Gotowe bibliografie tematyczne / Fluid flow

Gotowa bibliografia na temat „Fluid flow”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 8 czerwca 2024

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Artykuły w czasopismach na temat "Fluid flow"

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Abbasi, Aamar Kamal, Nasir Ali, Muhammad Sajid, Iftikhar Ahmad i Sadaqut Hussain. "Peristaltic Tube Flow of a Giesekus Fluid". Nihon Reoroji Gakkaishi 44, nr 2 (2016): 99–108. http://dx.doi.org/10.1678/rheology.44.99.

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Rumble, III. "Evidences of fluid flow during regional metamorphism". European Journal of Mineralogy 1, nr 6 (21.12.1989): 731–37. http://dx.doi.org/10.1127/ejm/1/6/0731.

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Guazzotto, L., i R. Betti. "Two-fluid equilibrium with flow: FLOW2". Physics of Plasmas 22, nr 9 (wrzesień 2015): 092503. http://dx.doi.org/10.1063/1.4929854.

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LIU, TIANSHU, i LIXIN SHEN. "Fluid flow and optical flow". Journal of Fluid Mechanics 614 (16.10.2008): 253–91. http://dx.doi.org/10.1017/s0022112008003273.

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The connection between fluid flow and optical flow is explored in typical flow visualizations to provide a rational foundation for application of the optical flow method to image-based fluid velocity measurements. The projected-motion equations are derived, and the physics-based optical flow equation is given. In general, the optical flow is proportional to the path-averaged velocity of fluid or particles weighted with a relevant field quantity. The variational formulation and the corresponding Euler–Lagrange equation are given for optical flow computation. An error analysis for optical flow computation is provided, which is quantitatively examined by simulations on synthetic grid images. Direct comparisons between the optical flow method and the correlation-based method are made in simulations on synthetic particle images and experiments in a strongly excited turbulent jet.
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Norasia, Yolanda, Mohamad Tafrikan i Bhamakerti Hafiz Kamaluddin. "ANALYSIS OF THE MAGNETOHYDRODYNAMICS NANOVISCOUS FLUID BASED ON VOLUME FRACTION AND THERMOPHYSICAL PROPERTIES". BAREKENG: Jurnal Ilmu Matematika dan Terapan 17, nr 1 (16.04.2023): 0331–40. http://dx.doi.org/10.30598/barekengvol17iss1pp0331-0340.

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Fluid flow control is applied in engineering and industry using computational fluid dynamics. Based on density, fluids are divided into two parts, namely non-viscous fluids and viscous fluids. Nanofluid is a fluid that has non-viscous and viscous characteristics. Nanoviscos fluid flow is interesting to study by considering the effect of volume fraction and thermophysical properties. Nanoviscous fluid flow models form dimensional equations that are then simplified into dimensionless equations. Dimensionless equations are converted into non-similar equations using flow functions and non-similar variables. Nanoviscous fluids with Cu particles and water-based fluids have higher temperatures and faster velocity. Based on the effect of volume fraction, the velocity of the nanoviscous fluid moves slower, while the temperature of the nanoviscous fluid increases.
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N, Rajiv Kumar, Umar Ahamed P i Mohamed Anwar A. U. "CFD Analysis of Fluid Flow in Sand Casting". International Journal of Trend in Scientific Research and Development Volume-3, Issue-2 (28.02.2019): 905–13. http://dx.doi.org/10.31142/ijtsrd21553.

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TANNER, P. W. GEOFF. "Metamorphic fluid flow". Nature 352, nr 6335 (sierpień 1991): 483–84. http://dx.doi.org/10.1038/352483a0.

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YARDLEY, BRUCE, SIMON H. BOTTRELL i R. A. CLIFF. "Metamorphic fluid flow". Nature 352, nr 6335 (sierpień 1991): 484. http://dx.doi.org/10.1038/352484a0.

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Hutnak, Michael. "Seabed Fluid Flow". Geofluids 7, nr 4 (listopad 2007): 468–69. http://dx.doi.org/10.1111/j.1468-8123.2007.00189.x.

