2007Shuitu baochi yanjiuRequires access

The Forecast Methods for the Range of Atomized Flow Caused by the Jet Overflow

Li Hu

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Abstract

Trajectory energy dissipation,as one of main dissipation ways of hydropower stations that locate in deep valleys and with high water head and large discharge capacity,is much effective.But discharge atomization causing from trajectory energy dissipation is often serious and has badly impact on the structures of hinge and downstream rock slope stability,which is arousing attention of the community,so there is a need for the research about the atomized flow.The forecast methods to calculate the range of atomized flow caused by the trajectory energy dissipation is presented.

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Trajectory energy dissipation,as one of main dissipation ways of hydropower stations that locate in deep valleys and with high water head and large discharge capacity,is much effective.But discharge atomization causing from trajectory energy dissipation is often serious and has badly impact on the structures of hinge and downstream rock slope stability,which is arousing attention of the community,so there is a need for the research about the atomized flow.The forecast methods to calculate the range of atomized flow caused by the trajectory energy dissipation is presented.

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Available abstract

Trajectory energy dissipation,as one of main dissipation ways of hydropower stations that locate in deep valleys and with high water head and large discharge capacity,is much effective.But discharge atomization causing from trajectory energy dissipation is often serious and has badly impact on the structures of hinge and downstream rock slope stability,which is arousing attention of the community,so there is a need for the research about the atomized flow.The forecast methods to calculate the range of atomized flow caused by the trajectory energy dissipation is presented.

Key concepts: Dissipation, Hydropower, Trajectory, Range (aeronautics), Flow (mathematics), Mechanics, Jet (fluid), Environmental science

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