scholarly journals The new political scales of citizenship in a global area; the politics of hydroelectric development in the James Bay Region.

2000 ◽  
Author(s):  
Jean Rousseau
1984 ◽  
Vol 21 (2) ◽  
pp. 213-222 ◽  
Author(s):  
J. J. Paré ◽  
N. S. Verma ◽  
H. M. S. Keira ◽  
A. D. McConnell

The LG 4 dam, the second largest structure on the La Grande Complex of the James Bay hydroelectric development, is 125 m high, about 4 km long, and is composed of 19 × 106 m3 of fill materials.The design of the dam is characterised by (i) a zoned earth–rockfill section based on a judicious use of the limited quantities of various materials available, (ii) a 70 m high abutment in the river valley with a steep inclination of about 55°, and (iii) a 50 m high section of the dam with its axis curved in the downstream direction.Detailed stress-deformation analyses were carried out in the critical sections of the dam using finite element methods to verify any presence of arching and hydraulic fracturing potentials in the nonplastic till core. An interesting aspect of these analyses was the fact that the material properties were established based on laboratory testing as well as the observed deformation behaviour of the already completed 156 m high LG 2 main dam.The analyses have indicated that the design has adequate reserve of safety against hydraulic fracturing and arching. Nevertheless, the design sections and material placement requirements were optimised, where necessary, to ensure a satisfactory behaviour of the dam. The instrumentation design was also adapted to the findings of this study. Keywords: earth dam, steep abutment, stress-strain, hydraulic fracturing, arching.


1985 ◽  
Vol 42 (6) ◽  
pp. 1216-1221 ◽  
Author(s):  
R. Grant Ingram ◽  
Louis Legendre ◽  
Yvan Simard ◽  
Serge Lepage

Phytoplankton, nutrients, and hydrodynamic conditions were regularly sampled in the estuary of the Eastmain River (Québec) and offshore in James Bay, before and after the diversion of the river for hydroelectric development on 19 July 1980. In the estuary, mean flow decreased by over 90% and the semidiurnal tidal amplitude increased significantly over a 5-d period. The most dramatic event was a major phytoplankton bloom in the river mouth, during a 10-d period of higher water column stability in late August; the cells then remained and bloomed in the thin photic layer. This stresses the role of hydrodynamics (as determined here by the freshwater runoff) in the timing of phytoplankton blooms.


1984 ◽  
Vol 21 (1) ◽  
pp. 75-91
Author(s):  
J.-J. Paré ◽  
N. S. Verma ◽  
A. A. Loiselle ◽  
S. Pinzariu

The EOL (Eastmain – Opinaca – La Grande) diversion scheme of the La Grande Complex (phase I) for the James Bay Hydroelectric development in northern Québec diverts the waters of the Eastmain, Opinaca, and Petite Opinaca Rivers into the LG 2 reservoir. The EOL diversion consists of four dams and seven dykes about half of which are founded for part of their length on overburden foundations of variable thickness and consisting of heterogeneous deposits of glacial till or sandy and silty alluvia. The till core of these zoned embankments is either placed directly on the till strata or extended through the alluvia to the underlying till by a core trench. The construction of these embankments was completed in 1979 and the maximum reservoir level achieved in November 1980.This paper deals with the seepage and pore pressure behaviour in the overburden foundations, namely, dams OA-10B and OA-11 and the dyke OA-8B, during and subsequent to the reservoir filling. The results of the parametric seepage analyses carried out by finite element methods are compared with the observations. Special attempts are made to resolve the long-existing speculations regarding the anisotropy of natural deposits. Comments are made regarding the effective anisotropy of such deposits in the James Bay region and its effect on exit gradients and uplift forces, which influence the design and safety of dams and dykes. Keywords: seepage, pore pressure, hydraulic conductivity, anisotropy, foundation treatment, cutoff.


Planta Medica ◽  
2010 ◽  
Vol 76 (12) ◽  
Author(s):  
H Eid ◽  
A Brault ◽  
M Ouchfoun ◽  
F Thong ◽  
D Vallerand ◽  
...  

1977 ◽  
Vol 12 (1) ◽  
pp. 51-76
Author(s):  
B. Bobée ◽  
D. Cluis ◽  
A. Tessier

Abstract A water quality sampling programme for James Bay territory established in a previous study has been carried out for the Department of Natural Resources of the Province of Quebec. The network is composed of 5 base-stations, sampled every fortnight to determine the variability with time of the parameters and 16 satellite-stations, sampled five times yearly with a view to determine the spatial variability. The data (major ions and certain nutrients) gathered during the 1974–1975 field survey are subjected to an analysis by a multivariate technique (correspondence analysis) in addition to certain classical statistical methods. The latter have shown that the mean values obtained at satellite stations were representative of the annual mean. In addition, the results permit the determination for a given parameter, of the relationship between stations and, for a given station, the relationship between parameters. In both cases, the formulation of predictive equations was attempted. An overall evaluation of the data by correspondence analysis has permitted: - a more precise definition of the qualitative behaviour of the different sub-basins of the James Bay territory and characterization of their waters;- a proof of the existence of gradual concentration changes in both East-West and North-South directions. Within the original objectives of the network, the results of the study have led to the following recommendations: - to continue synchronised samplings;- to transform a base station with a low information content into a satellite station;- to create a new base station in the eastern part of the territory.


1991 ◽  
Author(s):  
S. F. Railsback ◽  
G. F. Cada ◽  
C. H. Petrich ◽  
M. J. Sale ◽  
J. A. Shaakir-Ali ◽  
...  

Polar Record ◽  
1976 ◽  
Vol 18 (113) ◽  
pp. 183-184 ◽  
Keyword(s):  

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