SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 60:1495-1501 (1996)
© 1996 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Evans, C. V.
Right arrow Articles by Mokma, D. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Evans, C. V.
Right arrow Articles by Mokma, D. L.
Agricola
Right arrow Articles by Evans, C. V.
Right arrow Articles by Mokma, D. L.

Sandy Wet Spodosols: Water Tables, Chemistry, and Pedon Partitioning

C. V. Evans*

Department of Natural Resources, Univ. of New Hampshire, 215 James Hall, Durham, NH 03824

D. L. Mokma

Dep. of Crop and Soil Sciences, Michigan State Univ.

*Corresponding author (cve{at}christa.unh.edu).

ABSTRACT

Spodosols are notably difficult to classify in terms of moisture regime, presumably because redox colors are masked by spodic colors, or perhaps because the absence of structure in sandy Spodosols is a hindrance to detection of redox features. Some views of Spodosol pedons as a series of compartments raise the possibility that some portions of the spodic pedon are simply more responsive than others to saturation parameters. This study attempts to determine whether compartmentalization within Spodosol pedons results in differentiation of soil response to saturation and water table fluctuation. Water table and chemical data were compiled from 16 Aquod pedons. Pyrophosphate-extractable Fe and Al, oxalate-extractable Fe and Al, and dithionite-extractable Fe and Al were determined for all soils; organic C was also determined for at least Bh, Bhs, and Bs horizons, and oxalate-extractable Si and the optical density of the oxalate extract (ODOE) were also determined for eight of the pedons. Comparisons of chemical data to saturation and water table fluctuation indicated that spodic horizon chemistry was unresponsive to both saturation duration and water table fluctuation. Chemistry of E horizons was most responsive to water table fluctuation, while Al and Si levels of C horizons were more sensitive to saturation and water table fluctuations. Thus, due to compartmentalization of Spodosol pedons, interpretations of saturation and water table fluctuation can be most effectively made from the chemistry of C and E horizons, respectively. The B horizon chemistry was not a good indicator of saturation duration or of water table fluctuation patterns.


NOTES

Scientific Contribution no. 1922 of the New Hampshire Agric., Exp. Stn., Durham

Received for publication July 24, 1995.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1996 by the Soil Science Society of America.