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


     


Published in J Environ Qual 23:730-738 (1994)
© 1994 American Society of Agronomy, Crop Science Society of America, and 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
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wieder, R. K.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Wieder, R. K.
Agricola
Right arrow Articles by Wieder, R. K.

Diel Changes in Iron(III)/Iron(II) in Effluent from Constructed Acid Drainage Treatment Wetlands

R. Kelman Wieder*

Department of Biology, Villanova Univ., Villanova, PA 19085.

* Corresponding author (wieder{at}ucis.vill.edu).

ABSTRACT

Within the past decade, over 400 wetlands have been constructed to treat acid coal mine drainage (AMD). This study was undertaken to examine whether the efficiency with which constructed wetlands retain Fe present in AMD changes on a day-night basis. In each of live AMD treatment wetlands, constructed with a different organic substrate (Sphagnum peat with limestone and fertilizer, Sphagnum peat, sawdust, straw-manure, or mushroom compost), hourly sampling of inflow and outflow waters was conducted over a 19-h (July 1990) and 24-h period (May 1991). The chemical composition of the influent AMD was relatively stable over the duration of either sampling period. However, a striking diel pattern of shifts in the relative abundances of Fe2+ and Fe3+ in outflow waters was observed for both Sphagnum peat wetlands on both sampling dates, and for the straw-manure and mushroom compost wetlands on the May 1991 sampling date. Prior to sunrise, 75 to 100% of the soluble Fe in outflow waters was Fe2+; prior to sunset, 62 to 88% of the soluble Fe was Fe3+. The documented did shifts in Fe3+ vs. Fe2+ abundance in outflow waters are greater in magnitude than any previously reported for a natural system and suggest that the cycling of Fe in AMD treatment wetlands is more dynamic than previously recognized and that standard daytime only sampling protocols are inadequate for assessing Fe retention-release in AMD treatment wetlands.


Received for publication May 7, 1993.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Copyright © 1994 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.