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Articoli di riviste sul tema "Stratified flow"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 25 luglio 2025

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1

Cisneros-Aguirre, Jesús, J. L. Pelegrí, and P. Sangrà. "Experiments on layer formation in stratified shear flow." Scientia Marina 65, S1 (2001): 117–26. http://dx.doi.org/10.3989/scimar.2001.65s1117.

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2

BALMFORTH, NEIL J., and YUAN-NAN YOUNG. "Stratified Kolmogorov flow." Journal of Fluid Mechanics 450 (January 9, 2002): 131–67. http://dx.doi.org/10.1017/s0022111002006371.

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In this study we investigate the Kolmogorov flow (a shear flow with a sinusoidal velocity profile) in a weakly stratified, two-dimensional fluid. We derive amplitude equations for this system in the neighbourhood of the initial bifurcation to instability for both low and high Péclet numbers (strong and weak thermal diffusion, respectively). We solve amplitude equations numerically and find that, for low Péclet number, the stratification halts the cascade of energy from small to large scales at an intermediate wavenumber. For high Péclet number, we discover diffusively spreading, thermal bounda

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3

Ng, T. S., C. J. Lawrence, and G. F. Hewitt. "Laminar stratified pipe flow." International Journal of Multiphase Flow 28, no. 6 (2002): 963–96. http://dx.doi.org/10.1016/s0301-9322(02)00004-6.

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4

Fan, Jiahua. "Stratified flow through outlets." Journal of Hydro-environment Research 2, no. 1 (2008): 3–18. http://dx.doi.org/10.1016/j.jher.2008.04.001.

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5

Moiseev, K. V. "Stratified flow with natural convection weakly stratified fluid." Proceedings of the Mavlyutov Institute of Mechanics 11, no. 1 (2016): 88–93. http://dx.doi.org/10.21662/uim2016.1.013.

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In work on the basis of a mathematical model based on a linear approximation, we study the formation of the layered flows with natural convection, poorly stratified inhomogeneous liquid. The regions of the parameters under which a layered structure of the flow-cell in a side heating.

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6

Shogo, Shakouchi, and Uchiyama Tomomi. "1097 MIXING PHENOMENA OF DENSITY STRATIFIED FLUID WITH JET FLOW." Proceedings of the International Conference on Jets, Wakes and Separated Flows (ICJWSF) 2013.4 (2013): _1097–1_—_1097–4_. http://dx.doi.org/10.1299/jsmeicjwsf.2013.4._1097-1_.

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7

Vlachos, N. A. "Studies of Wavy Stratified and Stratified/Atomization Gas-Liquid Flow." Journal of Energy Resources Technology 125, no. 2 (2003): 131–36. http://dx.doi.org/10.1115/1.1576265.

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Studies of wavy stratified and stratified/atomization two-phase flow in horizontal pipes are outlined. Notable features of this flow regime include the appearance of disturbance waves, the atomization onset and the drastic change of the gas/liquid interface profile from flat to “concave.” Liquid-to-wall shear stress tends to decrease circumferentially. A computational procedure for predicting main flow characteristics, which takes into account the above results in its design relations, is first assessed with detailed experimental data and is then combined with a CFD code, aiming at enhancing t

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8

BALMFORTH, N. J., and Y. N. YOUNG. "Stratified Kolmogorov flow. Part 2." Journal of Fluid Mechanics 528 (April 10, 2005): 23–42. http://dx.doi.org/10.1017/s002211200400271x.

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9

Castro, I. P., and W. H. Snyder. "Upstream motions in stratified flow." Journal of Fluid Mechanics 187 (February 1988): 487–506. http://dx.doi.org/10.1017/s0022112088000539.

