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Variation of horizontal velocity with depth calculated from Eq. (10). assuming
uniform temperature and n = 3, compared with four measured velocity profiles.
ms - u = 2A(pg sin a)"y"H/(n + 1) (10) where A and n are the flow law parameters,
A method based on the generalized flow law [Eqs. (3) and (4)] has to be used. As
a result, shear can be either more or less concentrated in the basal layers than
the simple theory predicts (Fig. 12). Simple models that lead to equations with ...
by each arc is the flow, and the second is the capacity. The net flow in this case is
4. A cut in a network D is a partition of the vertices V into two subsets S and 5 with
s & S and / e S. The capacity of the cut is the sum of the capacities of the edges ...
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Fusion Devices Explosive 1 Brij Agrawal
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