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) were a function of parameters of Fr1, S and the relative distance from the beginning of the basin (X/Y1). The results showed that the maximum values of Cʹp < /sub> coefficient for the Type II stilling basin decreased around 30% compared to the smooth basins. The mean values of Cʹp < /sub> in submerged jumps decreased around 25% compared to the free jumps at the downstream zone of the stilling basin (X/Y1>10).]]>
p. 15−29
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p. 31−45
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p. 47−58
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p. 59−73
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p. 75−89
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p. 91−102
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