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Goals and Objectives: The goal of the project is to predict the
transport of zebra mussel larvae in rivers and estuaries so that
control strategies can be designed and evaluated. The physical
processes of the transport are being coupled with models of the
biological processes to determine the most important factors
affecting settlement. This work will help in applying the
results of this study to other rivers and estuaries. To achieve
the goals, we will
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Identify the main mechanisms affecting
physical transport in the Illinois and Hudson Rivers.
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Model the less well-understood
mechanisms in detail and parameterize them in terms of
easily-measured parameters.
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Construct a single model that combines
the physical transport mechanisms with the biology and
population dynamics.
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Identify the processes controlling the
transport and settlement patterns.
Summary of Progress:
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Separated effects of
dispersion, mortality, and settlement on the evolution of
zebra mussel larvae in the Illinois River and predicted
settlement patterns for simple hydrodynamic conditions.
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Constructed and started testing
a model that predicts the transport of larvae and evolution
of adult zebra mussels in a river with more realistic
hydrodynamics.
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Identified several key areas in
the Illinois River that affect larval transport, including
Peoria Lake and several locks and dams.
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Conducted two dye tracking
experiments in the Hudson River to measure dispersion
parameters and assess the importance of side embayments on
the trapping of zebra mussel larvae.
Accomplishments/Benefits:
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Data from previous float trips
following cohorts of zebra mussels in the Illinois River
allowed us to obtain quantitative estimates of dispersion,
mortality, and settlement in the field rather than in a
laboratory. This information was used in a simplified model to
predict settlement patterns in the Illinois River and estimate
transport and settlement in other large rivers. The model
shows that differences in flow and larval cohort
characteristics can lead to significant variations in
settlement location, area, and abundance.
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A mathematical model of transport
of larvae and evolution of adult populations will allow us to
account for the biological and physical processes in more
detail and predict settlement pattern in the Illinois River
and other rivers. This model includes effects of ‘dead zones’
(such as backwater lakes and areas behind locks and dams) and
nonuniform larval age in a cohort. Agencies like the Army
Corps of Engineers can use such a model to predict effects of
control schemes on the downstream zebra mussel populations.
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A dye study in the Hudson River
in August 2000 suggested that side embayments can be important
in trapping zebra mussel larvae and that accounting for the
hydrology of the region can be important. In particular,
embayments may act as refuges for zebra mussels and runoff
from large storms may flush larvae (or dye) into the main
channel of the river. Measurements of abundance and settlement
from the companion National Sea Grant project that show a
correlation between settlement and rainfall support the
inferences from the dye study.
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A dye study in the Hudson River
in August 2001 measured the exchange between a large bay and
the main channel. The dye, which acts as a surrogate for
nutrients or zebra mussel larvae, was released at two inlets
to North Tivoli Bay as water started entering the bay (i.e.,
just after low tide). Preliminary results from one of the
inlets suggest that much of the dye leaves the bay in a single
tidal cycle but little returns. The final results of the study
will allow us to quantify the exchange between the bay and the
main channel and construct an approximate exchange model for
the monthly tidal cycle.
Narrative Report: This project, along with a companion project
funded by the National Sea Grant College Program, seeks to help
in reducing the destructive effects of the zebra mussel. Zebra
mussels have affected the ecology of North American water bodies
and caused hundreds of millions of dollars of damage at
hydropower plants, sewage treatment plants, and water supply
facilities. Most schemes to control the zebra mussel focus on
individual sites―either to remove them from a particular
facility or to prevent future invasions. However, Stoeckel et
al. (1997) suggested a scheme to control zebra mussels in an
entire ecosystem. They recognized that since local populations
of zebra mussels in a large river are maintained not by larvae
produced locally but by larvae produced upstream, blocking the
upstream larval supply will cause the downstream populations to
quickly decline.
The success of such an ecosystem-wide control
scheme requires an understanding of both the biological factors
and the physical processes affecting the transport. The goal of
this project is to predict the transport and settlement patterns
of zebra mussel larvae in rivers and estuaries so that a control
strategy exploiting the biology of the zebra mussel and the
hydrodynamics of the river can be designed and evaluated. We
have focused on the Illinois River, in which the flow and
therefore larval transport is mainly downstream, and a section
of the Hudson River in which the tidal effects are significant.
