Modelling Produced Water Transport and Mixing with a Lagrangian Particle Model
Abstract:
Using a Lagrangian particle model, we investigate the effects of flow field resolution and sub-grid turbulent mixing parametrisation on produced water dispersion. We consider a simplified produced water discharge, modelled as a non-degradable tracer, discharged from a point source off the coast of mid-Norway, and advected with ocean model currents at two different resolutions (800 m and 4 km), during two different seasons (winter and spring).
The reconstructed tracer concentrations from the Lagrangian model are compared with predictions from an Eulerian grid model. In general, the models are in reasonable agreement, with the Lagrangian predictions tending to drift further from the Eulerian over time. We find a significant difference in tracer distribution and concentrations between the two model resolutions, and to a lesser extent between seasons; additionally, the 800 m model has less mixing towards the coast than the 4 km in the spring scenario.