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In this paper experimental measurements of the time-dependent velocity and density perturbations upstream of obstacles towed through linearly stratified fluid are presented. Attention is concentrated on two-dimensional obstacles which generate turbulent separated wakes at Froude numbers, based on velocity and body height, of less than 0.5. The form of the upstream columnar modes is shown to be largely that of first-order unattenuating disturbances, which have little resemblance to the perturbations described by small-obstacle-height theories. For two-dimensional obstacles the disturbances are

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10

Lin, Q., W. R. Lindberg, D. L. Boyer, and H. J. S. Fernando. "Stratified flow past a sphere." Journal of Fluid Mechanics 240, no. -1 (1992): 315. http://dx.doi.org/10.1017/s0022112092000119.

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11

Govindarajan, Rama, and Kirti Chandra Sahu. "Instabilities in Viscosity-Stratified Flow." Annual Review of Fluid Mechanics 46, no. 1 (2014): 331–53. http://dx.doi.org/10.1146/annurev-fluid-010313-141351.

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12

Soo, S. L., and R. W. Lyczkowski. "Analysis of Stratified Flow Mixing." Nuclear Science and Engineering 91, no. 3 (1985): 349–58. http://dx.doi.org/10.13182/nse85-a17310.

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13

Valentine, Greg A. "Stratified flow in pyroclastic surges." Bulletin of Volcanology 49, no. 4 (1987): 616–30. http://dx.doi.org/10.1007/bf01079967.

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14

Korbel, A., and W. Bochniak. "Stratified plastic flow in metals." International Journal of Mechanical Sciences 128-129 (August 2017): 269–76. http://dx.doi.org/10.1016/j.ijmecsci.2017.04.006.

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15

Barnard, Richard C., and Peter R. Wolenski. "Flow Invariance on Stratified Domains." Set-Valued and Variational Analysis 21, no. 2 (2013): 377–403. http://dx.doi.org/10.1007/s11228-013-0230-y.

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16

Boubnov, B. M., E. B. Gledzer, and E. J. Hopfinger. "Stratified circular Couette flow: instability and flow regimes." Journal of Fluid Mechanics 292 (June 10, 1995): 333–58. http://dx.doi.org/10.1017/s0022112095001558.

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The stability conditions of the flow between two concentric cylinders with the inner one rotating (circular Couette flow) have been investigated experimentally and theoretically for a fluid with axial, stable linear density stratification. The behaviour of the flow, therefore, depends on the Froude number Fr = Ω/N (where Ω is the angular velocity of the inner cylinder and N is the buoyancy frequency of the fluid) in addition to the Reynolds number and the non-dimensional gap width ε, here equal to 0.275.Experiments show that stratification has a stabilizing effect on the flow with the critical

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17

Boubnov, B. "Stratified circular Couette flow: instability and flow regimes." International Journal of Multiphase Flow 22 (December 1996): 127. http://dx.doi.org/10.1016/s0301-9322(97)88413-3.

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18

Al-Sarkhi, A., E. Pereyra, I. Mantilla, and C. Avila. "Dimensionless oil-water stratified to non-stratified flow pattern transition." Journal of Petroleum Science and Engineering 151 (March 2017): 284–91. http://dx.doi.org/10.1016/j.petrol.2017.01.016.

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19

FUKUSHIMA, Chiharu, Suketsugu NAKANISHI, and Hideo OSAKA. "321 Stratified flow induced by an impulsively started rotating cylinder : Patterns of stratified circular flow." Proceedings of Conference of Chugoku-Shikoku Branch 2006.44 (2006): 123–24. http://dx.doi.org/10.1299/jsmecs.2006.44.123.

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20

Denier, James P., and Jillian A. K. Stott. "Wave-Mean Flow Interactions in Thermally Stratified Poiseuille Flow." Studies in Applied Mathematics 102, no. 2 (1999): 121–36. http://dx.doi.org/10.1111/1467-9590.00106.

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21

Dentz, Marco, and Jesus Carrera. "Mixing and spreading in stratified flow." Physics of Fluids 19, no. 1 (2007): 017107. http://dx.doi.org/10.1063/1.2427089.

