The main purpose of this study is to investigate the turbulence characteristics of a non-buoyant jet discharged vertically in steady conditions and beneath a regular wave field. A LDA system was developed to measure simultaneously the two dimensional velocity field. The turbulent micro and integral scales were determined at different cross sections. The results show that the production of turbulent kinetic energy is primarily used for dissipation and secondarily to increase the turbulent kinetic energy of the entrained mass for jets in a stagnant ambient or in a wave environment. This balance is different from the one of immiscible flows. The characteristic behaviour of turbulence is closely related to entrainment, which may be vortex-generated (jet, plume, etc.) or cusp-generated (free surface buoyant flow, dense bottom current, etc.).
Turbulent energy transport of a jet in stagnant or wave environment / Mossa, Michele; Petrillo, Antonio Felice (WATER FOR A CHANGING GLOBAL COMMUNITY). - In: Environmental and coastal hydraulics : protecting the aquatic habitat. Volume B / [a cura di] S S Y Wang; T Carstens. - STAMPA. - New York, NY : ASCE, 1997. - ISBN 0-7844-0272-8. - pp. 173-178
Turbulent energy transport of a jet in stagnant or wave environment
Mossa, Michele;Petrillo, Antonio Felice
1997-01-01
Abstract
The main purpose of this study is to investigate the turbulence characteristics of a non-buoyant jet discharged vertically in steady conditions and beneath a regular wave field. A LDA system was developed to measure simultaneously the two dimensional velocity field. The turbulent micro and integral scales were determined at different cross sections. The results show that the production of turbulent kinetic energy is primarily used for dissipation and secondarily to increase the turbulent kinetic energy of the entrained mass for jets in a stagnant ambient or in a wave environment. This balance is different from the one of immiscible flows. The characteristic behaviour of turbulence is closely related to entrainment, which may be vortex-generated (jet, plume, etc.) or cusp-generated (free surface buoyant flow, dense bottom current, etc.).I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.