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Letteratura scientifica selezionata sul tema "Stratified flow"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 1 agosto 2024

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Articoli di riviste sul tema "Stratified flow"

1

Cisneros-Aguirre, Jesús, J. L. Pelegrí e P. Sangrà. "Experiments on layer formation in stratified shear flow". Scientia Marina 65, S1 (30 luglio 2001): 117–26. http://dx.doi.org/10.3989/scimar.2001.65s1117.

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2

BALMFORTH, NEIL J., e YUAN-NAN YOUNG. "Stratified Kolmogorov flow". Journal of Fluid Mechanics 450 (9 gennaio 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 boundary layers in which the stratification temporarily impedes, but does not saturate, the growth of the instability; the instability eventually mixes the temperature inside the boundary layers, so releasing itself from the stabilizing stratification there, and thereby grows more quickly. We solve the governing fluid equations numerically to compare with the asymptotic results, and to extend the exploration well beyond onset. We find that the arrest of the inverse cascade by stratification is a robust feature of the system, occurring at higher Reynolds, Richards and Péclet numbers – the flow patterns are invariably smaller than the domain size. At higher Péclet number, though the system creates slender regions in which the temperature gradient is concentrated within a more homogeneous background, there are no signs of the horizontally mixed layers separated by diffusive interfaces familiar from doubly diffusive systems.

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3

Ng, T. S., C. J. Lawrence e G. F. Hewitt. "Laminar stratified pipe flow". International Journal of Multiphase Flow 28, n. 6 (giugno 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, n. 1 (settembre 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, n. 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, e 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

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

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8

Castro, I. P., e W. H. Snyder. "Upstream motions in stratified flow". Journal of Fluid Mechanics 187 (febbraio 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 similar to those found by Wei, Kao & Pao (1975) and it is shown that provided a suitable obstacle drag coefficient is specified, the lowest-order modes (at least) are quantitatively consistent with the results of the Oseen inviscid model.Discussion of some results of similar measurements upstream of three-dimensional obstacles, the importance of towing tank endwalls and the relevance of the Foster & Saffman (1970) theory for the limit of zero Froude number is also included.

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Lin, Q., W. R. Lindberg, D. L. Boyer e H. J. S. Fernando. "Stratified flow past a sphere". Journal of Fluid Mechanics 240, n. -1 (luglio 1992): 315. http://dx.doi.org/10.1017/s0022112092000119.

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10

Govindarajan, Rama, e Kirti Chandra Sahu. "Instabilities in Viscosity-Stratified Flow". Annual Review of Fluid Mechanics 46, n. 1 (3 gennaio 2014): 331–53. http://dx.doi.org/10.1146/annurev-fluid-010313-141351.

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Tesi sul tema "Stratified flow"

1

Kurban, Adib Paulo Abdalla. "Stratified liquid-liquid flow". Thesis, Imperial College London, 1997. http://hdl.handle.net/10044/1/7553.

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Bourban, Sebastien E. "Stratified shallow flow modelling". Thesis, Open University, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.664520.

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Environmental hydraulics covers a very wide range of applications including free surface flows in rivers. estuaries and lakes. To find engineering solutions to environmental hydraulics problems. 3D numerical modelling is nowadays widely used. However. the computation of sharp spatial gradients (such as found in stratified estuaries and lakes. around plumes near outfalls along rivers and coasts or in exchange areas of high shear). and the modelling of these processes along steep bathymetric slopes (such as found at the edge of dredged channels or of the continental shelf) remains a challenge. In addition. crude assumptions (such as the hydrostatic assumption) are often made to the primary differential equations in order to simplify the problem and enable long term prediction of environmental hydraulic changes. In this thesis. a robust adaptive mesh displacement (AMD) method is implemented and validated against the lock exchange case in particular. The AMD method aims at vertically focusing nodes within each water column to capture sharp gradients. while reducing the number of nodes or requiring prior knowledge of the flow structure. Second. a direct computation of dynamic pressure is introduced based on the equation of vertical momentum and validated against the analytical potential flow theory solution of a source-sink pair. Dynamic pressure is necessary to model destratification recirculation devices. or flow over dredge channel. or solitary waves. for instance. This direct computation method makes the hydrostatic assumption redundant. Third. a new advection scheme is implemented. whose main advantage is simplicity averaging over Riemann problems without solving them. while excessive numerical viscosity is compensated for by using high-resolution MUSCL type reconstruction. Recommendations are made in this thesis to extend the advection scheme developed herein for tracer advection to the non-linear shallow water equations. to the diffusion terms and to turbulence closure laws within the same finite element framework.

