Missouri Water Science Center

Water Quality, Hydrology, and Invertebrate Communities of Three Remnant Wetlands in Missouri, 1995—97

By: David C. Heimann and Suzanne R. Femmer, U.S. Geological Survey

ABSTRACT

This report presents the results of a study conducted by the U.S. Geological Survey in cooperation with the Missouri Department of Natural Resources from December 1995 through May 1997 to describe the water quality, hydrologic, and invertebrate characteristics of three remnant wetlands. These data may be used to help develop selected water-quality standards for wetlands in Missouri. Wetlands monitored in this study include Spile Lake, Vernon County; Little Bean Marsh, Platte County; and Forker Oxbow, Linn County, Missouri.

Extremes in physicochemical properties in these wetlands were greatly affected by thermal stratification, hydrologic fluctuations, biological activity, and ice formation. The wetlands had dissolved-oxygen concentrations below the 5-milligrams-per-liter State water-quality standard from 40 to 60 percent of a selected 1-year period, corresponding to periods of thermal stratification. Hydrologic fluctuations were common as the water-surface elevation changes in these systems ranged up to 12 feet during the course of the study. Photosynthesis and respiration are likely causes of diurnal fluctuations in pH and dissolved oxygen throughout the study period, but particularly in the summer months. Periods of ice formation were short lived in the wetlands, but corresponded with maximum values of specific conductance and dissolved oxygen in all three systems.

Analyses of invertebrate results using the Jaccard Coefficient of Community Similarity indicated mixed results. Woody snag sample results showed little similarities between sites, while sweep net sample results indicated similarities existed. Most of the families detected at these sites are considered organic tolerant as indicated by the Hilsenhoff Biotic Index. Analysis of the dominant taxon indicates that one or two invertebrate families that are tolerant to organic enrichment generally dominate the wetlands.

The hydrologic, water quality, and invertebrate information analyzed in this study indicate that while there are similarities among wetlands, these are unique systems. The statistical comparisons between water-quality constituents in wetlands and streams indicate dissimilarities are common. Including the presence of thermal stratification in these wetlands, the exclusions and modifications in State standards that are applied to lakes and reservoirs also may be applicable.

TABLE OF CONTENTS

Abstract

Introduction

Purpose and Scope

Previous Investigations

Study Site Location and Description

Acknowledgements

Methods

Water Quality

Statistical Analyses

Hydrology

Invertebrates

Hydrologic Characteristics

Water-Surface Elevation

Bathymetry, Area, and Storage

Hydraulic Residence Time

Water-Quality Characteristics

Physicochemical Properties

Specific Conductance

pH

Water Temperature

Dissolved Oxygen

Turbidity

Nutrients

Statistical Comparison of Physicochemical Properties and Nutrient Concentrations Between Wetlands and Streams

Wetland Response During Hydrologic and Seasonal Extremes

Hydrologic Extremes

Seasonal Extremes

Invertebrate Community Characteristics

Summary

References Cited

FIGURES

1.—4.  Maps showing:

 1.  Location of three study wetlands and natural divisions of Missouri

 2.  Location of sampling site in Spile Lake near Horton, Missouri, and vicinity

 3.  Location of sampling site in Little Bean Marsh near Bean Lake, Missouri, and vicinity

 4.  Location of sampling site in Forker Oxbow near Fountain Grove, Missouri, and vicinity

 5.  Photographs showing site characteristics of Spile Lake, Little Bean Marsh, and Forker Oxbow in Missouri

 6.  Photograph showing retrieval of multi-parameter water-quality sensor and protective case at Spile Lake, January 1996

 7.  Graphs showing temporal variability in water-surface elevations in Spile Lake, Little Bean Marsh, and Forker Oxbow

8.—10.  Maps showing:

 8.  Bathymetry of Spile Lake near Horton, Missouri

 9.  Bathymetry of Little Bean Marsh near Bean Lake, Missouri

10. Bathymetry of Forker Oxbow near Fountain Grove, Missouri

11.—30.  Graphs showing:

11. Temporal variability in wetland wetted-surface area at Spile Lake, Little Bean Marsh, and Forker Oxbow

12. Temporal variability in wetland storage in Spile Lake, Little Bean Marsh, and Forker Oxbow

13. Distributions of specific conductance, pH, near-surface and near-bottom water temperatures, and dissolved oxygen in Spile Lake, Little Bean Marsh, and Forker Oxbow

