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The advanced stage of flow is described approximately by a steady velocity field.
A non-steady pattern of rupture bands is shown to develop from the discharge outlet towards the traction-free boundary of the material in the initial stage of flow.
Key geometric design factors of the flow channel are investigated regarding the effect to the development of a symmetric velocity profile after the flow channel bifurcation, as the symmetric velocity profile is critical to the even split of the flow into two streams in the next stage of flow channel bifurcation.
At this stage of flow clustering, these differing flows of Zeus are expected to get separated into different clusters.
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It was also found that the geographical location has a greater impact on major ion ratios than does the stage of stream flow.
For example, McDougall and Hungr (2004) developed an SPH model combined with depth-integrated equations to simulate the propagation stage of flow-like landslides.
Four axial stages of flow development were distinguished based on radial distributions of particle velocity and concentration.
But during the 1931-1940 period the average seasonal diversion rate for the section was only 2 acre feet, since in low stages of flow some of the ditches are unable to divert any water.
The results show that multiple stages of flow distribution can achieve an evenly distributed pressure drop with an ideal distribution of reactant among channels.
Rapids, similar formations that show white water at all stages of flow, are common in bedrock channels, are generally composed of boulders, and are more random in distribution along the channel.
The sedimentary facies and facies associations show a downflow trend that can be subdivided into three distinct stages of flow development: (1) a zone of flow establishment (ZFE), (2) a zone of transition (ZFT), and (3) an established zone (ZEF).
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