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Rea, Suzanne. "Stratified flow at T-junctions". Thesis, University of Nottingham, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.287195.

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4

Ng, Tzuu Shing. "Interfacial structure of stratified pipe flow". Thesis, Imperial College London, 2002. http://hdl.handle.net/10044/1/11274.

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5

Shaha, Jonathan. "Phase interactions in transient stratified flow". Thesis, Imperial College London, 2000. http://hdl.handle.net/10044/1/8653.

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6

Iial-Awad, Ahmad Salmeh. "Stratified flow in the built environment". Thesis, University of Hertfordshire, 2006. http://hdl.handle.net/2299/14350.

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Stratified flow in an environmental chamber has been investigated. The chamber of dimensions (7.5m long, 5.6m wide and 3.0m) at the University of Hertfordshire has been used. Sets of experiments investigating the effect of the major flow parameters such as airflow rate, jet momentum, flow conditions and height of the air supply device have been conducted. Results have been obtained to evaluate the flow characteristics and thermal stratification mechanism. The study has demonstrated the validity of using smoke visualization to evaluate the stratified flow characteristics such as interface level height, stratified layer thickness, and degree of stratification. The effects of both hot and cold airflow rates in the ranges of (0.0 to 8.0 m3 /min) were investigated. The flow characteristics vary depending on the flow parameters and the experimental conditions. The effect of supply terminal and extract terminal at various airflow rates on the flow characteristics is experimentally investigated. It has been found that relative influence of inertia and buoyancy forces resolves the stratified flow characteristics. The stratification interface level height and the ventilation flow rates are two main factors in the design of natural ventilation system. The results can be used to obtain a good estimation of the effectiveness of a ventilation system at design stage. Experimental work was carried out using ceiling jet to supply hot and cold air to a confined space, to investigate the effect of jet momentum in breaking and mixing the stratified layer. The flow of high momentum was supplied downward from the ceiling. The magnitude of momentum needed depends on the degree of stratification, stratified layer interface level height and the stratification conditions. It can be seen that the jet momentum has significant influence on the mixing of the stratified flow characteristics. The results indicated that once the momentum was initiated a mixed flow grew in the occupied zone above the floor. The height of this zone depends on the stratified flow characteristics, and the temperature and momentum of the ceiling jet. Another area of experimentation was the inversion of input airflow supplies. In this case, the flow of high buoyancy was supplied upward, whilst the flow of high momentum was supplied downward from the ceiling. The stratified layer lost its stability and broke down due to the drag and tearing of cold air penetrated downward from higher levels. The compound effect of these two conditions will circulate the air in the whole space and disturb the stability of the stratified layer to reach fully mixed flow A comprehensive definition of the degree of stratification was formulated. Analytical solutions were developed for the stratified layer thickness and location as a function of temperature gradient and airflow ratios. These expressions were calibrated using the experimental results. The critical momentum needed to breakdown the stratified layer also evaluated. Comparisons with previous studies where also carried out. It was found that the stratified layer interface level height is dependent on the ratio of airflow rate and geometrical effects. If mixed flow is desired then the cold inflow aperture should be located higher than the hot inflow aperture, whiles the interface level height is not located at the exhaust aperture height. The critical vertical momentum necessary in order to break down a stratified layer has been found to depend on the stratified layer interface level height. A semi-empirical formula based on the present experimental results has been developed to predict the critical vertical momentum for given stratified conditions. Based on the present experimental results, the effect of momentum is greater than the effect of buoyancy and the time needed to break down the stratified layer is considerable less than the time it takes to stratify. Experimental data also demonstrate a ventilation method for increasing the occupied zone height without breaking down the stratified layer.

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Feng, Yanhua. "Stably stratified shear flow over complex terrain". Thesis, University of Cambridge, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.264359.

