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


     


Published online 14 July 2009
Published in Soil Sci Soc Am J 73:1587-1596 (2009)
DOI: 10.2136/sssaj2008.0218
© 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
Google Scholar
Right arrow Articles by Donohue, S. W.
Right arrow Articles by Groffman, P.
PubMed
Right arrow Articles by Donohue, S. W.
Right arrow Articles by Groffman, P.
Agricola
Right arrow Articles by Donohue, S. W.
Right arrow Articles by Groffman, P.
Related Collections
Right arrow Saturation
Right arrow Redox Processes
Right arrow Ground Water Quality

WETLAND SOILS

Human-Transported Material Soils of Urbanizing Estuarine Landscapes

Sean W. Donohuea, Mark H. Stolta,*, Art Golda and Peter Groffmanb

a Dep. of Natural Resources Science, Univ. of Rhode Island, Kingston, RI 02892
b Institute of Ecosystem Studies, Box AB, Millbrook, NY 12545

* Corresponding author (mstolt{at}uri.edu).

Additions of human-transported materials (HTM) have significantly altered many coastal shorelines and wetlands. The hydrology and the ability of these anthropogenic soils to support ecologically important functions is poorly understood. In this study, we documented soil hydrologic patterns along disturbed estuarine shorelines and wetlands. Our goal was to determine if the soils had properties relative to the potential to support denitrification (i.e., labile C, saturation, and reducing conditions). Eleven anthropogenic sites, located in Rhode Island and 30 to >60 yr old, were studied. Auger transects were completed to characterize anthropogenic soils. Water table levels were monitored twice a month. Anthropogenic soils were described and sampled from pits at five representative locations. Soil organic C (SOC), permanganate-oxidizable C (POC), bulk density, and pH were measured. Deposits of HTM, comprised of dredge and fill materials, ranged in thickness from 26 to >285 cm, were predominantly sandy and often contained artifacts. In the thickest HTM deposits, water table levels rose as much as 2.5 m above the original buried soil surface. Redoximorphic features were identified within the range of water table activity in 16 of the 18 monitored anthropogenic soils, suggesting reducing conditions. Soil organic C ranged from 1.6 to 88.9 g kg–1, was highest in surface horizons, and had an irregular distribution with depth. Labile C, estimated from POC measurements, followed the SOC distribution. Evidence of labile C, saturation, and reducing conditions in the majority of these soils suggest that most of the disturbed estuarine soils we studied have the capacity for denitrification.

Abbreviations: HTM, human-transported materials • POC, permanganate-oxidizable carbon • RMF, redoximorphic features • SOC, soil organic carbo







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.