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Research
Objectives
Based on initial field sampling in 2002, researchers from both the National
Water Research Institute (NWRI) and the University of Waterloo carried
out intensive field work in the summer of 2003 to address the following:
- The distribution
of Cladophora on the north shore of Western Lake Ontario and
determine if point sources of nutrients are associated with high Cladophora
production
- The importance
of watershed point vs. non-point sources of nutrients for Cladophora
growth and if hydrodynamic processes deliver higher nutrient levels
to Cladophora in nearshore waters
- The role of
ambient nutrient
levels in controlling growth
Using
the field sampling data, the approach for 2004 focused on:
- Predictability
- implementing existing Cladophora growth models, tracking
historical changes, and developing rapid assessment tools
- Management - using
a validated Cladophora growth model to predict the outcomes
of possible management interventions to identify the most cost effective
means of reducing Cladophora biomass
Key Research Findings
Role of Phosphorus
(P)
In 2002, "hot
spots" in both biomass and P were identified. This reinforces
the role for P in Cladophora biomass as identified in the 1960s
and 1970s. It was difficult to establish clear relationships between high
P concentrations and point sources of nutrients.
Point vs. Non–Point
Sources
In 2003,
three
locations were chosen to represent point sources of nutrients: a river,
an outfall and an unimpacted (control) site. For each of the locations,
8 sampling sites at distances of 0 to 2 km west of each location along
the nearshore and at depths within the water column of 2 and 5m were selected
and sampled for water chemistry and plant tissue on a biweekly basis starting
in May.
Results indicated
that on average the Soluble
Reactive Phosphorus (SRP) concentrations (the type of phosphorus in
the water that is in the right form for plants and algae to use) was highest
at the river and outfall sites. As one moved away from the river or outfall
sites, the concentrations of SRP decreased. No noticeable change was noted
with distance from the unimpacted (control) site. Total Phosphorus levels
showed a similar trend.
Levels of phosphorus
found in the plant tissue (tissue P) were found to be higher in the river
and outfall sites samples but did not decrease with distance from the
sites as SRP did, however, seasonal differences in tissue P were noted.
Predictive models indicate that Cladophora seems to be less limited
by P early in the growing season. It then experiences some nutrient stress
during the summer and then rebounds in late August. These differences
may be due to environmental factors influencing P delivery to the plants.
Cladophora
growth along the north shore
A large scale west
to east survey of the north shore was conducted from late July to
early August of 2003 with 15 sites sampled at depths of 2, 5, 8 &
10 m for total phosphorus (TP), tissue P and when applicable an underwater
video was recorded.
On average the 2 m
sites showed higher levels of TP in the water than the deeper sites. There
was an overall increase in TP, and tissue P, as you moved from west
to east which may be the result of the greater urbanization and associated
surface runoff as you move towards Toronto. 3 noticeable hotspots were
found that displayed significantly higher TP concentrations than the other
sampled sites. An in-depth look at these sites is underway to determine
the specific source of the TP.
Cooperative research
with stakeholders in the Halton Region found that stormwater outfalls
are a major source of TP to the nearshore zone.
Role of Storm Water
Runoff
Non-point
sources of nutrients also contribute to measurable concentrations of nutrients
in lake waters. However, their relative contribution and role in plant
growth remains unclear. Water and plant Phosphorus concentrations were
measured following a three-day rainstorm event. Surges in both parameters
relative to pre-event levels were detected. This suggests that ephemeral
peaks in nutrients, particularly Phosphorus, may sustain Cladophora
growth rates even though ambient background levels of nutrients are relatively
low.
Nutrients in the
Nearshore Waters
The physical
stratification of the lake can also play a role in algae growth early
in the season. In the spring, water temperature increases most rapidly
in shallow areas along the shorelines of the lake. As the season progresses,
a band of warm, less dense water forms along the shore, creating a ‘thermal
bar’ separating the nearshore zone from the dense cool offshore
water. The difference in the densities of the water in these zones prevents
them from mixing. As a result, nutrients from point and non-point sources
remain trapped in the nearshore area and are readily available to Cladophora
early in the season. This "thermal bar" gradually expands towards
the centre of the lake until the lake becomes thermally stratified.
In 2002, the evolution
of the thermal bar in Lake Ontario was intensively studied. This work,
funded by the OWWRC has enhanced earlier research on the function and
formation of the thermal bar.
