Ultisols
Encyclopedia
Ultisols, commonly known as red clay soils, are one of twelve soil orders in the United States Department of Agriculture soil taxonomy
. They are defined as mineral soils which contain no calcareous
material anywhere within the soil, have less than 10% weatherable minerals in the extreme top layer of soil, and have less than 35% base
saturation throughout the soil. Ultisols occur in humid temperate or tropical regions. While the term is usually applied to the red clay soils of the Southern United States
, Ultisols are also found in regions of Africa
, Asia
, and South America
. In the World Reference Base for Soil Resources
system, most Ultisols are known as Acrisol
s. Others are classed as Lixisols or Nitosols.
The word "Ultisol" is derived from "ultimate", because Ultisols were seen as the ultimate product of continuous weathering
of minerals in a humid, temperate climate without new soil formation via glaciation.
Ultisols vary in color from purplish-red, to a blindingly bright reddish-orange, to pale yellowish-orange and even some subdued yellowish-brown tones. They are typically quite acid
ic, often having a pH
of less than 5. The red and yellow colors result from the accumulation of iron oxide
(rust) which is highly insoluble in water. Major nutrients, such as calcium
and potassium
, are typically deficient in Ultisols, which means they generally cannot be used for sedentary agriculture without the aid of lime
and other fertilizer
s, such as superphosphate. They can be easily exhausted, and require more careful management than Alfisols
or Mollisols
. However, they can be cultivated over a relatively wide range of moisture conditions.
Ultisols can have a variety of clay minerals, but in many cases the dominant mineral is kaolinite
. This clay has good bearing capacity
and no shrink-swell property
. Consequently, well-drained kaolinitic Ultisols such as the Cecil
series are suitable for urban development.
Ultisols are the dominant soils in the American South (where the Cecil series is most famous), southeastern China
, Southeast Asia
and some other subtropical and tropical areas. Their northern limit (except fossil
soils) is very sharply defined in North America
by the limits of maximum glaciation during the Pleistocene
, because Ultisols typically take hundreds of thousands of years to form - far longer than the length of an interglacial
period today.
The oldest fossil Ultisols are known from the Carboniferous
period when forests first developed. Though known from far north of their present range as recently as the Miocene
, Ultisols are surprisingly rare as fossils overall, since they would have been expected to be very common in the warm Mesozoic
and Tertiary
paleoclimates.
USDA soil taxonomy
USDA Soil Taxonomy developed by United States Department of Agriculture and the National Cooperative Soil Survey provides an elaborate classification of soil types according to several parameters and in several levels: Order, Suborder, Great Group, Subgroup, Family, and Series.- Example of...
. They are defined as mineral soils which contain no calcareous
Calcareous
Calcareous is an adjective meaning mostly or partly composed of calcium carbonate, in other words, containing lime or being chalky. The term is used in a wide variety of scientific disciplines.-In zoology:...
material anywhere within the soil, have less than 10% weatherable minerals in the extreme top layer of soil, and have less than 35% base
Base (chemistry)
For the term in genetics, see base A base in chemistry is a substance that can accept hydrogen ions or more generally, donate electron pairs. A soluble base is referred to as an alkali if it contains and releases hydroxide ions quantitatively...
saturation throughout the soil. Ultisols occur in humid temperate or tropical regions. While the term is usually applied to the red clay soils of the Southern United States
Southern United States
The Southern United States—commonly referred to as the American South, Dixie, or simply the South—constitutes a large distinctive area in the southeastern and south-central United States...
, Ultisols are also found in regions of Africa
Africa
Africa is the world's second largest and second most populous continent, after Asia. At about 30.2 million km² including adjacent islands, it covers 6% of the Earth's total surface area and 20.4% of the total land area...
, Asia
Asia
Asia is the world's largest and most populous continent, located primarily in the eastern and northern hemispheres. It covers 8.7% of the Earth's total surface area and with approximately 3.879 billion people, it hosts 60% of the world's current human population...
, and South America
South America
South America is a continent situated in the Western Hemisphere, mostly in the Southern Hemisphere, with a relatively small portion in the Northern Hemisphere. The continent is also considered a subcontinent of the Americas. It is bordered on the west by the Pacific Ocean and on the north and east...