14. Median daily specific conductance at Spile Lake, Little Bean Marsh, and Forker Oxbow

15. Maximum and minimum daily pH values at Spile Lake, Little Bean Marsh, and Forker Oxbow

16. Maximum daily near-surface and near-bottom water temperatures for Spile Lake, Little Bean Marsh, and Forker Oxbow

17. Maximum and minimum daily dissolved-oxygen concentrations at Spile Lake, Little Bean Marsh, and Forker Oxbow

18. Cumulative time frequency distribution of dissolved-oxygen concentrations at Spile Lake, Little Bean Marsh, and Forker Oxbow for period of record and selected one-year period

19. Distribution of selected nutrients in Spile Lake, Little Bean Marsh, and Forker Oxbow

20. Temporal variability of physicochemical properties and stage at Spile Lake during a February 20–28, 1997, flood event from adjacent Little Osage and Marmaton Rivers

21. Temporal variability of physicochemical properties and stage at Little Bean Marsh during an April 10–15, 1997, rainfall-runoff event

22. Temporal variability of physicochemical properties and stage at Forker Oxbow during a May 25–30, 1997, flood event from adjacent Locust Creek

23. Temporal variability of physicochemical properties and stage at Spile Lake during a summer low-stage period

24. Temporal variability of physicochemical properties and stage at Spile Lake during a winter low-stage period

25. Temporal variation in normalized invertebrate abundance data for Spile Lake, Little Bean Marsh, and Forker Oxbow

26. Variability by sampling method of normalized invertebrate abundance data for Spile Lake, Little Bean Marsh, and Forker Oxbow

27. Contribution percentage by three dominant invertebrate taxon by sampling method and sample period

28. Number of families represented in invertebrate snag and sweep samples by site and sample period

29. Taxonomic distribution of invertebrate data for August 1996 snag samples

30. Taxonomic distribution of invertebrate data for August 1996 sweep samples

TABLES

  1.    Summary of hourly wetland physicochemical property results, December 1995 to May 1997
  2.    Wetland nutrient results
  3.    Summary of statistical comparison (Mann-Whitney test) of wetland physicochemical properties and constituents to those of selected stream in the same natural division
  4.    Taxonomic summary of invertebrate snag and sweep samples from three wetlands for March, June, August, and October 1996 sampling periods
  5.    Jaccard Coefficient of Community Similarity results for March, June, August, and October 1996 invertebrate snag and sweep samples
  6.    Hilsenhoff Biotic Index Classification results for June and August 1996 invertebrate sweep samples
Conversion Factors and Datum
Multiply By To obtain
  Length  
     
inch (in.) 2.54
centimeter
inch (in) 25.4 millimeter
foot (ft) 0.3048 meter
mile (mi) 1.609 kilometer
     
  Area  
     
acre 4,047 square meter (m2)
acre 0.4047 hectare
acre 0.4047 square hectometer
acre 0.004047 square kilometer
square foot (ft2) 0.09290 square meter
square mile (mi2) 259.0 hectare
     
  Volume  
     
cubic foot (ft3) 28.32 cubic liter
cubic foot (ft3) 0.02832 cubic meter
acre-foot (acre-ft) 1,233 cubic meter
acre-foot (acre-ft) 0.001233 cubic hectometer
gallon (gal) 4.20 liters
     
  Flow rate  
     
cubic foot per second (ft3/s) 0.02832 cubic meter per second
     
  Mass
     
ounce, avoirdupois (oz) 28.35 gram
pound, avoirdupois (lb) 0.4356 kilogram
     
  Density  
     
pound per cubic foot (lb/ft3) 16.02 kilogram per cubic meter
pound per cubic foot (lb/ft3) 0.01602 gram per cubic centimeter

Temperature in degrees Celsius (°C) may be converted to degrees Fahrenheit (°F) as follows:
° F = (1.8 x °C) + 32

Temperature in degrees Fahrenheit (°F) may be converted to degrees Celsius (°C) as follows:
° C = (°F - 32) / 1.8

Sea level: In this report, "sea level" refers to the National Geodetic Vertical Datum of 1929 (NGVD of 1929)—a geodetic datum derived from a general adjustment of the first-order level nets of both the United States and Canada, formerly called Sea Level Datum of 1929.

 


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For more information about USGS activities in Missouri contact:

Director

U.S. Geological Survey

Missouri Water Science Center

1400 Independence Road

Rolla, Missouri 65401

Telephone: (573) 308-3667

Fax: (573) 308-3645


or access the USGS Missouri Water Science Center home page at:  http://mo.water.usgs.gov/.



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