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dc.contributor.authorKarn, Asish-
dc.contributor.authorChawdhary, Saurabh-
dc.date.accessioned2023-07-20T05:22:32Z-
dc.date.available2023-07-20T05:22:32Z-
dc.date.issued2018-03-17-
dc.identifier.urihttps://doi.org/10.1016/j.ijmultiphaseflow.2018.03.015-
dc.identifier.urihttp://hdl.handle.net/123456789/4216-
dc.descriptionPaper published in the journal International Journal of Multiphase Flow, 104 (2018), Pp. 1-8en_US
dc.description.abstractA supercavity can be attained via two distinct routes: vaporous and ventilated supercavitation. A vaporous supercavity is one that is obtained by the coalescence of individual vapor bubbles formed by cavitation. On the other hand, a ventilated supercavity results from the coalescence of bubbles of non-condensable gas formed through gas injection at the rear part of the cavitator. A typical strategy of operation of a supercavitating underwater vehicle entails an interplay between these two modes viz. accelerating it to a high speed using ventilation, when a natural supercavity can be sustained. This fact necessitates a systematic study of the synergistic relationship between the process of supercavity formation under these two modes. Thus, in the current work, we have systematically carried out water tunnel experiments to study the effect of vaporous and ventilated modes of supercavitation on each other during supercavity formation. The results show a systematic dependence between the relevant parameters which include the formation natural cavitation number and the formation gas entrainment coefficient. Further, the effects of change in Froude number and blockage are also reported and discussed.en_US
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectPublished Papersen_US
dc.subjectMechanical Engineeringen_US
dc.subjectCavitationen_US
dc.subjectNatural Supercavitationen_US
dc.subjectArtificial Supercavitationen_US
dc.subjectGas Entrainmenten_US
dc.subjectVentilation Demanden_US
dc.subjectSupercavity Formationen_US
dc.titleOn the synergistic interrelation between supercavity formation through vaporous and ventilated routesen_US
dc.typeArticleen_US
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