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Transitional and Turbulent Flow in a Bed of Spheres as Measured with Stereoscopic Particle Image Velocimetry
Luleå tekniska universitet, Institutionen för teknikvetenskap och matematik, Strömningslära och experimentell mekanik.
Luleå tekniska universitet, Institutionen för teknikvetenskap och matematik, Strömningslära och experimentell mekanik.ORCID-id: 0000-0002-1033-0244
Luleå tekniska universitet, Institutionen för teknikvetenskap och matematik, Strömningslära och experimentell mekanik.ORCID-id: 0000-0001-8355-2414
Luleå tekniska universitet, Institutionen för teknikvetenskap och matematik, Strömningslära och experimentell mekanik.
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Rekke forfattare: 52017 (engelsk)Inngår i: Transport in Porous Media, ISSN 0169-3913, E-ISSN 1573-1634, Vol. 117, nr 1, s. 45-67Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Stereoscopic particle image velocimetry has been used to investigate inertia dominated, transitional and turbulent flow in a randomly packed bed of monosized PMMA spheres. By using an index-matched fluid, the bed is optically transparent and measurements can be performed in an arbitrary position within the porous bed. The velocity field observations are carried out for particle Reynolds numbers, (Formula presented.), between 20 and 3220, and the sampling is done at a frequency of 75 Hz. Results show that, in porous media, the dynamics of the flow can vary significantly from pore to pore. At (Formula presented.) around 400 the spatially averaged time fluctuations of total velocity reach a maximum and the spatial variation of the time-averaged total velocity, (Formula presented.) increases up to about the same (Formula presented.) and then it decreases. Also in the studied planes, a considerable amount of the fluid moves in the perpendicular directions to the main flow direction and the time-averaged magnitude of the velocity in the main direction, (Formula presented.), has an averaged minimum of 40% of the magnitude of (Formula presented.) at (Formula presented.) about 400. For (Formula presented.), this ratio is nearly constant and (Formula presented.) is on average a little bit less than 50% of (Formula presented.). The importance of the results for longitudinal and transverse dispersion is discussed.

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Springer, 2017. Vol. 117, nr 1, s. 45-67
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URN: urn:nbn:se:ltu:diva-61843DOI: 10.1007/s11242-017-0819-yISI: 000395621700003Scopus ID: 2-s2.0-85009872759OAI: oai:DiVA.org:ltu-61843DiVA, id: diva2:1072052
Merknad

Validerad; 2017; Nivå 2; 2017-03-06 (andbra)

Tilgjengelig fra: 2017-02-07 Laget: 2017-02-07 Sist oppdatert: 2018-10-04bibliografisk kontrollert

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Khayamyan, ShervinLundström, StaffanGren, PerLycksam, HenrikHellström, Gunnar

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