JEQ Grow Your Career With ASA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 17:185-188 (1988)
© 1988 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 Kunishi, H. M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Kunishi, H. M.
Agricola
Right arrow Articles by Kunishi, H. M.

Sources of Nitrogen and Phosphorus in an Estuary of the Chesapeake Bay

H. M. Kunishi*

USDA, Agric. Res. Service, Environ. Chem. Lab., Beltsville, MD 20705.

* Corresponding author.

ABSTRACT

This study examined the contribution of agriculture to the nutrient (N and P) concentrations in the Wye River, an estuarine tributary the Chesapeake Bay. The river drains a watershed that is devoted mainly to farming and is devoid of any sources of municipal and industrial wastes. Water samples were analyzed for NO3-N + NO2-N and molybdate-reactive P (MRP). The concentrations of these forms nutrients were then examined in relation to sampling site, sample salinity, and time of year. Freshwater entering the river (brackish) from the watershed contained consistently high concentrations of NO3-N (about 4 mg L–1) and low concentrations of PO4-P (about 40 µg L–1). Once these nutrients entered the estuarine part of the river, however, the concentrations of NO3-N decreased to low levels within a short distance (500–700 m) from the point of riverine discharge, through both dilution with brackish water and apparent microbial action. The concentrations of MRP increased markedly through release from within estuary sources. Concomitantly, the estuary released large quantities of NH4. The estuary itself, therefore, was the immediate major source of N (as NH4) and P.

Key Words: Tide • Ammonium-N • Nitrate-N • Molybdate-reactive phosphate • Salinity


Received for publication March 19, 1987.





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
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 1988 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.