. In the World Reference Base for Soil Resources
World Reference Base for Soil Resources
The World Reference Base for Soil Resources is the international standard taxonomic soil classification system endorsed by the International Union of Soil Sciences . It was developed by an international collaboration coordinated by the International Soil Reference and Information Centre and...
system, most Ultisols are known as Acrisol
Acrisol
An acrisol is a type of soil as classified by the Food and Agriculture Organization. It is clay-rich, and is associated with humid, tropical climates, such as those found in Brazil, and often supports forested areas. It is one of the 30 major soil groups of the World Reference Base for Soil Resources...
s. Others are classed as Lixisols or Nitosols.
The word "Ultisol" is derived from "ultimate", because Ultisols were seen as the ultimate product of continuous weathering
Weathering
Weathering is the breaking down of rocks, soils and minerals as well as artificial materials through contact with the Earth's atmosphere, biota and waters...
of minerals in a humid, temperate climate without new soil formation via glaciation.
Ultisols vary in color from purplish-red, to a blindingly bright reddish-orange, to pale yellowish-orange and even some subdued yellowish-brown tones. They are typically quite acid
Acid
An acid is a substance which reacts with a base. Commonly, acids can be identified as tasting sour, reacting with metals such as calcium, and bases like sodium carbonate. Aqueous acids have a pH of less than 7, where an acid of lower pH is typically stronger, and turn blue litmus paper red...
ic, often having a pH
Soil pH
The soil pH is a measure of the acidity or basicity in soils. pH is defined as the negative logarithm of the activity of hydrogen ions in solution. It ranges from 0 to 14, with 7 being neutral. A pH below 7 is acidic and above 7 is basic. Soil pH is considered a master variable in soils as it...
of less than 5. The red and yellow colors result from the accumulation of iron oxide
Iron oxide
Iron oxides are chemical compounds composed of iron and oxygen. All together, there are sixteen known iron oxides and oxyhydroxides.Iron oxides and oxide-hydroxides are widespread in nature, play an important role in many geological and biological processes, and are widely utilized by humans, e.g.,...
(rust) which is highly insoluble in water. Major nutrients, such as calcium
Calcium
Calcium is the chemical element with the symbol Ca and atomic number 20. It has an atomic mass of 40.078 amu. Calcium is a soft gray alkaline earth metal, and is the fifth-most-abundant element by mass in the Earth's crust...
and potassium
Potassium
Potassium is the chemical element with the symbol K and atomic number 19. Elemental potassium is a soft silvery-white alkali metal that oxidizes rapidly in air and is very reactive with water, generating sufficient heat to ignite the hydrogen emitted in the reaction.Potassium and sodium are...
, are typically deficient in Ultisols, which means they generally cannot be used for sedentary agriculture without the aid of lime
Agricultural lime
Agricultural lime, also called aglime, agricultural limestone, garden lime or liming, is a soil additive made from pulverized limestone or chalk. The primary active component is calcium carbonate...
and other fertilizer
Fertilizer
Fertilizer is any organic or inorganic material of natural or synthetic origin that is added to a soil to supply one or more plant nutrients essential to the growth of plants. A recent assessment found that about 40 to 60% of crop yields are attributable to commercial fertilizer use...
s, such as superphosphate. They can be easily exhausted, and require more careful management than Alfisols
Alfisols
Alfisols are a soil order in USDA soil taxonomy. Alfisols form in semiarid to humid areas, typically under a hardwood forest cover. They have a clay-enriched subsoil and relatively high native fertility. "Alf" refers to aluminium and iron . Because of their productivity and abundance, the...
or Mollisols
Mollisols
Mollisols are a soil order in USDA soil taxonomy. Mollisols form in semi-arid to semi-humid areas, typically under a grassland cover. They are most commonly found in the mid-latitudes, namely in North America, mostly east of the Rocky Mountains, in South America in Argentina and Brazil, and in...
. However, they can be cultivated over a relatively wide range of moisture conditions.
