arXiv subjects

Lianzheng Cui

Publications and source records attributed to Lianzheng Cui.

3 recordsLinked to original sources

arXiv2026

Particle settling in turbidity currents: inertia-independent biased sampling

We investigate the mechanisms governing particle settling in turbidity currents using Eulerian-Lagrangian direct numerical simulations. The Eulerian carrier flow is driven either by solutal buoyancy or particle feedback, with the Lagrangian phase comprising passive tracers or inertial particles, respectively. The effective particle settling velocity is decomposed into a fluid velocity sampled at particle positions and a particle-fluid slip velocity. The Eulerian mean profiles of these velocities are obtained using a concentration-weighted average of the coarse-grained fields. The mean sampled fluid velocity is shown to be approximately equal to the ratio of the vertical turbulent flux of particles to their mean concentration and reflects biased sampling of upward turbulent fluctuations at particle positions, despite the zero Eulerian mean vertical fluid velocity. The passive-tracer cases show that the upward bias is inertia-independent and arises from turbulent transport acting on concentration gradients, as it persists for inhomogeneous tracer seeding but disappears under uniform seeding. For the weakly inertial regime considered here, the upward bias dominates downward-directed biases associated with particle inertia. The mean slip velocity is well approximated by the terminal settling velocity predicted for a quiescent fluid. This is consistent with a leading-order balance between buoyancy and drag in the slope-normal direction. Modelling the sampled fluid velocity from the turbulent flux and using the slip-velocity approximation yield an Eulerian prediction for the settling velocity, in good agreement with the simulation data for the dilute, weakly inertial particles considered here.

physics.flu-dyn↗

arXiv2026

Intermittent turbulence in inclined gravity currents

Inclined gravity currents on shallow slopes can exhibit pronounced turbulence intermittency. Using direct numerical simulations, we investigate this behaviour for a temporal gravity current over a range of initial Reynolds numbers $Re_0$. For $Re_0=2500$ and a slope angle of $0.5^\circ$, the outer layer of the current exhibits large excursions in turbulence intensity and repeated transitions between turbulent and weakly turbulent states. Analysis of the flow energetics reveals that the intermittency is associated with a finite delay between shear production and dissipation of turbulent kinetic energy. During transitional phases, this delay permits a transient amplification of turbulence, which significantly weakens the mean shear by extracting kinetic energy from the mean flow and promoting entrainment-driven layer growth, ultimately leading to relaminarisation. Increasing $Re_0$ reduces the delay and progressively suppresses intermittency, steering the flow towards a more sustained turbulent state. Motivated by these observations, we develop an autonomous delay-differential model based on the coupled evolution of the mean and turbulent kinetic energies. The model reproduces the observed transition from intermittent to sustained turbulence as the delay is reduced and predicts an increased tendency towards intermittency at larger flux Richardson numbers. The results support an interpretation of intermittent turbulence in inclined gravity currents as a delay-induced oscillation arising from the finite adjustment time of turbulence to changes in the mean flow.

physics.flu-dyn↗

arXiv2025

Structure and scaling of inclined gravity currents

We explore the fundamental flow structure of inclined gravity currents with direct numerical simulations. A velocity maximum naturally divides the current into inner and outer shear layers, which are weakly coupled by exchange of momentum and buoyancy on timescales that are much longer than the typical timescale characterizing either layer. The outer layer evolves to a self-similar regime with flow parameters taking constant characteristic values. The flow behaviour in the outer layer is consistent with that found in a current on a free-slip slope by van Reeuwijk et al. ($\textit{J. Fluid Mech.}$, vol. 873, 2019, pp. 786-815), and the integral buoyancy forcing in the layer is balanced solely by entrainment drag. The inner layer evolves to a quasi-steady state, in which the buoyancy forcing is approximately balanced by wall drag. The inner layer can be further decomposed into viscous and turbulent wall regions that have much in common with fully developed open channel flow. Using scaling laws within each layer and a matching condition at the velocity maximum, we solve the entire flow system as a function of slope angle $α$, in good agreement with the simulation data. We further derive an entrainment law from the solution, which exhibits relatively high accuracy across a wide range of Richardson numbers and provides new insights into the long-runout of oceanographic gravity currents on mild slopes.

physics.flu-dyn↗