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April 2014 CFD techniques for mixing and dispersion of desalination and other marine discharges ICDEMOS, Muscat, Sultanate of Oman, 2014 David Robinson, Matthew Wood, Matthew Piggott & Gerard Gorman
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April 2014

CFD techniques for mixing and dispersion of desalination and other marine discharges

ICDEMOS, Muscat, Sultanate of Oman, 2014

David Robinson, Matthew Wood, Matthew Piggott & Gerard Gorman

© HR Wallingford 2014

Content

Background and motivation CFD: a tool for dispersion modelling Preliminary results Planned work

April 2014

© HR Wallingford 2014

Motivation

Desal / IWPP discharge plumes Benthic thermal-saline impact Dispersion prediction is vital for: EIA Engineering studies (outfall design, recirculation)

April 2014

© HR Wallingford 2014

HR Wallingford in Oman

April 2014

© HR Wallingford 2014

Far-field dispersion

Model coupling

Near-field dilution

(mixing zone)

Dispersion modelling approaches

April 2014

© HR Wallingford 2014

Validated procedure

April 2014

Coupled studies are common

HR Wallingford framework: “Dense Jet Assessment Procedure”, Wood & Mead (2008)

Validated against newly available mid-/far-field data: “Validation of computational models for hypersaline and other dense marine discharges”, Wood et al, (2014)

© HR Wallingford 2014

Benefits & drawbacks

Benefits: Methods generally work well for smaller discharges:

Simple exchanges of mass & momentum Relatively quick to implement

Drawbacks Plume interactions / neighbouring facilities :

2-way exchange of pollutant concentrations is challenging

Potential solution: CFD Computing power increases Adaptive meshing techniques Seamless coverage of the entire domain

April 2014

Barka

Sohar

© HR Wallingford 2014

CFD

History – near-field Fluidity:

Open-source, developed by Imperial Navier-Stokes on 3D unstructured meshes Discretisation: Finite element & control volume Mesh adaptivity

Key differentiator – multi-scale:

3D CFD model + efficient coastal flow modelling system

Used to simulate ocean and tidal flows

April 2014

© HR Wallingford 2014

PhD research

Long-term goals: Extend Fluidity’s multi-scale capabilities a fully integrated CFD hydrodynamic & pollutant dispersion model

First stage: Explore near-field abilities

Horizontal buoyant jet Angled dense jet

Compared predictions with published laboratory data, or validated integral models.

April 2014

© HR Wallingford 2014

Near-field test cases

April 2014

Parameter Horizontal buoyant jet Angled dense jet

Inlet diameter (mm) 9.4 3.3 Densimetric Froude number, F 10.7 21.3 Reynolds number 6000 2500 References for comparison CorJet integral model Experimental data

Parameters for comparison • Centreline trajectory • Mean axial velocity decay

• Centreline terminal rise height • Bottom impact distance • Minimum impact dilution

Zt

Si Xi

© HR Wallingford 2014

Numerical methods

Unstructured tetrahedral elements Turbulence:

k-ε V-LES

Adaptive time-stepping and meshing

April 2014

© HR Wallingford 2014

Horizontal buoyant jet

April 2014

© HR Wallingford 2014

Horizontal buoyant jet

April 2014

Centreline trajectory

Centreline velocity decay

© HR Wallingford 2014

Angled dense jet

April 2014

© HR Wallingford 2014

Angled dense jet

April 2014

k1 = zt/dF k2 = xi/dF k3 = Si/F Zeitoun et al. (1972) - 3.19 1.12 Roberts et al. (1997) - 2.4 1.6 +/- 0.12 Nemlioglu & Roberts (2006) - 3.25 1.7 Cipollina et al. (2005) 1.77 2.25 - Kikkert et al. (2007) 1.6 2.72 1.81 Papakonstantis et al. (2011a and 2011b) 1.68 2.75 1.68 +/- 0.1

Terminal rise

height

Impact distance

Impact dilution

© HR Wallingford 2014

Summary

HR Wallingford uses a validated coupled modelling procedure involving Hydrodynamic models Near-field models

Future will involve more CFD

Preliminary work with Imperial College is encouraging:

Buoyant jet compares well (trajectories and dilutions) Dense case requires mesh refinement

Next steps of PhD: Adapt mesh to far-field Range of ambient currents Multiport diffusers

April 2014

© HR Wallingford 2014

Thank you!

Matthew Wood Principal Scientist HR Wallingford [email protected]

David Robinson Imperial College London [email protected]

January 2014 Page 17


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