Mollisol

Mollisol
A Mollisol profile
Used in	USDA soil taxonomy
Parent material	Loess, Limestone
Climate	Humid continental, semi-arid

Mollisol is a

), typically between 60 and 80 cm in depth. This fertile surface horizon, called a mollic epipedon, is the defining diagnostic feature of Mollisols. Mollic epipedons are created by long-term addition of organic materials derived from plant roots and typically have soft, granular soil structure.

Mollisols typically occur in savannahs and mountain valleys (such as Central Asia, and the North American

due to the fertility of the horizon). Globally, they represent ~7% of ice-free land area. As the world's agriculturally most productive soil order, the Mollisols represent one of the most economically important soil orders.

Though most other soil orders known today were formed at the beginning of the Carboniferous Ice Age 280 million years ago, Mollisols are best known from the paleopedological record as early as the Eocene. Their development is very closely associated with cooling and drying of the global climate that occurred during the Oligocene, Miocene and Pliocene.

Suborders

Albolls—wet soils; aquic soil moisture regime with an

eluvial horizon

Aquolls—wet soils; aquic soil moisture regime

Cryolls—cold climate; frigid or cryic soil temperature regime

Gelolls—very cold climate; mean annual soil temperature < 0 °C

Rendolls—lime parent material

Udolls—humid climate; udic moisture regime

Ustolls—subhumid climate; ustic moisture regime

Xerolls—Mediterranean climate; xeric moisture regime

Soils which are mostly similar to Mollisols but contain either continuous or discontinuous

and provide the best grazing land in such cold climates because they are not acidic like many other soils of very cold climates.

Other soils which have a mollic epipedon are classified as

but the andic properties take precedence.

In the World Reference Base for Soil Resources (WRB), Mollisols are split up into Chernozems, Kastanozems and Phaeozems. Shallow or gravelly Mollisols may belong to the Leptosols. Many Aquolls are Gleysols, Stagnosols or Planosols. Mollisols with a natric horizon belong to the Solonetz.^[1]

See also

• Pedogenesis
• Pedology (soil study)
• Soil classification
• Soil science
• Soil type

References

• Brady, N.C. and Weil, R.R. (1996). ‘The Nature and Properties of Soils.’ 11th edition. (Prentice Hall, New Jersey).
• Buol, S.W., Southard, R.J., Graham, R.C., and McDaniel, P.A. (2003). ‘Soil Genesis and Classification.’ 5th edition. (Iowa State University Press - Blackwell, Ames.)

External links

• "Mollisols". USDA-NRCS. Archived from the original on 2006-05-09. Retrieved 2006-05-14.
• "Mollisols". University of Florida. Archived from the original on April 4, 2006. Retrieved 2006-05-14.
• "Mollisols". University of Idaho. Archived from the original on 2006-05-15. Retrieved 2006-05-14.