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GILLILAND, MELISSA. "TRACKING FLUID FLOW". Nursing 25, nr 7 (lipiec 1995): 72. http://dx.doi.org/10.1097/00152193-199507000-00028.

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Rozprawy doktorskie na temat "Fluid flow"

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Marshall, G. S. "Muiticomponent fluid flow computation". Thesis, Teesside University, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.384659.

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Paleo, Cageao Paloma. "Fluid-particle interaction in geophysical flows : debris flow". Thesis, University of Nottingham, 2014. http://eprints.nottingham.ac.uk/27808/.

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Small scale laboratory experiments were conducted to study the dynamic mor- phology and rheological behaviour of fluid-particle mixtures, such as snout-body architecture, levee formation, deposition and particle segregation effects. Debris flows consist of an agitated mixture of rock and sediment saturated with water. They are mobilized under the influence of gravity from hill slopes and channels and can reach long run-out distance and have extremely destructive power. Better understanding of the mechanisms that govern these flows is required to assess and mitigate the hazard of debris flows and similar geophysical flows. Debris flow models are required to accurately deal with evolving behaviours in space and time, to be able to predict flow height, velocity profiles and run-out distances and shapes. The evolution of laboratory debris flows, both dry glass beads and mixtures with water or glycerol, released from behind a lock gate to flow down an inclined flume, was observed through the channel side wall and captured with high speed video and PIV analysis to provide velocity profiles through out the flow depth. Pore pressure and the normal and shear stress at the base of the flow were also measured. Distinct regions were characterized by the non-fluctuating region and the in- termittent granular cloud surrounding the flows. The extent of these regions was shown to be related to flow properties. The separation of these two regions allowed the systematic definition of bulk flow characteristics such as characteristic height and flow front position. Laboratory flows showed variations in morphology and rheological characteristics under the influence of particle size, roughness element diameter, interstitial fluid viscosity and solid volume fraction. Mono-dispersed and poly-dispersed components mixed with liquids without fine sediments, reveal a head and body structure and an appearance similar to the classic anatomy of real debris flows. Unsaturated fronts were observed in mono-dispersed flows, suggesting that particle segregation is not the only mechanism. A numerical simulation of laboratory debris flows using the computer model RAMMS (RApid Mass Movements Simulation) was tested with dry laboratory flows, showing close similarity to calculated mean velocities.
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Oswell, J. E. "Fluid loading with mean flow". Thesis, University of Cambridge, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239158.

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Padley, Robert William. "Fluid flow past rotating bodies". Thesis, University of Leeds, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.396927.

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Cooper, Laura. "Investigations of lymphatic fluid flow". Thesis, University of Southampton, 2016. https://eprints.soton.ac.uk/393578/.

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The lymphatic system returns fluid to the blood stream from the tissues to maintain tissue fluid homeostasis. The collecting lymphatic vessels actively pump fluid against a body scale pressure gradient, i.e., from tissue interstitial space to the venous side of the blood circulatory system. The collecting lymphatic vessels pass the lymphatic fluid to lymph nodes that filter the lymph before it is returned to the circulatory system. This thesis presents work undertaken to create a fluid structure interaction model of a lymph node with afferent and efferent lymphatic vessels. The model is built in COMSOL Multiphysics, a commercial finite element software. Four pieces of novel work are presented in this thesis. Firstly, an optimisation method used to approximate the material properties for the collecting lymphatic vessel from the pressure diameter behaviour. Secondly, model of the collecting lymphatic valve with surrounding wall used to investigate valve closing behaviour. Thirdly, an image based model of a lymph node where the material properties are optimised to experimental data and based on selective plane illumination microscopy images. Finally, an image based model of a lymph node based on computed tomography images that shows how the structure within the node affects the fluid flow pathways.
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Barker, Shaun, i sbarker@eos ubc ca. "Dynamics of fluid flow and fluid chemistry during crustal shortening". The Australian National University. Research School of Earth Sciences, 2007. http://thesis.anu.edu.au./public/adt-ANU20090711.074630.

