It is noted that losses during flow along the surface is the basic form of loss in hydrocyclones. The special role of the axisymmetric frontal effect, which results in vigorous longitudinal circulation that transfers losses from the boundary layer to the core of the flow, is demonstrated. The velocity and pressure distribution along the radius is determined from the equality of the losses on the surface and in the core of the flow, but in the axial direction, it is determined on the basis of the principle of maximum flow rate. A model of the flow in the conical zone of a hydrocyclone, which makes it possible to determine the narrowing of the air column toward the vertex of the cone and the flow rate through the slime opening is created. An explanation is given for a number of anomalous hydrodynamic phenomena.
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Translated from Khimicheskoe i Neftegazovoe Mashinostroenie, No. 2, pp. 7–9, February, 2009.
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Khodus, V.V. Improving the accuracy of hydrocyclone analysis by accounting for transfer of hydrodynamic losses from the boundary layer to the core of the flow. Chem Petrol Eng 45, 63–68 (2009). https://doi.org/10.1007/s10556-009-9144-9
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DOI: https://doi.org/10.1007/s10556-009-9144-9