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22

Rouseff, Daniel, Kraig B. Winters, and Peter Kaczkowski. "Tomographic reconstruction of stratified fluid flow." Journal of the Acoustical Society of America 89, no. 4B (1991): 1875. http://dx.doi.org/10.1121/1.2029346.

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23

Bala, Manju. "Stability of Stratified Compressible Shear Flow." International Journal of Mathematics Trends and Technology 46, no. 2 (2017): 53–61. http://dx.doi.org/10.14445/22315373/ijmtt-v46p511.

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24

Jacobitz, F. G., M. M. Rogers, and J. H. Ferziger. "Waves in stably stratified turbulent flow." Journal of Turbulence 6 (January 2005): N32. http://dx.doi.org/10.1080/14685240500462069.

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25

Winters, K. B., and D. Rouseff. "Tomographic reconstruction of stratified fluid flow." IEEE Transactions on Ultrasonics, Ferroelectrics and Frequency Control 40, no. 1 (1993): 26–33. http://dx.doi.org/10.1109/58.184995.

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26

Torres, C. R., and J. E. Castillo. "Stratified rotating flow over complex terrain." Applied Numerical Mathematics 47, no. 3-4 (2003): 531–41. http://dx.doi.org/10.1016/s0168-9274(03)00085-0.

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27

Chernyshenko, S. "Stratified Sadovskii flow in a channel." Journal of Fluid Mechanics 250 (May 1993): 423–31. http://dx.doi.org/10.1017/s002211209300151x.

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Abstract (sommario):

Stably stratified and non-stratified flows past a touching pair of vortices with continuous velocity are considered. An asymptotic solution for the very long eddies is determined. Numerical results cover the whole range of subcritical stratification and eddy length.

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28

Kadri, Y., P. Bonneton, J. M. Chomaz, and M. Perrier. "Stratified flow over three-dimensional topography." Dynamics of Atmospheres and Oceans 23, no. 1-4 (1996): 321–34. http://dx.doi.org/10.1016/0377-0265(95)00433-5.

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29

Taitel, Y. "Stratified three phase flow in pipes." International Journal of Multiphase Flow 22 (December 1996): 118. http://dx.doi.org/10.1016/s0301-9322(97)88338-3.

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30

Kuru, W. "Linear stability of stratified channel flow." International Journal of Multiphase Flow 22 (December 1996): 122. http://dx.doi.org/10.1016/s0301-9322(97)88369-3.

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31

Strack, Otto D. L. "Vertically integrated flow in stratified aquifers." Journal of Hydrology 548 (May 2017): 794–800. http://dx.doi.org/10.1016/j.jhydrol.2017.01.039.

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32

Hunt, Bruce, and Martin Gribble. "Stratified Flow Approximation for Sloping Aquifers." Journal of Hydrologic Engineering 2, no. 2 (1997): 50–55. http://dx.doi.org/10.1061/(asce)1084-0699(1997)2:2(50).

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33

Dewey, Richard, David Richmond, and Chris Garrett. "Stratified Tidal Flow over a Bump." Journal of Physical Oceanography 35, no. 10 (2005): 1911–27. http://dx.doi.org/10.1175/jpo2799.1.

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Abstract (sommario):

Abstract The interaction of a stratified flow with an isolated topographic feature can introduce numerous disturbances into the flow, including turbulent wakes, internal waves, and eddies. Measurements made near a “bump” east of Race Rocks, Vancouver Island, reveal a wide range of phenomena associated with the variable flow speeds and directions introduced by the local tides. Upstream and downstream flows were observed by placing two acoustic Doppler current profilers (ADCPs) on one flank of the bump. Simultaneous shipboard ADCP surveys corroborated some of the more striking features. Froude n

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34

Mahrt, L., and N. Gamage. "Observations of Turbulence in Stratified Flow." Journal of the Atmospheric Sciences 44, no. 7 (1987): 1106–21. http://dx.doi.org/10.1175/1520-0469(1987)044<1106:ootisf>2.0.co;2.