Ultisols can have a variety of clay minerals, but in many cases the dominant mineral is kaolinite
Kaolinite
Kaolinite is a clay mineral, part of the group of industrial minerals, with the chemical composition Al2Si2O54. It is a layered silicate mineral, with one tetrahedral sheet linked through oxygen atoms to one octahedral sheet of alumina octahedra...
. This clay has good bearing capacity
Bearing capacity
In geotechnical engineering, bearing capacity is the capacity of soil to support the loads applied to the ground. The bearing capacity of soil is the maximum average contact pressure between the foundation and the soil which should not produce shear failure in the soil...
and no shrink-swell property
Shrink-swell capacity
The Shrink-swell capacity of clay refers to the extent to which a clay will expand when wet and retract when dry. Soil that is problematic due to high capacity is known as shrink-swell soil, or expansive soil.-Description:...
. Consequently, well-drained kaolinitic Ultisols such as the Cecil
Cecil (soil)
]Originally mapped in Cecil County, Maryland in 1899, more than 10 million acres of the Cecil soil series are now mapped in the Piedmont region of the southeastern United States...
series are suitable for urban development.
Ultisols are the dominant soils in the American South (where the Cecil series is most famous), southeastern China
China
Chinese civilization may refer to:* China for more general discussion of the country.* Chinese culture* Greater China, the transnational community of ethnic Chinese.* History of China* Sinosphere, the area historically affected by Chinese culture...
, Southeast Asia
Southeast Asia
Southeast Asia, South-East Asia, South East Asia or Southeastern Asia is a subregion of Asia, consisting of the countries that are geographically south of China, east of India, west of New Guinea and north of Australia. The region lies on the intersection of geological plates, with heavy seismic...
and some other subtropical and tropical areas. Their northern limit (except fossil
Fossil
Fossils are the preserved remains or traces of animals , plants, and other organisms from the remote past...
soils) is very sharply defined in North America
North America
North America is a continent wholly within the Northern Hemisphere and almost wholly within the Western Hemisphere. It is also considered a northern subcontinent of the Americas...
by the limits of maximum glaciation during the Pleistocene
Pleistocene
The Pleistocene is the epoch from 2,588,000 to 11,700 years BP that spans the world's recent period of repeated glaciations. The name pleistocene is derived from the Greek and ....
, because Ultisols typically take hundreds of thousands of years to form - far longer than the length of an interglacial
Interglacial
An Interglacial period is a geological interval of warmer global average temperature lasting thousands of years that separates consecutive glacial periods within an ice age...
period today.
The oldest fossil Ultisols are known from the Carboniferous
Carboniferous
The Carboniferous is a geologic period and system that extends from the end of the Devonian Period, about 359.2 ± 2.5 Mya , to the beginning of the Permian Period, about 299.0 ± 0.8 Mya . The name is derived from the Latin word for coal, carbo. Carboniferous means "coal-bearing"...
period when forests first developed. Though known from far north of their present range as recently as the Miocene
Miocene
The Miocene is a geological epoch of the Neogene Period and extends from about . The Miocene was named by Sir Charles Lyell. Its name comes from the Greek words and and means "less recent" because it has 18% fewer modern sea invertebrates than the Pliocene. The Miocene follows the Oligocene...
, Ultisols are surprisingly rare as fossils overall, since they would have been expected to be very common in the warm Mesozoic
Mesozoic
The Mesozoic era is an interval of geological time from about 250 million years ago to about 65 million years ago. It is often referred to as the age of reptiles because reptiles, namely dinosaurs, were the dominant terrestrial and marine vertebrates of the time...
and Tertiary
Tertiary
The Tertiary is a deprecated term for a geologic period 65 million to 2.6 million years ago. The Tertiary covered the time span between the superseded Secondary period and the Quaternary...
paleoclimates.
Suborders
- Aquults - Ultisols with a water table at or near the surface for much of the year
- Humults - well-drained Ultisols that have high organic matter content
- Udults - Ultisols of humid climates
- Ustults - Ultisols of semiarid and subhumid climates
- Xerults - temperate Ultisols with very dry summers and moist winters