We have progressed toward developing a model that can be used to
evaluate the effectiveness of control strategies, like dispersal
barriers, under a range of physical and biological conditions.
The model can also be used to identify the main factors
affecting the establishment of zebra mussel populations to
facilitate the design of control measures in other rivers.
For the Illinois River we have estimated
effects of dispersion, mortality, and settlement on the
evolution of zebra mussel larvae and identified and started
modeling key areas that affect larval transport. Data collected
during float trips on the Illinois River have allowed us to
estimate physical and biological parameters. As part of a
previous Sea Grant project, co-PI Schneider and other
investigators on the companion National Sea Grant project
followed cohorts of zebra mussel larvae as they drifted
downstream. Thus, we are able to observe the evolution of a
cohort from early in the life cycle to settlement. A time series
of larval abundance measurements typically shows three stages.
At first, the abundance decreases simply because the cohort is
spreading due to physical dispersion along the channel. In the
second stage, a sharp decrease typically occurs because of
increased mortality as the larvae move from the D-stage to the
umbonal stage. In the final stage, the abundance decreases
sharply once more when the larvae are large enough to settle.
We have used these data in developing a model
that combines the hydrodynamics with the biology. We estimated
dispersion, which affects the cohort throughout its evolution,
from regressions based on the tracer experiments of Zuehls
(1987) in the Illinois River. Once dispersion is accounted for,
mortality and settlement as a function of time or larval age can
be estimated from solutions to a transport equation that
includes advection, dispersion, mortality, and settlement. The
scientific impact of this part of the project is that it
provides one of the few estimates of mortality and settlement in
the field rather than the laboratory. It also shows a large
increase in mortality occurs near the transition between the
D-stage and umbonal stage. Compared to the decrease in peak
abundance due to mortality, the decrease due to dispersion is
small. The practical benefits include improved ability to
predict settlement patterns and information that can be
exploited in targeting zebra mussels during critical stages of
their development.
The analysis of the field data used a
relatively simple description of the physical transport.
However, the details of the transport can be crucial for the
success of a control scheme; for example, if zebra mussels can
form and sustain a local population behind a navigation dam,
they may be able to supply downstream populations with larvae
and reduce the effectiveness of a dispersal barrier in the
Chicago waterways. To include the effects of these details, we
have developed a mathematical model based on the aggregrated
dead zone model (Rutherford 1994). Because the mortality and
settlement depend strongly on age or stage of the larvae, we
have also accounted for variations in ages of the larvae in a
cohort. We are now implementing a numerical simulation of the
mathematical model. This model can then be used by agencies like
the Army Corps of Engineers to assess the effect of control
schemes.
To choose the parameters for the model, we
have used two dye studies in the Hudson River to help us
understand and quantify exchange between a side embayment and
the main channel of a river. In August 2000 we injected a slug
of fluorescent dye, Rhodamine WT, at Mills-Norrie State Park and
measured concentrations at the injection site and nearby sites
over several tidal cycles, or two to three days. Because the
reach of the Hudson River we studied has significant tidal
influence, an issue with the injection was the timing relative
to the tidal cycle. To minimize dispersion during the injection
and avoid high concentrations near Poughkeepsie, we released the
dye just as the current turned north. We injected dye twice; the
first release of 3 gallons of dye showed that much of the dye
entered a marina just north of the injection site. For the
second experiment, we released 9 gallons of dye and focused on
the exchange between the side embayment (i.e., the marina) and
the main channel. We sampled concentrations at the injection
site, at five locations in the marina, and one location just
north of the marina. Sampling continued until concentrations
reached the background level measured before the injection.
During the second release much of the dye
entered the marina and remained visible for about a tidal cycle,
or half a day. A severe thunderstorm arrived about eight hours
after the injection and lasted for several hours. Over 500 water
samples were collected in the marina. From these samples, we
determined the fraction of the dye that is in the marina or
embayment as a function of time and obtained a quantitative
estimate of the exchange between the marina and the main
channel. The embayment initially trapped nearly 50% of the dye,
but runoff from the storm entered the marina and apparently
flushed the dye, bringing concentrations back to background
levels after about 1.5 tidal cycles. In contrast, dye
concentrations measured in the main channel showed that the dye
cloud returned to the injection site three times (that is, over
three tidal cycles) before it dispersed enough to be
undetectable.
