A Numerical Investigation of the Dynamic Interaction between the Deep-Sea Mining Vehicle and Sediment Plumes Based on a Small-Scale Analysis

• Published in: Journal of marine science and engineering 2023-07, Vol.11 (7), p.1458
• Main Authors: Liu, Shihang, Yang, Jianmin, Lu, Haining, Sun, Pengfei, Zhang, Bei
• Format: Article
• Language: English
• Subjects: Analysis; Deep sea environments; Deep sea mining; Deep water; deep-sea mining (DSM); Discharge; discrete phase model (DPM); Ecological monitoring; Emissions; Evolution; Investigations; Lateral diffusion; Marine geography; Mechanics; Mineral reserves; Mineral resources; Numerical analysis; Oceanography; Particle trajectories; Physical oceanography; Plumes; Plumes (Fluid dynamics); Sediment; Sediment concentration; sediment concentration and particle trajectories; Sediment transport; Sediments (Geology); Sustainable design; Turbulence models; Vehicles; Velocity
• ISSN: 2077-1312; 2077-1312
• DOI: 10.3390/jmse11071458

The discharge of sediment plumes, which occurs mainly in the two depth zones, has a critical impact on assessing the deep-sea environment. Therefore, it is necessary to establish the corresponding physical oceanography for the evolution of these sediment plumes. For a more accurate evolution estimation of the plumes, the model in this research is concerned with the dynamic interaction between the deep-sea mining vehicle (DSMV) and the sediment plumes on small scales (t ≤ 2 s), contributing to a focus on the vital physical mechanics of controlling the extent of these plumes. The sediment concentration and particle trajectories of the plume emissions were determined using the Lagrangian discrete phase model (DPM). The results show that (1) the wake structure of the DSMV wraps the plume vortex discharged from the rear of the vehicle and inhibits the lateral diffusion of the plume, (2) the length of the entire wake (Lw) increases exponentially as the relative discharge velocity of the plume (U*) increases, where U* is defined as the dimensionless difference between the traveling velocity of the DSMV and the discharge velocity of the plume, and (3) at the same traveling speed of the DSMV and U* less than 0.75, the dispersion of the sediment particles in the early discharge stage of the plume does not vary with the plume discharge rate. This will be beneficial for the more accurate monitoring of ecological changes in deep-sea mining activities and provide theoretical guidance for the green design of DSMVs.