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Environmental Monitoring of La Grande-2-A and La Grande-1 Projects. Danielle Messier McGill University, 2003-09-25. La Grande Complex. Context of the monitoring. Required by the certificates of authorization of projects constructed during phase II of the La Grande Complex - PowerPoint PPT Presentation
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Environmental Monitoring of La Grande-2-A and La Grande-1
Projects
Danielle Messier
McGill University, 2003-09-25
La Grande Complex
Context of the monitoring
• Required by the certificates of authorization of projects constructed during phase II of the La Grande Complex
• Section 22 of the James Bay and Northern Québec Agreement (1975)
The projects on the Grande Rivière
• Addition of La Grande-2A underground generating station beside Robert-Bourassa's (PK 112)
• Construction of La Grande-1 run-of-river generating station (PK 37)
Sources of modifications
• Increase of the designed flow from 4300 m3/s to 5920 m3/s– Changes in the production pattern: increase
flow in winter time, decrease in summer time
• Creation of La Grande-1 reservoir – Area of 70 km2
• Operation of La Grande-1 generating station
Objectives of the monitoring
• To verify the actual modifications of the environment following impact assessment study
• To detect unpredicted impacts and take action to avoid or mitigate them
• To enhance impact assessment and mitigation measures
Criteria used for the monitoring
• Components of the monitoring program must reflect the changes
• Changes must be measurable
• Methods must be accepted
• Changes must be beyond natural variability
Components of the monitoring
• Hydrology – discharge, water level,
temperature, current
• Erosion of river banks• Water quality• Riparian and aquatic
vegetation• Fish• Mercury in fish• Underice freshwater
plume• Eelgrass
Main periods of the monitoring
• Reference period : 1985-1990
• Transitory period : 1991-1992
• Monitoring period : 1992-2000
Modifications of the discharge
Hydraulic Modifications downstream from La Grande-1Phase I Phase II
Mean annual variation of water level : 4,7 m
Mean annual variation of water level : 4,0 m
Mean current : 0,90 m/s Mean current : 1 - 2 m/s
Summer temp.: 8–12 °C
Winter temp.: near 0°C
Summer temp.: 8–14 °C
Winter temp.: 0–0,15 °C
Thin ice cover;(air temperature and discharge)
Many openings
River banks erosion
Transitory : 1991-1993 Exploitation : 1997-1999
Upstream LG-1:
500 000 m3 material eroded
Upstream LG-1
200 000 m3 material eroded
Downstream LG-1:
100 000 m3 material eroded
Downstream LG-1:
75 000 m3
Construction of protection structures
River banks erosion
• The Grande Rivière is enlarging to adapt to increased mean annual discharge
• 3 large landslides occurred :– 3.5 M m3 in 1987– 1.5 M m3 in 1989– > 1 M m3 in 2003
Fish Communities
• Few changes in the fish communities of La Grande-1 reservoir and estuary
• No transfer of fish between Grande Rivière and other tributaries of James Bay
Mercury in fish
• Impoundment of La Grande-1 reservoir did not change mercury concentrations in fish
• The effect of the Grande Rivière on James Bay fish is restricted to the summer plume area
22HQme0901
23HQme0901
The freshwater underice plume
• Increasing the discharge from 1700 m3/s to more than 4400 m3/s extends the plume area from 1600 km2 to 2100 km2 or 3500 km2, depending on ice conditions
The La Grande plume in 1995
Eelgrass in James Bay
• General distribution of eelgrass beds in James Bay shows high stability from 1986-87 up to 1996
• Massive decline in 1998-1999 along James and Hudson Bays, due to wasting disease
Production of eelgrass
• Data from 1988 to 2000• High annual variation at
all stations and all depths• Meterological conditions
are responsible for annual variations
• Isostatic uplift causes long term disappearance in shallow waters
Variation in eelgrass production
Variation in salt marshes
• 10 permanent stations from 1991 to 1999
• Vegetation changes under isostatic uplift
• Noticeable expanses of vegetation
Changes in salt marshes
Conclusions
• Most environmental changes in the Grande Rivière were observed during phase I
• Commissioning of La Grande-2A and La Grande-1 generating stations did not generate cumulative effects
• The main changes are direct hydrological conditions, including the increase of the freshwater underice plume