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Scientific Investigations Report 2010–5093

Prepared in cooperation with the New Jersey Department of Environmental Protection

Sediment Oxygen Demand in the Saddle River and Salem River Watersheds, New Jersey, July–August 2008

By Heather A. Heckathorn and Jacob Gibs

ABSTRACT

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Many factors, such as river depth and velocity, biochemical oxygen demand, and algal productivity, as well as sediment oxygen demand, can affect the concentration of dissolved oxygen in the water column. Measurements of sediment oxygen demand, in conjunction with those of other water-column water-quality constituents, are useful for quantifying the mechanisms that affect in-stream dissolved-oxygen concentrations. Sediment-oxygen-demand rates are also needed to develop and calibrate a water-quality model being developed for the Saddle River and Salem River Basins in New Jersey to predict dissolved-oxygen concentrations. This report documents the methods used to measure sediment oxygen demand in the Saddle River and Salem River watersheds along with the rates of sediment oxygen demand that were obtained during this investigation.

In July and August 2008, sediment oxygen demand was measured in situ in the Saddle River and Salem River watersheds. In the Saddle River Basin, sediment oxygen demand was measured twice at two sites and once at a third location; in the Salem River Basin, sediment oxygen demand was measured three times at two sites and once at a third location.

In situ measurements of sediment oxygen demand in the Saddle River and Salem River watersheds ranged from 0.8 to 1.4 g/m2d (grams per square meter per day) and from 0.6 to 7.1 g/m2d at 20 degrees Celsius, respectively. Except at one site in this study, rates of sediment oxygen demand generally were low. The highest rate of sediment oxygen demand measured during this investigation, 7.1 g/m2d, which occurred at Courses Landing in the Salem River Basin, may be attributable to the consumption of oxygen by a large amount of organic matter (54 grams per kilogram as organic carbon) in the streambed sediments or to potential error during data collection. In general, sediment oxygen demand increased with the concentration of organic carbon in the streambed sediments. Repeated measurements made 6 to 7 days apart at the same site locations resulted in similar values.

First posted July 16, 2010

For additional information contact:
Director, New Jersey Water Science Center
U.S. Geological Survey
810 Bear Tavern Rd., Suite 206
West Trenton, NJ 08628
http://nj.usgs.gov/

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Suggested citation:

Heckathorn, H.A., and Gibs, J., 2010, Sediment oxygen demand in the Saddle River and Salem River watersheds, New Jersey, July–August 2008: U.S. Geological Survey Scientific Investigations Report 2010–5093, 10 p.



Contents

Acknowledgments

Abstract

Introduction

Purpose and Scope

Study Areas

Methods and Procedures

Study Design

Sediment Oxygen Demand Chambers

Sediment Oxygen Demand Chamber Deployments

Calculation of Sediment Oxygen Demand

Sediment Oxygen Demand in the Saddle River and Salem River Watersheds

Rates of Sediment Oxygen Demand

Factors Affecting Sediment Oxygen Demand

Composition of Streambed Material and Streamflow Regime

Water-Column Oxygen Demand

Summary

References Cited



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