18. Ultisols: Low Base Status Soils with Finer-Textured Subsoil Horizons
Published Online: 5 AUG 2011
DOI: 10.1002/9780470960622.ch18
Copyright © 2011 John Wiley & Sons, Inc.
Book Title

Soil Genesis and Classification, Sixth Edition
Additional Information
How to Cite
Buol, S. W., Southard, R. J., Graham, R. C. and McDaniel, P. A. (2011) Ultisols: Low Base Status Soils with Finer-Textured Subsoil Horizons, in Soil Genesis and Classification, Sixth Edition, Wiley-Blackwell, Oxford, UK. doi: 10.1002/9780470960622.ch18
Publication History
- Published Online: 5 AUG 2011
- Published Print: 2 SEP 2011
ISBN Information
Print ISBN: 9780813807690
Online ISBN: 9780470960622
- Summary
- Chapter
Keywords:
- Ultisols, low base status soils - with finer-textured subsoil horizons;
- Ultisols, and clay content increase - with depth, identifying argillic or kandic horizon;
- Ultisols, forming in acidic parent materials - in locations, precipitation exceeding potential evapotranspiration;
- Ultisols, in southeastern Asia - the upper Amazon basin in South America, the Congo River basin in Africa;
- Ultisols, some classified as latosols or laterites - red color, in intertropical regions;
- pedogenic processes - extensive leaching, over a long period;
- lessivage, and formation - of argillic and kandic horizons, very pronounced;
- Ultisols, dominant soils - formed on piedmont of southeastern United States;
- timber production - extensive on many Ultisols;
- significant Ultisol features – abrupt, or a clay content increase
Summary
This chapter contains sections titled:
Setting
Pedogenic Processes
Uses of Ultisols
Classification of Ultisols
Perspective