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35

Vladimirov, I. Yu, N. N. Korchagin, A. S. Savin, and E. O. Savina. "Stratified unbounded flow past of obstacles." Oceanology 51, no. 6 (2011): 916–24. http://dx.doi.org/10.1134/s000143701106021x.

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36

Killworth, Peter D. "Flow Properties in Rotating, Stratified Hydraulics." Journal of Physical Oceanography 22, no. 9 (1992): 997–1017. http://dx.doi.org/10.1175/1520-0485(1992)022<0997:fpirsh>2.0.co;2.

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37

Allen, J. S., and P. A. Newberger. "On Intermediate Models for Stratified Flow." Journal of Physical Oceanography 23, no. 11 (1993): 2462–86. http://dx.doi.org/10.1175/1520-0485(1993)023<2462:oimfsf>2.0.co;2.

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38

Ponetti, G., M. Sammartino, and V. Sciacca. "Transitions in a stratified Kolmogorov flow." Ricerche di Matematica 66, no. 1 (2016): 189–99. http://dx.doi.org/10.1007/s11587-016-0296-6.

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39

Taitel, Y., D. Barnea, and J. P. Brill. "Stratified three phase flow in pipes." International Journal of Multiphase Flow 21, no. 1 (1995): 53–60. http://dx.doi.org/10.1016/0301-9322(94)00058-r.

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40

Kuru, W. C., M. Sangalli, D. D. Uphold, and M. J. McCready. "Linear stability of stratified channel flow." International Journal of Multiphase Flow 21, no. 5 (1995): 733–53. http://dx.doi.org/10.1016/0301-9322(95)00015-p.

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41

Imberger, J., and G. N. Ivey. "Boundary mixing in stratified reservoirs." Journal of Fluid Mechanics 248 (March 1993): 477–91. http://dx.doi.org/10.1017/s0022112093000850.

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We consider the steady flow driven by turbulent mixing in a benthic boundary layer along a sloping boundary in the general case of a non-uniform background density gradient. The velocity and density fields are decomposed into barotropic and baroclinic components, and a solution is obtained by taking an expansion in the small parameter A, the aspect ratio of the boundary layer defined as the thickness divided by the alongslope length. The flow in the boundary layer is governed by a balance between alongslope baroclinic and barotropic density fluxes. A number of flow regimes can exist, and we sh

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42

Louay Abd Al-Azez Mahdi, Hasanain Adnan Abdul Wahhab, and Miqdam Tariq Chaichan. "The Change of Flow Pattern from Stratified to Stratified-Wavy for Condensation in Wire on Tube Heat Exchangers." Journal of Advanced Research in Fluid Mechanics and Thermal Sciences 117, no. 2 (2024): 105–15. http://dx.doi.org/10.37934/arfmts.117.2.105115.

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Flow patterns inside wire-on-tube condensers with different refrigerant mass flow rates were studied in a theoretical study. In this study, tubes with diameters of 3.25 mm (3/16"), 4.83 mm (1/4") and 6.29 mm (5/16") were used. R-134a and R-600a cooling fluids were used at condensing temperatures of 54.4°C, 45°C, and 35°C. The results of this study were obtained using Equal Equation Solver (EES) software. The proposed model was able to predict the type of refrigerant flow pattern based on the limitations reported in previous studies. It was possible to distinguish four kinds of flow patterns: l

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43

BAINES, PETER G. "Two-dimensional plumes in stratified environments." Journal of Fluid Mechanics 471 (November 5, 2002): 315–37. http://dx.doi.org/10.1017/s0022112002002215.

