2010
DOI: 10.1007/s10652-010-9182-z
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3D numerical modelling of turbidity currents

Abstract: During floods, the density of river water usually increases due to a subsequent increase in the concentration of the suspended sediment that the river carries, causing the river to plunge underneath the free surface of a receiving water basin and form a turbidity current that continues to flow along the bottom. The study and understanding of such complex phenomena is of great importance, as they constitute one of the major mechanisms for suspended sediment transport from rivers into oceans, lakes or reservoirs… Show more

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Cited by 35 publications
(31 citation statements)
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“…This paper simulates a lock release density current at a Grashof number of 5 × 10 6 in two and three dimensions with a configuration similar to that of Necker et al (2002). The governing equations are well established and have been validated extensively against experimental data across a range of simulation configurations (Sequeiros et al, 2009;Necker et al, 2002;Espath et al, 2014;Huang et al, 2007;Georgoulas et al, 2010). This paper validates the use of novel computational methods, including unstructured mesh adaptivity and discontinuous finite elements, through convergence analyses and by direct comparison with the results from the previous models of Necker et al (2002) and Espath et al (2014), providing a framework for future modelling efforts of this type.…”
Section: S D Parkinson Et Al: Direct Numerical Simulations Of Partmentioning
confidence: 99%
“…This paper simulates a lock release density current at a Grashof number of 5 × 10 6 in two and three dimensions with a configuration similar to that of Necker et al (2002). The governing equations are well established and have been validated extensively against experimental data across a range of simulation configurations (Sequeiros et al, 2009;Necker et al, 2002;Espath et al, 2014;Huang et al, 2007;Georgoulas et al, 2010). This paper validates the use of novel computational methods, including unstructured mesh adaptivity and discontinuous finite elements, through convergence analyses and by direct comparison with the results from the previous models of Necker et al (2002) and Espath et al (2014), providing a framework for future modelling efforts of this type.…”
Section: S D Parkinson Et Al: Direct Numerical Simulations Of Partmentioning
confidence: 99%
“…The governing equations are solved sequentially using the control volume method. The equations and the solution procedure are presented and discussed in detail, in the work Georgoulas et al (2009). Therefore, due to space limitations, these equations are not presented here.…”
Section: Description Of Numerical Modelmentioning
confidence: 99%
“…lished laboratory experiments on hyperpycnal particulate currents, in the work of Georgoulas et al (2009). Finally, an additional series of numerical runs are conducted in order to further validate the numerical model, by checking its ability in capturing the critical suspended sediment concentration for the transition from hypopycnal to hyperpycnal particulate currents.…”
mentioning
confidence: 99%
“…However most of these previous works treat turbidity currents with a quasi-single-phase approach, solving one set of continuity and momentum equations for the ambient fluid and treating the transport of sediment particles through an advection-diffusion equation for sediment concentration. According to the authors' best knowledge, the first numerical effort that treats turbidity current flows through a multi-phase approach, assuming that the sediment-laden turbidity current flow consists of separate solid and fluid phases, is the recent work by Georgoulas et al (2010) [1]. In the proposed work a separate velocity field is calculated for each phase (water and sediment classes), since the laws for the conservation of mass and momentum are modified accordingly in order to be satisfied by each phase individually.…”
Section: Introductionmentioning
confidence: 99%
“…In the present paper, the multiphase numerical approach that is validated in the work of Georgoulas et al (2010) [1], is further applied in order to investigate the exact qualitative and quantitative effect of fundamental flow controlling parameters, such as bed slope and roughness, initial suspended sediment concentration and diameter, in the hydrodynamic and depositional characteristics of continuous, high density turbidity currents. For this purpose, four different series of parametric numerical experiments are conducted, using a laboratory scale experimental set-up, similar to the one used in the laboratory experiments of Baas et al (2004) [12].…”
Section: Introductionmentioning
confidence: 99%