SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 1 May 2009
Published in Soil Sci Soc Am J 73:831-840 (2009)
DOI: 10.2136/sssaj2008.0159
© 2009 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
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 Richardson, T. C.
Right arrow Articles by Hall, G. B.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Richardson, T. C.
Right arrow Articles by Hall, G. B.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Richardson, T. C.
Right arrow Articles by Hall, G. B.
Related Collections
Right arrow Ecosystem Management
Right arrow Soil Hydrology
Right arrow Wetland Soils

WETLAND SOILS

Hydrologic Signature Analysis of Select Organic Hydric Soil Indicators in Northeastern Florida

Travis C. Richardson*, C. Price Robison, Cliff P. Neubauer and Greenville B. Hall

St. Johns River Water Management District, Division of Environmental Resource, Management, P.O. Box 1429, Palatka, FL 32178-1429

* Corresponding author (TRichardson{at}sjrwmd.com).

The magnitude, duration, and return intervals of surface water flooding and dewatering of the landward extent of the hydric soil indicators muck (LM), histic epipedon (LHE), and Histosol (LH) were quantitatively defined, providing a better understanding of the hydrologic conditions maintaining these hydric soil indicators. Land surface elevations were determined for the LM, LHE, and LH at 16 lakes with long-term (30–60-yr) modeled or gauged hydrologic data. The probability of flooding and dewatering of the elevations of the LM, LHE, and LH were determined from frequency analysis of hydrologic data from each lake. The resulting hydrologic signatures for the LM, LHE, and LH are composed of magnitude and return interval of 1, 30, 90, 183, 274, and 365-d duration flooding and dewatering events. As an example, the LM, LHE, and LH were flooded for 30 continuous days with average annual probabilities of 42, 65, and 77%, respectively. As a second example, the LM, LHE, and LH were dewatered for 365 continuous days with average annual probabilities of 49, 24, and 16%, respectively. Probabilities of flooding and dewatering for the LM, LHE, and LH are presented for 1, 30, 90, 183, 274, and 365-d durations. Mean hydrologic signatures reduce variability and may be considered representative of each soil characteristic. Quantitatively defining the hydrology associated with the presence of the LM, LHE, and LH as well as other soil characteristics is essential for environmental protection, assessment of hydrologic impacts, wetlands restoration, wetlands creation, and other environmental management applications.

Abbreviations: DO, dissolved oxygen • LH, landward extent of Histosol • LHE, landward extent of histic epipedon • LM, landward extent of muck • NPP, net primary production • SOM, soil organic matter







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 © 2009 by the Soil Science Society of America.