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In this thesis, an integrated structural and chemical approach has been used to investigate the spatial and temporal evolution of fluid chemistry, and fluid flow pathways, during crustal shortening. The Taemas Vein Swarm is hosted in a limestone-shale sequence, the Murrumbidgee Group, in the Eastern Belt of the Lachlan Orogen, in New South Wales, Australia. The Taemas Vein Swarm (TVS) is composed of calcite ± quartz veins, hosted in a series of faults and fractures, which extends over an area of approximately 20 km2. The Murrumbidgee Group is composed of several formations, comprising massive grey micritic limestones, redbed sandstones and shales,and thinly interbedded (10–20 cm scale) limestones and shales. ¶ The sedimentary sequence has been folded into a series of upright, open to close folds, and was probably deformed during either mid-late Devonian, or early Carboniferous, crustal shortening. To the east, the Murrumbidgee Group is overthrust by a Silurian volcanic sedimentary sequence along the Deakin-Warroo Fault System. Crosscutting and overprinting relationships demonstrate that vein growth was synchronous with folding, with different vein types related to different fold mechanisms at various stages of fold growth. ¶ Flexural slip folding led to the development of bedding-concordant veins (hereafter called bedding-parallel veins). Flexural flow in semicompetent to incompetent beds caused en echelon extension vein arrays to grow. Decoupling between beds, and dilatancy at fold hinges led to significant vein growth. In addition, fold lock-up led to limb-parallel stretching, and the growth of bedding-orthogonal extension fractures. ¶ Vein growth is inferred to have occurred in a compressional tectonic regime (i.e. sigma3=vertical). Oxygen isotope quartz-calcite thermometry suggests that veins formed at temperatures of 100–200 oC. The depth of vein formation may have been between about 5 and 8 km. Vein textures indicate that growth of veins occurred during multiple cycles of permeability enhancement and destruction. Subhorizontal extension fractures, and faults at unfavourable angles for reactivation, imply that fluid pressures exceeded lithostatic levels during the growth of some veins. Coexisting extension and shear fractures imply that differential stress levels varied over time. ¶ Flexural slip continued throughout folding at Taemas, despite some fold limbs being at angles extremely unfavourable for reactivation ( > 60). As folds approached frictional lock-up, flexural slip continued to occur when supralithostatic fluid pressures were developed. Therefore, large, bedding-discordant faults were not developed to accommodate strain during folding, explaining a deficiency of larger faults in the TVS. ¶ Infiltration of overpressured fluids occurred into the base of the Murrumbidgee Group, and was channelled into a distributed mesh of small faults and fractures. At the point that a connected ‘backbone’ flow network developed in the TVS, highpressure fluids would no longer be available to allow continuing flexural slip on fold limbs approaching lockup. Thereafter, larger faults would develop, which would adjust the fault population in the TVS to a more ‘typical’ displacement-frequency distribution. This had not occurred in the Taemas area by the time crustal shortening ceased. An abundance of small faults, and fracturing driven by invasion of overpressured fluid, implies that the TVS formed via an ‘earthquake swarm’ process. ¶ Modern analytical techniques, utilising laser ablation sampling technology, allow high-spatial resolution chemical data to be collected from syntectonic veins. Insights into the role that fluid-mineral interface processes may have on the chemistry of minerals grown in syntectonic veins were provided by an experimental study. Moderate sized ( < 1−5 mm) synthetic calcite crystals were successfully grown to investigate the uptake of rare earth elements (REE) into calcite. Changes in crystal morphology are linked to variable solution chemistry, which has important implications for the interpretation of hydrothermal vein textures. High-spatial resolution chemical analyses of synthetic calcite crystals demonstrate significant fluctuations in REE concentrations over distances of < 200 μm within calcite crystals. Time-equivalent regions on different crystal faces have significantly different REE concentrations, indicating that fluctuations in calcite trace element composition cannot be interpreted exclusively in terms of changing ‘bulk fluid’ composition. Rare earth element anomalies (Eu/Eu* and Ce/Ce*) are not significantly influenced by compositional zoning, and may be robust indicators of changes in solution bulk chemistry and fluid oxidation state. ¶ Changes in isotopic ratios (13C, 18O and 87Sr/86Sr), and trace element concentrations in veins from the TVS are related to variations in fluid source, flow pathways and chemical conditions (e.g. trace element complexation, precipitation rate, fluid oxidation) during hydrothermal fluid flow. This integrated structural, textural and chemical approach has direct application to the examination of hydrothermal veins in fracture-hosted ore deposits, and may allow the fluid source and/or chemical conditions conducive to the formation of high-grade ore to be discerned. ¶ Vein 18O compositions systematically increase upwards through the Murrumbidgee Group, caused by progressive reaction of an externally derived, low-18O fluid (of probable meteoric origin) with host limestones. Vein 18O and 87Sr/86Sr compositions vary spatially and temporally within the same outcrop, and within individual veins, which is inferred to be caused by the ascent of packages of fluid along constantly changing flow pathways. Fluid-buffered oxygen isotope ratios at the earliest stages of deformation imply that the TVS formed via an ‘invasion percolation’ process. Fluid pathways are inferred to have changed constantly, with fractures ‘toggleswitching’ between high-permeability and low-permeability states, due to repeated fracture opening and sealing events.
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Yan, Baoshe. "Fluid flow induced by oscillating bodies and flows in cyclones". Thesis, University of Leeds, 1991. http://etheses.whiterose.ac.uk/435/.