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Laboratory experiments on the flow of negatively buoyant two-dimensional plumes adjacent to a wall in a density-stratified environment are described. The flow passes through several stages, from an inertial jet to a buoyant plume, to a neutrally buoyant jet, and then a negatively buoyant plume when it overshoots its equilibrium density. This fluid then ‘springs back’ and eventually occupies an intermediate range of heights. The flow is primarily characterized by the initial value of the buoyancy number, B0 = Q0N3/g′02, where Q0 is the initial volume flux per unit width, g′0 is the initial buoy

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44

Takagi, Norimasa, Toshifumi Noma, Masaaki Sakuta, Junpei Nakamura, and Hitoshi Imamura. "Flow visualization around an artificial upwelling structure in stratified flow." Journal of the Visualization Society of Japan 10, no. 1Supplement (1990): 115–18. http://dx.doi.org/10.3154/jvs.10.1supplement_115.

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45

Rotunno, Richard, and Manuela Lehner. "Two-Layer Stratified Flow past a Valley." Journal of the Atmospheric Sciences 73, no. 10 (2016): 4065–76. http://dx.doi.org/10.1175/jas-d-16-0132.1.

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Abstract Observations and models of nocturnal katabatic winds indicate strong low-level stability with much weaker stability aloft. When such winds encounter an embedded depression in an otherwise smooth sloping plane, the flow responds in a manner that is largely describable by the inviscid fluid dynamics of stratified flow. Building on earlier work, the present study presents a series of numerical simulations based on the simplest nontrivial idealization relevant to the observations: the height-independent flow of a two-layer stratified fluid past a two-dimensional valley. Stratified flow pa

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46

Spalding, Dudley Brian. "NUMERICAL BENCHMARK TEST NO. 2.7: STRATIFIED FLOW." Multiphase Science and Technology 3, no. 1-4 (1987): 483–84. http://dx.doi.org/10.1615/multscientechn.v3.i1-4.340.

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47

Hwang, Jong-Yeon, Kyung-Soo Yang, and Dong-Woo Kim. "Numerical Simulation of Stratified Taylor-Couette Flow." Transactions of the Korean Society of Mechanical Engineers B 30, no. 7 (2006): 630–37. http://dx.doi.org/10.3795/ksme-b.2006.30.7.630.

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48

Ali, Imad Taher, Imran Afgan, and Ilyas Khurshid. "Stratified Two-Phase Turbulent Pipe Flow Simulations." International Journal on Advanced Science, Engineering and Information Technology 12, no. 4 (2022): 1301. http://dx.doi.org/10.18517/ijaseit.12.4.16361.

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49

Xu, X., C. Yi, and E. Kutter. "Stably stratified canopy flow in complex terrain." Atmospheric Chemistry and Physics Discussions 14, no. 21 (2014): 28483–522. http://dx.doi.org/10.5194/acpd-14-28483-2014.

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Abstract. The characteristics of stably stratified canopy flows in complex terrain are investigated by employing the Renormalized Group (RNG) k-ε turbulence model. In this two-dimensional simulation, we imposed persistent constant heat flux at ground surface and linearly increasing cooling rate in the upper canopy layer, vertically varying dissipative force from canopy drag elements, buoyancy forcing induced from thermal stratification and the hill terrain. These strong boundary effects keep nonlinearity in the two-dimensional Navier–Stokes equations high enough to generate turbulent behavior.

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50

Zhang, Bing, Jing Lv, Peng Huo, and Shao Xiong Zhang. "Application of EFDC to Density Stratified Flow." Applied Mechanics and Materials 256-259 (December 2012): 2486–89. http://dx.doi.org/10.4028/www.scientific.net/amm.256-259.2486.

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Environmental Fluid Dynamics Code (EFDC) was developed by Hamrick at Virginia Institute of Marine Science for estuarine and coastal applications. EFDC is a general-purpose modeling package for simulating three-dimensional flow, transport, and biogeochemical processes in surface water systems such as rivers, lakes, reservoirs, estuaries, wetlands and coastal regions. Use the 3-D numerical model EFDC simulated the density stratified flow in a slut. Compared the simulation and experimental data, the results showed that EFDC could accurately simulated the density stratified flow.

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