University of Idaho - I Banner
students walk on University of Idaho campus

Visit U of I

Learn about the many reasons the University of Idaho could be a perfect fit for you. Schedule Your Visit

Parents on campus during orientation

Homecoming Oct. 14 - 21

Join other Vandal families for a week of celebration and Vandal traditions. View Calendar

campus full of students

U of I Retirees Association

UIRA has a membership of nearly 500 from every part of the University. Learn More

Contact

Department of Soil and Water Systems

Physical Address:
E. J. Iddings Agricultural Science Laboratory, Rm 242
606 S Rayburn St

Mailing Address:
875 Perimeter Drive MS 2340
Moscow, ID 83844-2340

Phone: 208-885-0111

Email: cals-sws@uidaho.edu

Web: uidaho.edu/cals/sws

Directions

Ultisols

Ultisols (from Latin ultimus, "last") are strongly leached, acid forest soils with relatively low native fertility. They are found primarily in humid temperate and tropical areas of the world, typically on older, stable landscapes. Intense weathering of primary minerals has occurred, and much Ca, Mg and K has been leached from these soils. Ultisols have a subsurface horizon in which clays have accumulated, often with strong yellowish or reddish colors resulting from the presence of Fe oxides. The "red clay" soils of the southeastern United States are examples of Ultisols. They are divided into five suborders: Aquults, Humults, Udults, Ustults and Xerults.

Because of the favorable climate regimes in which they are typically found, Ultisols often support productive forests. The high acidity and relatively low quantities of plant-available Ca, Mg and K associated with most Ultisols make them poorly suited for continuous agriculture without the use of fertilizer and lime. With these inputs, however, Ultisols can be very productive. They occupy approximately 8.1 percent of the global ice-free land area and support 18 percent of the world's population. They are the dominant soils of much of the southeastern U.S. and occupy approximately 9.2 percent of the total U.S. land area.

Ultisols
Ultisols have: (1) a subsurface zone of clay accumulation — either an argillic or kandic horizon; and (2) base saturation of less than 35 percent in the subsoil. This second criterion is what distinguishes Ultisols from Alfisols. (USDA-NRCS image)

Contact

Department of Soil and Water Systems

Physical Address:
E. J. Iddings Agricultural Science Laboratory, Rm 242
606 S Rayburn St

Mailing Address:
875 Perimeter Drive MS 2340
Moscow, ID 83844-2340

Phone: 208-885-0111

Email: cals-sws@uidaho.edu

Web: uidaho.edu/cals/sws

Directions