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8

Omar, Hanan. "Intrusion flow into a density stratified resevoir". Thesis, Omar, Hanan (2016) Intrusion flow into a density stratified resevoir. PhD thesis, Murdoch University, 2016. https://researchrepository.murdoch.edu.au/id/eprint/30247/.

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Steady two-dimensional flows from an angled structure into a lake or a reservoir where the interface between the intrusion and the ambient fluid separates from a solid wall is considered. The fluid is assumed to be of finite depth and the incoming channel makes an angle _ with the horizontal axis. The problem is formulated using conformal mapping and integral equation techniques and the resulting problem is solved using a surface angle approach. The shape of the interface is computed for a range of entry angle and flow rate. Exact solutions are presented at a high flow rate and compared with the solutions to nonlinear problem. Solutions with waves are shown to exist on the interface at small flow rate and these are computed at very small entry angles using a physical plane method. The case in which the lake or the reservoir is stratified in density is also considered and separation height is determined for different values of the stratification. In all cases, the parameter space in which steady solutions exist is studied and limiting solutions are obtained. The results have implications for the design of efficient inflow structures for reservoirs and for water quality management.

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9

Siqueira, Renato do Nascimento. "Transport and mixing processes in stratified flow". Thesis, Loughborough University, 2002. https://dspace.lboro.ac.uk/2134/34335.

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The processes of transport and mixing in stratified open channel flows are investigated in this thesis. Detailed measurements of velocity and salinity were conducted, through the use of Laser-Induced Fluorescence (LIP) technique together with Laser Doppler anemometry, so that the effects of secondary current and stratification on the flow behaviour could be analysed. Two configurations were investigated: a rectangular open channel, and a compound open channel. For each configuration, four different stratification levels were analysed. The main flow characteristics, such as corner flow and velocity dip in a rectangular channel, and the twin vortices formed in compound channels, were found to be affected by stratification. In order to understand the mechanisms involved in secondary flow generation, the vorticity balance was carried out. Through the vorticity balance, the contribution of each term in the longitudinal vorticity equation could be evaluated. The mechanisms involved in the turbulence generation were also verified through the turbulent kinetic energy (TKE) budget. One of the contributions of this work refers to the understanding of the effects of stratification on turbulence and secondary flow generation. The exchange coefficients of momentum and solute were also investigated. These coefficients were found to depend not only on stratification level but also on other flow parameters, like for instance the aspect ratio. A new formulation is proposed for narrow channels, but more research is necessary in order to evaluate the effect of other parameters on the exchange coefficients.

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Chilakamarri, Kiran Babu. "Rotating and stratified fluids /". The Ohio State University, 1988. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487584612163036.

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Più fonti

Libri sul tema "Stratified flow"

1

Pedersen, Flemming Bo. Environmental hydraulics: Stratified flows. Berlin: Springer-Verlag, 1986.

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2

Baines, Peter G. Topographic effects in stratified flows. Cambridge: Cambridge University Press, 1995.

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3

Lee, S. RELAP5 assessment on direct-contact condensation in horizontal cocurrent stratified flow. Washington, DC: U.S. Nuclear Regulatory Commission, 1992.

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4

Lee, S. RELAP5 assessment on direct-contact condensation in horizontal oncurrent stratified flow. Washington, DC: U.S. Nuclear Regulatory Commission, 1992.

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5

Lee, S. RELAP5 assessment on direct-contact condensation in horizontal oncurrent stratified flow. Washington, DC: U.S. Nuclear Regulatory Commission, 1992.

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6

Maderich, V. S. Dinamika vnutrennego peremeshivanii͡a︡ v stratifit͡s︡irovannoĭ srede. Kiev: Nauk. dumka, 1988.

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7

S, Puttock J., e Institute of Mathematics and Its Applications., a cura di. Stably stratified flow and dense gas dispersion. Oxford [Oxfordshire]: Clarendon Press, 1988.

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8

Akiyama, Juchiro. Gravity currents in lakes, reservoirs and coastal regions: Two- layer stratified flow analysis. Minneapolis: St. Anthony Falls Hydraulic Laboratory, University of Minnesota, 1987.

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9

Leble, S. B. Volnovodnoe rasprostranenie nelineĭnykh voln v stratifit͡s︡irovannykh sredakh. Leningrad: Izd-vo Leningradskogo universiteta, 1988.

