New model to determine forces at on-bottom slender pipelines
Abstract
The present paper proposes a numerical model to determine horizontal and vertical components of the hydrodynamic forces on a slender submarine pipeline lying at the sea bed and exposed to non-linearwaves plus a current. The new model is an extension of the Wake II type model, originally proposed for sinusoidal waves (Soedigdo et al., 1999) and for combined sinusoidalwaves and currents (Sabag et al., 2000), to the case of periodic or randomwaves, evenwith a superimposed current. TheWake II typemodel takes into account thewake effects on the kinematic field and the time variation of drag and lift hydrodynamic coefficients. The proposed extensionis based on an evolutional analysis carried out for each half period of the free stream horizontal velocity at the pipeline. An analytical expression of the wake velocity is developed starting from the Navier–Stokes and the boundary layer equations. The time variation of the drag and lift hydrodynamic coefficients is obtained using a Gaussian integration of the start-up function. A reduced scale laboratory investigation in a large wave flume has been conducted in order to calibrate the empirical parameters involved in the proposed model. Different wave and current conditions have been considered andmeasurements of free streamhorizontal velocities and dynamic pressures on a bottom-mounted pipeline have been conducted. The comparison between experimental and numerical hydrodynamic forces shows the accuracy of the new model in evaluating the time variation of peaks and phase shifts of the horizontal and vertical wave and current induced forces.
Autore Pugliese
Tutti gli autori
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Aristodemo F. , Tomasicchio G.R. , Veltri P.
Titolo volume/Rivista
COASTAL ENGINEERING
Anno di pubblicazione
2011
ISSN
0378-3839
ISBN
Non Disponibile
Numero di citazioni Wos
8
Ultimo Aggiornamento Citazioni
28/04/2018
Numero di citazioni Scopus
10
Ultimo Aggiornamento Citazioni
28/04/2018
Settori ERC
Non Disponibile
Codici ASJC
Non Disponibile
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