6.4 - Soil Orders

Soil properties can vary greatly from one location to the next, even within distances of a few meters. These same soil properties can also exhibit similar characteristics over broad regional areas of like climate and vegetation.

The most general level of classification in the USDA system of Soil Taxonomy is the Soil Order. All of the soils in the world can be assigned to one of 12 orders. By surveying soil properties of color, texture, and structure; thickness of horizons; parent materials; drainage characteristics; and landscape position, soil scientists have mapped and classified nearly the entire contiguous United States and much of the rest of the world.

Use Table 6.1 (below) for a brief overview of Soil Orders, or go to Lesson 5, where Soil Orders are described in detail.

Table 6.1 - Soil Orders and General Descriptions

Type Description  Type Description
Entisols Little, if any horizon development Inceptisols Beginning of horizon development
Aridisols Soils located in arid climates Mollisols Soft, grassland soils
Alfisols Deciduous forest soils Spodosols Acidic, coniferous forest soils
Ultisols Extensively weathered soils Oxisols Extremely weathered, tropical soils
Gelisols Soils containing permafrost Histosols Soils formed in organic material
Andisols Soil formed in volcanic material Vertisols Shrinking and swelling clay soils

Global Soil Regions Key and Map. Image courtesy of the USDA-NRCS, edited by UNL.

The nature and properties of soils can vary widely from one location to the next, even within distances of a few meters. These same soil properties can also be found to exhibit similar characteristics over broad regional areas of like climate and vegetation. The soil forming factors of parent material, climate, vegetation (biota), topography, and time (Lesson 3.2) tend to produce a soil that describes the environment in which it is formed. By surveying properties of soil color, texture, and structure; thickness of horizons; parent materials; drainage characteristics; and landscape position, soil scientists have mapped and classified nearly the entire contiguous   United States and much of the rest of the world.

Global Soil Regions-Orders Key and Map. Image courtesy of the USDA-NRCS, edited by UNL.

For descriptions of the 12 Soil orders, see Lesson 5.2

Table 6.2 Percent of World Ice-free Land Area of Each Soil Order.

Soil Order

 

Estimated % of World Land Area

Approximate Area (million km2) Soil Order

Estimated % of World Land Area

Approximate Area (million km2)
 Entisols 16 21.0  Inceptisols  17  22.3
 Aridisols 12 15.7  Mollisols  7  9.2
 Alfisols 10  13.1   Spodosols  4  5.2
 Ultisols 8 10.5  Oxisols  8  10.5
 Gelisols 9 11.8  Histosols  1  1.3
 Andisols 1.3   Vertisols  2  2.6
 Other 5 6.6 Total 100 131

Quiz

Question

Although considered some of the most naturally fertile and productive soils, Mollisols constitute what percent of total world ice-free land area?

Looks Good! Correct: Mollisol soils occur on less than 10% of the total ice-free land area.
Question

Entisol and Aridisol soils are commonly found together in arid desert regions. How much of the global ice-free land area is covered by these two soil orders combined?

Looks Good! Correct: Correct! Over one-third of the global ice-free land area is classified in these two commonly associated soil orders.
Question

Looking at the soil orders maps, which continental area appears to have the greatest single expanse of combined Entisol-Aridisol soils?

Looks Good! Correct: The Sahara Desert is a land area equal to the size of the continental United States and is classified as mainly Entisol and Aridisol soils.
Question

Use the soil orders maps above to locate regions of Mollisol soils. At what latitudes in the world do Mollisol soils tend to exist to the greatest extent?

Looks Good! Correct: Mollisol is found frequently in semi-arid, mountain steppe regions of the middle latitudes.