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10

Leble, S. B. Nonlinear waves in waveguides: With stratification. Berlin: Springer-Verlag, 1991.

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Capitoli di libri sul tema "Stratified flow"

1

Pedersen, Flemming Bo. "Winddriven Stratified Flow". In Environmental Hydraulics: Stratified Flows, 113–26. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-86600-5_10.

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2

Pedersen, Flemming Bo. "Winddriven Stratified Flow". In Environmental Hydraulics: Stratified Flows, 113–26. Berlin Heidelberg: Springer-Verlag, 2013. http://dx.doi.org/10.1002/9781118669709.ch10.

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3

Pedersen, Flemming Bo. "Horizontal Buoyant Flow". In Environmental Hydraulics: Stratified Flows, 127–45. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-86600-5_11.

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4

Pedersen, Flemming Bo. "Horizontal Buoyant Flow". In Environmental Hydraulics: Stratified Flows, 127–45. Berlin Heidelberg: Springer-Verlag, 2013. http://dx.doi.org/10.1002/9781118669709.ch11.

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5

Ghajar, Afshin J. "Modeling of Stratified Flow". In Mechanical Engineering Series, 225–36. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-87281-6_17.

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6

Pedersen, Flemming Bo. "A Multipurpose Stratified Flow Flume". In Environmental Hydraulics: Stratified Flows, 263–73. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-86600-5_21.

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Bo Pedersen, Flemming. "A Multipurpose Stratified Flow Flume". In Environmental Hydraulics: Stratified Flows, 263–73. Berlin Heidelberg: Springer-Verlag, 2013. http://dx.doi.org/10.1002/9781118669709.ch22.

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8

Lawrence, Gregory A., Edmund W. Tedford e Jeffrey R. Carpenter. "Instabilities in Stratified Shear Flow". In Coherent Flow Structures at Earth's Surface, 63–71. Chichester, UK: John Wiley & Sons, Ltd, 2013. http://dx.doi.org/10.1002/9781118527221.ch5.

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9

Fabre, Jean. "Modelling of Stratified Gas-Liquid Flow". In Modelling and Experimentation in Two-Phase Flow, 79–116. Vienna: Springer Vienna, 2003. http://dx.doi.org/10.1007/978-3-7091-2538-0_2.

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10

Wong, Teck Neng, Cheng Wang, Haiwang Li, Yandong Gao, Nam-Trung Nguyen, Chun Yang e Kim Tiow Ooi. "Liquid-Liquid Stratified Flow in Microchannels". In Encyclopedia of Microfluidics and Nanofluidics, 1662–78. New York, NY: Springer New York, 2015. http://dx.doi.org/10.1007/978-1-4614-5491-5_817.

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Atti di convegni sul tema "Stratified flow"

1

Jirk, Aleš, e Josef Brechler. "Stratified atmospheric flow modeling". In INTERNATIONAL CONFERENCE OF COMPUTATIONAL METHODS IN SCIENCES AND ENGINEERING 2009: (ICCMSE 2009). AIP, 2012. http://dx.doi.org/10.1063/1.4772136.

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2

Jacobitz, Frank G. "TURBULENT DISPERSION IN STABLY STRATIFIED SHEAR FLOW". In Third Symposium on Turbulence and Shear Flow Phenomena. Connecticut: Begellhouse, 2003. http://dx.doi.org/10.1615/tsfp3.590.

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3

Remmler, Sebastian, e Stefan Hickel. "SPECTRAL EDDY VISCOSITY OF STRATIFIED TURBULENCE". In Eighth International Symposium on Turbulence and Shear Flow Phenomena. Connecticut: Begellhouse, 2013. http://dx.doi.org/10.1615/tsfp8.1170.

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4

Höhne, T., e C. Vallée. "Modelling of stratified two phase flows using an interfacial area density model". In MULTIPHASE FLOW 2009. Southampton, UK: WIT Press, 2009. http://dx.doi.org/10.2495/mpf090111.

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Benz, M., e T. Schulenberg. "Validation analyses of advanced turbulence model approaches for stratified two-phase flows". In MULTIPHASE FLOW 2015. Southampton, UK: WIT Press, 2015. http://dx.doi.org/10.2495/mpf150311.