Other Contributing Factors
Other factors that may be contributing to the recent increase of biomass
are the invasion of zebra mussels and climate change. The hypothesis for
the role of mussels is that they increase P in the near shore waters through
their filtering action. Moreover, they increase water clarity by removing
suspended particles and may allow Cladophora to grow in deeper
water.
Climate change may
be leading to more severe summer rainstorms, with resulting impacts on
non-point sources of P. Alternatively, if there are warmer springs Cladophora
growth would increase.
Under Water Videography,
Biosonics and Artificial Substrates
Experiments
using under water videography, biosonics and artificial substrates constructed
of ceramic
tiles and floats were conducted to determine the extent of offshore
algal growth. The biosonics experiment revealed extensive growth of Cladophora
in shallow water (25-50 cm) and copius growth at 5m. Although mussels
were mostly found at 10m and 15m, Cladophora growth was still
evident.
Artificial substrates
were installed off
Coronation Park east of Bronte. Water depth over tiles was the same
at all stations. This experiment revealed more Cladophora
growth on inshore tiles than offshore tiles. In addition, Phosphorus
content of algae tended to be higher at stations situated nearest to the
shore.
Growth Models
Numerical
models have been developed to predict Cladophora growth and biomass
accumulation in Lake Erie. Once they have been calibrated and verified
with historical data from Lake Ontario, the models can be applied to recent
data to predict current Cladophora growth rates. Among
the most important model inputs are solar irradiance, water turbidity,
water temperature and TP concentrations in the water column.
Tracking Historical
Changes
Estimated
annual and seasonal TP loadings to the nearshore are based on historical
sewage treatment plant effluent discharges, storm sewer contributions,
river data and nearshore modeling of dilution rates. Historical reconstructions
of loadings are necessary to assess if TP loadings to the Lake are changing
over the long-term and if these changes are driving increased Cladophora
growth. This project is using data from municipal and provincial agencies
as well as modeling to determine the extent to which each of the sources
of P contributes to nuisance growth of Cladophora.
Using Rapid Assessment
Tools To Predict Growth
Preliminary
experiments were undertaken in 2004 to develop a rapid assessment tool
that can predict differences in potential growth rates of Cladophora.
These experiments assessed how changes in light and temperature affect
the response of Cladophora to TP and tested if these responses
can be rapidly measured in the field.
Management
Of the key
variables influencing Cladophora growth - light, temperature
and TP concentrations - TP concentration is the only factor that can be
locally managed. Analysis of concentrations measured 2002 and 2003 suggests
that while Cladophora growing at some sites would likely respond
to small reductions in TP concentration, Cladophora in many areas
will require more dramatic reductions before changes in growth rates and,
therefore, biomass accumulation are noticeable.
Currently, it is unclear
what species of Cladophora predominates or if there are multiple
species present in the western basin of Lake Ontario. Sample differences
have been seen in the branching
pattern of Cladophora plants taken from Oakville (Dingle
Park) and from Pickering (OPG Pickering plant). This has clear management
implications as different species are likely to differ in their environmental
requirements, includig P needs. Researchers at the University of Waterloo
continue to address this issue in the laboratory.
Research conducted
in 2003 showed that sites near point sources of nutirents have higher
water column TP concentrations and higher plant tissue P concentrations
than unimpacted sites. Analyses of samples taken at 16 sites at various
distances from the mouth of Cooksville Creek in 2004 indicate that storm
events can significantly increase local concentrations of TP and, thus,
storm water discharges have to be considered in developing management
strategies.
2005-2006 Research
Plan
The factors influencing
Cladophora growth are complex. Increased emphasis on modelling,
with extensive ground proofing, should help to understand these factors
in the future.
- Isolation and cultivation
of Cladophora samples from Lake Ontario to determine if variations
in phosphorus, light and temperature requirements exist between isolates
- Analysis of historical
data to better understand wastewater treatment plant discharges, river
and storm water loadings to determine their contribution to making P
available for Cladophora growth
- Biological/hydrodynamic
modeling of TP concentrations and Cladophora growth in nearshore
waters
- Compilation and
interpretation of 2002-2005 field data
- Completion of a
final report encompassing the 2002-2006 research efforts and final recommendations
for possible management action

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