### Abstract

Original language | English |
---|---|

Pages (from-to) | 176-180 |

Number of pages | 5 |

Journal | International journal of multiphase flow |

Volume | 80 |

DOIs | |

Publication status | Published - 2016 |

### Fingerprint

### Keywords

- METIS-318156
- IR-101775

### Cite this

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*International journal of multiphase flow*, vol. 80, pp. 176-180. https://doi.org/10.1016/j.ijmultiphaseflow.2015.12.009

**On flux terms in volume averaging.** / Chu, S.G.; Prosperetti, Andrea.

Research output: Contribution to journal › Article › Academic › peer-review

TY - JOUR

T1 - On flux terms in volume averaging

AU - Chu, S.G.

AU - Prosperetti, Andrea

PY - 2016

Y1 - 2016

N2 - This note examines the modeling of non-convective fluxes (e.g., stress, heat flux and others) as they appear in the general, unclosed form of the volume-averaged equations of multiphase flows. By appealing to the difference between slowly and rapidly varying quantities, it is shown that the natural closure of these terms leads to the use of a single, slowly-varying combined average flux, common to both phases, plus rapidly-varying local contributions for each phase. The result is general and only rests on the hypothesis that the spatial variation of the combined average flux is adequately described by a linear function of position within the averaging volume. No further hypotheses on the nature of the flow (e.g., about specific flow regimes) prove necessary. The result agrees with earlier ones obtained by ensemble averaging, is illustrated with the example of disperse flows and discussed in the light of some earlier and current literature. A very concise derivation of the general averaged balance equation is also given.

AB - This note examines the modeling of non-convective fluxes (e.g., stress, heat flux and others) as they appear in the general, unclosed form of the volume-averaged equations of multiphase flows. By appealing to the difference between slowly and rapidly varying quantities, it is shown that the natural closure of these terms leads to the use of a single, slowly-varying combined average flux, common to both phases, plus rapidly-varying local contributions for each phase. The result is general and only rests on the hypothesis that the spatial variation of the combined average flux is adequately described by a linear function of position within the averaging volume. No further hypotheses on the nature of the flow (e.g., about specific flow regimes) prove necessary. The result agrees with earlier ones obtained by ensemble averaging, is illustrated with the example of disperse flows and discussed in the light of some earlier and current literature. A very concise derivation of the general averaged balance equation is also given.

KW - METIS-318156

KW - IR-101775

U2 - 10.1016/j.ijmultiphaseflow.2015.12.009

DO - 10.1016/j.ijmultiphaseflow.2015.12.009

M3 - Article

VL - 80

SP - 176

EP - 180

JO - International journal of multiphase flow

JF - International journal of multiphase flow

SN - 0301-9322

ER -