Conclusions
-
1.
Relation (8) was established, according to which the coefficient of aeration of a rapid uniform flow (coefficient of stabilized aeration), regardless of the roughess of the bed, is uniquely determined by the measure of the dissipation of specific energy — its gradient (I).
-
2.
Relation (15), being a more accurate realization than (4) of relation (8) for cross sections bounded by a conditional free surface with a local value of the water saturation coefficient βloc=0.01−0.02 (a loc=0.99−0.98), was developed. Relation (15) is recommended for engineering calculations in the entire practical range.
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3.
The establishment of relation (8) clears up the problem of modeling the phenomenon of stabilized aeration in prismatic channels, reducing it to the condition I=idem, with simultaneous provision of the necessary path length of stabilization.
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4.
Relation (6) does not correspond to the actual data on aeration of rapid flows.
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Translated from Gidrotekhnicheskoe Stroitel'stvo, No. 12, pp. 33–40, December, 1986.
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Aivazyan, O.M. Stabilized aeration on chutes. Hydrotechnical Construction 20, 713–722 (1986). https://doi.org/10.1007/BF01425070
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DOI: https://doi.org/10.1007/BF01425070