Non-equilibrium processes in ash-laden volcanic plumes: new insights from 3D multiphase flow simulations
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Weak and strong plumes are simulated in 3D with a non-equilibrium gas–particle model.

Multiphase effects have a secondary role in the analysed large-scale plume dynamics.

Integral model assumptions and the entrainment hypothesis hold for weak plumes.

In the strong plume case, a supersonic fountaining structure is formed.

Atmospheric stratification hinders the achievement of self-similarity.

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