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6

Xiao, Yuan, Wenxian Lin, Jessie McCormack, Yinghe He, Steven W. Armfield e Michael P. Kirkpatrick. "TURBULENT MIXING IN CROSS SHEARED STRATIFIED FLOW". In Ninth International Symposium on Turbulence and Shear Flow Phenomena. Connecticut: Begellhouse, 2015. http://dx.doi.org/10.1615/tsfp9.780.

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Castro, M. S. de, C. C. Pereira, J. N. dos Santos e O. M. H. Rodriguez. "Geometrical and kinematic properties of interfacial waves in horizontal heavy oil-water stratified flow". In MULTIPHASE FLOW 2011. Southampton, UK: WIT Press, 2011. http://dx.doi.org/10.2495/mpf110191.

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Moradi, B., M. Hossain e G. Oluyemi. "Mechanistic model for four-phase sand/water/oil/gas stratified flow in horizontal pipes". In MULTIPHASE FLOW 2015. Southampton, UK: WIT Press, 2015. http://dx.doi.org/10.2495/mpf150291.

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Martinat, Guillaume, Andres E. Tejada-Martinez e Chester E. Grosch. "LES OF LANGMUIR TURBULENCE IN STABLY STRATIFIED FLOW". In Eighth International Symposium on Turbulence and Shear Flow Phenomena. Connecticut: Begellhouse, 2013. http://dx.doi.org/10.1615/tsfp8.420.

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Wunsch, Scott, e Yuan-nan Young. "UNIVERSALITY OF TEMPERATURE STATISTICS IN STABLY STRATIFIED TURBULENCE". In Second Symposium on Turbulence and Shear Flow Phenomena. Connecticut: Begellhouse, 2001. http://dx.doi.org/10.1615/tsfp2.1760.

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Rapporti di organizzazioni sul tema "Stratified flow"

1

Gregg, Michael C., e Parker MacCready. Stratified Flow over Rough, Sloping Topography. Fort Belvoir, VA: Defense Technical Information Center, settembre 1999. http://dx.doi.org/10.21236/ada629721.

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2

Lee, S. Stability of steam-water countercurrent stratified flow. Office of Scientific and Technical Information (OSTI), ottobre 1985. http://dx.doi.org/10.2172/5093990.

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3

Nielsen, Peter V., Chen Zhang e Li Liu. Airborne transmission of disease in stratified flow. Department of the Built Environment, 2023. http://dx.doi.org/10.54337/aau541985833.

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4

Kim, H. Local properties of countercurrent stratified steam-water flow. Office of Scientific and Technical Information (OSTI), ottobre 1985. http://dx.doi.org/10.2172/6402013.

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Carnevale, George F. Stratified Flow, Wave Packet Reflection and Topographic Currents. Fort Belvoir, VA: Defense Technical Information Center, settembre 2001. http://dx.doi.org/10.21236/ada624782.

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6

Farmer, David M., e Svein Vagle. Stratified Flow Over Topography and Internal Solitary Waves. Fort Belvoir, VA: Defense Technical Information Center, settembre 2002. http://dx.doi.org/10.21236/ada626450.

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7

Monismith, Stephen G., e Mark T. Stacey. Shear Production and Dissipation in a Stratified Tidal Flow. Fort Belvoir, VA: Defense Technical Information Center, settembre 2001. http://dx.doi.org/10.21236/ada624684.

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Stacey, Mark T., e Stephen G. Monismith. Shear Production and Dissipation in a Stratified Tidal Flow. Fort Belvoir, VA: Defense Technical Information Center, settembre 2002. http://dx.doi.org/10.21236/ada626388.

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9

Gallacher, Patrick C., e Hemantha W. Wijesekera. Convection and Internal Waves in a Stably Stratified Shear Flow,. Fort Belvoir, VA: Defense Technical Information Center, luglio 1994. http://dx.doi.org/10.21236/ada304864.

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10

Helfrich, Karl R. Time-dependent Stratified Flow over Topography: Waves and Rotating Hydraulics. Fort Belvoir, VA: Defense Technical Information Center, settembre 1997. http://dx.doi.org/10.21236/ada628665.

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