Nonsteady discharge of granular media from a silo driven by a pressurized gas
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作者:
Zou, Z.
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Inst Radioprotect & Surete Nucl IRSN, PSN RES, SEMIA, LSMA, F-13115 St Paul Les Durance, France
Aix Marseille Univ, CNRS, IUSTI, F-13013 Marseille, FranceInst Radioprotect & Surete Nucl IRSN, PSN RES, SEMIA, LSMA, F-13115 St Paul Les Durance, France
Zou, Z.
[1
,2
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Ruyer, P.
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Inst Radioprotect & Surete Nucl IRSN, PSN RES, SEMIA, LSMA, F-13115 St Paul Les Durance, FranceInst Radioprotect & Surete Nucl IRSN, PSN RES, SEMIA, LSMA, F-13115 St Paul Les Durance, France
Ruyer, P.
[1
]
Lagree, P. -Y.
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Sorbonne Univ, CNRS UMR7190, Inst Jean le Rond dAlembert, F-75005 Paris, FranceInst Radioprotect & Surete Nucl IRSN, PSN RES, SEMIA, LSMA, F-13115 St Paul Les Durance, France
Lagree, P. -Y.
[3
]
Aussillous, P.
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Aix Marseille Univ, CNRS, IUSTI, F-13013 Marseille, FranceInst Radioprotect & Surete Nucl IRSN, PSN RES, SEMIA, LSMA, F-13115 St Paul Les Durance, France
Aussillous, P.
[2
]
机构:
[1] Inst Radioprotect & Surete Nucl IRSN, PSN RES, SEMIA, LSMA, F-13115 St Paul Les Durance, France
[2] Aix Marseille Univ, CNRS, IUSTI, F-13013 Marseille, France
[3] Sorbonne Univ, CNRS UMR7190, Inst Jean le Rond dAlembert, F-75005 Paris, France
We studied experimentally and numerically the effect of an imposed gas pressure on the discharge flow of granular media from a cylindrical silo. This study is motivated by a nuclear safety related phenomenology of fuel fragments displaced from a fuel rod under several accidental conditions, the flow being potentially driven by pressurized fission gases within the rod. We imposed a moderate constant air pressure at the top of the granular column (???3000 Pa) and we varied the size and type of the particles and the surrounding fluid where the discharge occurs, using air and water to test the role of the coolant fluid in the nuclear safety problem. The measured parameters are the particle mass flow rate, the volumetric flow rate of air, and the pressure along the silo. The particle and air flow rates are found to be nonsteady and to increase with time. To model these behaviors, we use a twophase continuum model with a frictional rheology to describe particle-particle interactions, and we propose a simple quasisteady analytical model considering the air-pressure gradient at the orifice as an additional driving force to the gravity. We implemented numerically the two-phase continuum model in an axisymmetric configuration which reproduces the experimental results.
机构:
Univ Simon Bolivar, Dept Fis, Caracas 1080A, VenezuelaUniv Simon Bolivar, Dept Fis, Caracas 1080A, Venezuela
Colonnello, C.
Reyes, L. I.
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Univ Simon Bolivar, Dept Fis, Caracas 1080A, VenezuelaUniv Simon Bolivar, Dept Fis, Caracas 1080A, Venezuela
Reyes, L. I.
Clement, E.
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CNRS UMR 7636, ESPCI, PMMH, F-75005 Paris, France
Univ Paris 6 & Paris 7, F-75005 Paris, FranceUniv Simon Bolivar, Dept Fis, Caracas 1080A, Venezuela
Clement, E.
Gutierrez, G.
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Univ Simon Bolivar, Dept Fis, Caracas 1080A, VenezuelaUniv Simon Bolivar, Dept Fis, Caracas 1080A, Venezuela
机构:
Univ Texas Austin, Hildebrand Dept Petr & Geosyst Engn, 200 E Dean Keeton, Austin, TX 78712 USA
Univ Texas Austin, Ctr Subsurface Energy & Environm, 200 E Dean Keeton, Austin, TX 78712 USAUniv Texas Austin, Hildebrand Dept Petr & Geosyst Engn, 200 E Dean Keeton, Austin, TX 78712 USA
Li, Zihao
Espinoza, D. Nicolas
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Univ Texas Austin, Hildebrand Dept Petr & Geosyst Engn, 200 E Dean Keeton, Austin, TX 78712 USA
Univ Texas Austin, Ctr Subsurface Energy & Environm, 200 E Dean Keeton, Austin, TX 78712 USAUniv Texas Austin, Hildebrand Dept Petr & Geosyst Engn, 200 E Dean Keeton, Austin, TX 78712 USA
Espinoza, D. Nicolas
Balhoff, Matthew T.
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机构:
Univ Texas Austin, Hildebrand Dept Petr & Geosyst Engn, 200 E Dean Keeton, Austin, TX 78712 USA
Univ Texas Austin, Ctr Subsurface Energy & Environm, 200 E Dean Keeton, Austin, TX 78712 USAUniv Texas Austin, Hildebrand Dept Petr & Geosyst Engn, 200 E Dean Keeton, Austin, TX 78712 USA