17. Spodosols: Soils with Subsoil Accumulations of Humus and Sesquioxides
Published Online: 5 AUG 2011
DOI: 10.1002/9780470960622.ch17
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) Spodosols: Soils with Subsoil Accumulations of Humus and Sesquioxides, in Soil Genesis and Classification, Sixth Edition, Wiley-Blackwell, Oxford, UK. doi: 10.1002/9780470960622.ch17
Publication History
- Published Online: 5 AUG 2011
- Published Print: 2 SEP 2011
ISBN Information
Print ISBN: 9780813807690
Online ISBN: 9780470960622
- Summary
- Chapter
Keywords:
- Spodosols, soils with subsoil accumulations - of humus and sesquioxides;
- “white earths,” the Spodosols - contrasting sharply with “black earths,” the Mollisols;
- Spodosols, and soils called Podzols - from the Russian pod (beneath) and zol (ash);
- major setting for Spodosols - humid boreal climatic zone microthermal snow-forest climate;
- profile, of the Myakka soils in Florida;
- pedogenic processes - mobilization and eluviation of aluminum and iron, from O, A, and E horizons;
- immobilization of organometallic complexes - in spodic horizon, and mechanisms;
- profile distributions of aluminum, iron and carbon - optical density of oxalate extract (ODOE) distribution;
- uses of Spodosols - for forestry, pasture, hay and cultivated crops;
- Spodosols, with high water tables (or artificially drained) - in suborder Aquods
Summary
This chapter contains sections titled:
Setting
Pedogenic Processes
Uses of Spodosols
Classification of Spodosols
Perspective
