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 19:83-88 (1990)
© 1990 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 Clausen, J. C.
Right arrow Articles by Johnson, G. D.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Clausen, J. C.
Right arrow Articles by Johnson, G. D.
Agricola
Right arrow Articles by Clausen, J. C.
Right arrow Articles by Johnson, G. D.

Lake Level Influences on Sediment and Nutrient Retention in a Lakeside Wetland

J. C. Clausen*

School of Nat. Resourc., Aiken Center, Univ. of Vermont, Burlington, VT 05405;

G. D. Johnson

Minn. Pollut. Control Agency, St. Paul, MN 55155;

* Corresponding author.

ABSTRACT

Lake levels, sediment and nutrient retention, and flows were studied in a 180-ha wetland adjacent to Lake Champlain, VT, to assess the role of lake levels on sediment and nutrient retention within the wetland. This wetland received both point and nonpoint sources of nutrients. Input, output, and within-wetland water samples were collected at 15 sites, and flows were measured nine times in 1983 at lake levels varying over 2 m. The ratio of wetland inflow to outflow was related to changes in lake levels. During spring, the concentrations of total suspended solids, total P, and total Kjeldahl N throughout the wetland were lower than during summer and fall periods. Wetland outlet concentrations decreased with rising lake levels. When wetland inflows exceeded outflow, there was a net mass retention of total suspended solids, total P, and total Kjeldahl N. Exports from the wetland decreased as lake level increased. The sediment and nutrient treatment capacity of this lakeside wetland appeared to be dominated by hydrologic influences.


NOTES

Contribution from the School of Natural Resources, Univ. of Vermont.

Funding provided by USDA-ASCS and SCS.

Received for publication July 11, 1988.





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 © 1990 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.