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Dominant Soil Orders1

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MOLLISOLS <br />

Mollisols have a dark-colored, organic-rich surface horizon (A horizon) and are found<br />

largely in grasslands. They occur from tropical to cold temperate, and from subhumid<br />

to semiarid environments.<br />

SPODOSOLS<br />

Spodosols have moderately acidic sandy profiles with an ashywhite<br />

upper horizon. In these soils, amorphous mixtures of<br />

organic matter and aluminum, with or without iron, have<br />

accumulated. They are typical of sandy soils under cool, wet<br />

conditions under conifer and hardwood forests such as in the<br />

boreal/cold temperate forests of Canada.<br />

GELISOLS <br />

Gelisols are soils that have permafrost within 100 cm of the soil<br />

surface and/or have gelic materials within 100 cm of the soil<br />

surface and have permafrost within 200 cm. Gelic materials are<br />

mineral or organic soil materials that have evidence of<br />

cryoturbation (frost churning) and/or ice segeration in the active<br />

layer (seasonal thaw layer) and/or the upper part of the permafrost.<br />

Occur in arctic and subarctic regions. Permafrost influences<br />

pedogenesis through its effect on the downward movement of the<br />

soil solution and on the soil forming processes.<br />

HISTOSOLS<br />

Histosols are dominantly organic. They are mostly soils that are<br />

commonly called bogs, moors, or peats and mucks. A soil is<br />

classified as Histosols if it does not have permafrost and is<br />

dominated by organic soil materials.<br />

ENTISOLS <br />

Entisols are recent soils with little or no profile development. At<br />

the most, have a weak organic matter surface layer (O horizon).<br />

Include deep, uniform sandy aeolian deposits (pictured here) to<br />

complex fluvial deposits. Some Entisols have steep, actively<br />

eroding slopes, and others are on flood plains or glacial outwash<br />

plains that frequently receive new deposits of alluvium.<br />

VERTISOLS<br />

Vertisols have a high content of expending clay and that have at<br />

some time of the year deep wide cracks. They shrink when drying<br />

and swell when they become wetter.<br />

______________<br />

1 Descriptions and images from–<br />

- NRCS http://soils.usda.gov/technical/classification/orders/ (Accessed 6/13/04)<br />

- Brady NC. RR Weil. 2008. The Nature and Properties of <strong>Soil</strong>s. Prentice-Hall. Ch 3.<br />

- Donahue, RL, R Miller, J Shickluna. 1983. <strong>Soil</strong>s: An Introduction to <strong>Soil</strong>s and Plant<br />

Growth. 5th Ed. Prentice-Hall.<br />

Other resources –<br />

http://soils.cals.uidaho.edu/soilorders/orders.htm<br />

http://soils.ifas.ufl.edu/faculty/grunwald/teaching/e<strong>Soil</strong>Science/soil_orders.shtml<br />

T.Kittel 604, 211

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