acid to neutral in the upper part and neutral to slightly alkaline in lower parts. Average annual precipitation is 52 inches. Average annual air temperature is 63 °F (17 °C). The soil has developed in the upper Pleistocene age material.

Sources

  • This article utilizes text taken verbatim from Natchez Silt Loam- Mississippi State Soil, a public domain
    Public domain
    Works are in the public domain if the intellectual property rights have expired, if the intellectual property rights are forfeited, or if they are not covered by intellectual property rights at all...

     publication of the United States Department of Agriculture
    United States Department of Agriculture
    The United States Department of Agriculture is the United States federal executive department responsible for developing and executing U.S. federal government policy on farming, agriculture, and food...

    .
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