The dye study results suggest that side
embayments can trap significant amounts of zebra mussel larvae
spawned near the shore. However, they also show that while the
small tributaries may have a minor effect on the flow in the
main channel, they may affect zebra mussel populations
dramatically by flushing larvae from refuges on the side of
rivers. Measurements of abundance and settlement over several
months, which were part of the companion National Sea Grant
project, support this conclusion: At Mills-Norrie State Park,
which was downstream of the marina, settlement and rainfall were
highly correlated. However, at Marist College in Poughkeepsie,
which is far from any side embayment, no such correlation was
observed. This combined study of hydrodynamics and biology
illustrates the importance of sporadic hydrologic events such as
storms and local geometric features such as side embayments.
In August 2001 we conducted another dye study
to measure exchange between a side bay and the main channel.
This study, partially supported by the National Estuarine
Research Reserve System, occurred in North Tivoli Bay near
Annandale, NY. This bay has four main inlets and outlets: two
channels under railroad bridges that connect the bay directly to
the main channel, a small area on a peninsula between North and
South Tivoli Bays in which the bays exchange water at high tide,
and Stony Creek, which empties into the eastern part of the bay.
We measured the flow in Stony Creek, neglected the exchange
between the North and South Bays, and focused on the two
channels under the bridges. We injected 6 gallons of Rhodamine
WT at each bridge as the water started entering the bay (i.e.,
just after low tide), and we measured profiles of dye
concentration and water velocity across the cross-section. The
detailed measurements occurred over about one tidal cycle, and
continuously-recording fluorometers measured the dye
concentration over about 1.5 tidal cycles.
From these measurements, the inflow and
outflow of dye will be estimated, and a dye mass balance will be
evaluated. In particular, the fraction of dye leaving the bay
and the fraction of dye remaining in the bay can be estimated.
Results from one of the fluorometers allow for some preliminary
conclusions. If the dye cloud did not spread as it moved through
the channels in the bay, it would theoretically reappear at the
outlet after one tidal cycle. The fluorometer data show that dye
returns to the outlet after about half a tidal cycle, or almost
immediately after the tide turns. This observation suggests that
some of the dye is trapped in dead zones near the outlet.
Concentrations remained relatively high as the water left the
bay. After the tide turned again, significant dye concentrations
were recorded over only about one hour. Thus, once the dye (or
larval cohort) enters the main channel, not much appears to
return to the bay. After fully analyzing the results of this dye
study, we hope to construct a mathematical model of the mixing
and exchange in this bay.
Brief Summary: This project seeks to reduce the
destructive effects of zebra mussels by determining how they are
transported in rivers and estuaries. Because a patch of mussels
cannot sustain itself without a constant supply of larvae, the
number of zebra mussels in an entire river can be drastically
reduced if the larval supply can be blocked. For example, the U.
S. Army Corps of Engineers is designing a barrier to be placed
in the Chicago waterways to reduce the number of larvae that
enter the Illinois River from Lake Michigan. The success of this
and other control measures depends on the details of the river
flow and the biology of the zebra mussel. In the Illinois River,
zebra mussels may be able to establish local populations in
areas with low flow, like backwater lakes and areas behind locks
and dams. In the Hudson River, which has significant tidal
effects over much of its length, larvae may simply oscillate
around the spot where they were spawned. The goal of this
project is to understand the interaction between the physics of
the river flow and the biology of the zebra mussel so that
control schemes can be designed and evaluated.
We have used our previous field measurements
of larval abundance and size from the Illinois River to
determine the spread of a cloud or cohort of larvae as it moves
downstream, the larval death rate, and the rate at which they
settle out of the flow. This information is critical for
predicting the spread and establishment of zebra mussel
populations; by knowing how quickly they die and when they
settle, we can predict the location and size of mussel patches.
To determine where larvae might travel in the Hudson River, we
performed two experiments in which we tracked the spread of a
non-toxic, fluorescent dye. These studies allowed us to evaluate
the ability of side bays to act as refuges for zebra mussel
larvae. If adult mussels can live in side bays and serve as
sources of larvae for the rest of the river, then a single
dispersal barrier upstream would be relatively ineffective at
controlling zebra mussels.
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