Relationships of Aquatic Macrophytes to Sediment and Groundwater Characteristics in McDill Pond -- Implications for Lake Management

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Date
2000-06Author
Lyden, Tiffany G.
Publisher
University of Wisconsin-Stevens Point, College of Natural Resources
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Show full item recordAbstract
McDill Pond is a 261 acre impoundment located in Stevens Point,
Wisconsin. Since the late 1960's, abundant macrophyte growth has prompted
the use of control methods. Despite control methods, surveys have shown
substantial increases in aquatic plant growth over time.
This study was conducted in 1996 and 1997 as part of a DNR lake
planning grant to investigate the relationships of aquatic plants to sediment and
groundwater characteristics. Improved understanding of the influence of
environmental factors on aquatic plant growth and distribution can provide for
more effective aquatic plant management. Study results will be incorporated into
a comprehensive lake management plan for McDill Pond.
Thirty sampling sites were established on McDill Pond. Aquatic plant and
sediment data were collected in June, July, and August of 1996. Seepage meter
and mini-piezometers were used to collect pore water chemistry. Interstitial
water chemistry was collected at all sites in 1997 in an attempt to characterize
the pore water in the aquatic plants' rooting zones. Aquatic plant samples were
collected and analyzed for biomass, species distribution, and plant nutrition, and
sediment was collected and analyzed for chemistry, organic matter, and texture.
Seepage meter, mini-piezometer, and interstitial samples were analyzed for
chemistry.
Elodea canadensis (Elodea) was significantly positively correlated with
sediment potassium levels, and increasing sediment ammonia levels occurred
with increasing plant biomass for all four dominant species in the lake. In terms
of sediment texture, Ceratophyllum demersum (Coontail) was significantly
positively correlated with finer grained sediments, and negatively correlated with
coarser grained sediments. Significant physical and chemical differences were
noted between groundwater inflow and non-groundwater inflow sites.
Groundwater inflow sites showed oxidized conditions and lower nutrient levels,
suggesting that redox conditions control nutrient availability. Interstitial nutrient
results also suggest the release of phosphorus and nitrogen under reduced
conditions and the unavailability of those same nutrients under oxidized
conditions.
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http://digital.library.wisc.edu/1793/80772Type
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