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9. Reservoir Problems
Pages 272-277

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From page 272...
... The Vaiont reservoir slide is a spectacular and catastrophic example (see Figure 9-1~. These movements can be initiated by changes in the piezometric conditions within the mass as a result of reservoir loading, saturation of soil and weak rock materials with a resulting lowering of the internal coefficient of friction, erosion and subsequent undercutting of large earth masses by wave action and reservoir operations (raising and lowering)
From page 273...
... Increases in the siltation of a reservoir, whether from slide materials or normal sedimentation processes, can reduce the reservoir capacity to store floods. As a result overtopping can occur if such reduced storage capacity has not been considered in the dam and spillway design.
From page 274...
... g., the weight of the reservoir may increase stresses at epicentral depths sufficiently to trigger fault activity (there is little to support this thesis) , the downward movement of reservoir water may increase hydrostatic pressures in the rock masses (this increase presumably would increase pressure on a fault plane that may be under a critical state of strain)
From page 275...
... ICE The development of an ice layer on a reservoir surface can cause structural damage and produce maintenance difficulties. The main damage is commonly from the impact of ice against thin-walled structures such as parapets on masonry dams.
From page 276...
... Ice can also block spillway control structures, particularly gated ones, thereby reducing the spillway capacity, raising the water level, or resulting in a sudden water surge when the ice finally breaks loose. A number of empirical formulas have been proposed for calculating ice loads on a dam.
From page 277...
... The latter is important because the rate of temperature rise and its duration can determine the pressure likely to be exerted. Figure 9-2 compares ice pressure with ice thickness and considers whether the reservoir banks act as a restraint.


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