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In this thesis the following aspects have been investigated: (i) the numerical solutions for unsteady 2-dimensional, incompressible viscous fluid flows induced by a harmonically oscillating cascade, and (ii) the fluid flows in industrial cyclones and their separation efficiencies. In the first part of the thesis we deal with fluid flows induced by harmonically oscillating cascades of cylinders with different cross sectional shapes. Numerical solutions for large amplitude oscillations of a cascade of normal flat plates are obtained by using a finite-difference method and it is found that solutions are in good agreement with some related experimental results. For small amplitude oscillations a perturbation method, series truncation technique and finite-difference methods are used to obtain solutions for cascades of normal flat plates and square cylinders. By assuming that the streaming Reynolds number is 0(1) then the outer streaming flows for cascades of square cylinders, normal flat plates and circular cylinders are investigated numerically for the streaming Reynolds number Rs up to 70. Conformal mapping, grid generation and boundary element methods are used to deal with the different geometries in order to determine the outer potential flows. For small values of the streaming Reynolds number it is found experimentally that the flow remains symmetrical and the numerically predicted fluid flow is in good agreement with the experimental results. As the value of the streaming Reynolds number increases then it is found experimentally that the flow develops asymmetries and this occurs when 8
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Kalb, Virginia L. "Low-dimensional models for fluid flow". College Park, Md. : University of Maryland, 2004. http://hdl.handle.net/1903/1846.

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Thesis (Ph. D.) -- University of Maryland, College Park, 2004.
Thesis research directed by: Mathematics. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.
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Shook, Andrew A. "Fluid flow in horizontal injection regimes". Thesis, University of British Columbia, 1986. http://hdl.handle.net/2429/26738.

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Physical and mathematical modelling studies have been performed to investigate liquid flow driven by a horizontally injected gas. The experimental work consisted of water velocity measurements made at 100 locations within a plexiglass tank. Air was introduced into the tank through a series of side-mounted tuyeres, and the effect of air flowrate on water recirculation velocity was observed. The results of the experiments indicate that the maximum water velocity occurs at the water surface. The effect of bubbles coalescing from adjacent tuyeres was observed with increasing air flowrate, and was found to diminish the water recirculation rate. The mathematical model employed a variant of the Marker and Cell (MAC) technique to compute fluid flow with a free surface. The model predictions indicate that the flow in the experimental tank is largely driven by water flowing across the free surface. Based on this knowledge, qualitative predictions of the flow regimes in a Peirce-Smith copper converter and a zinc slag fuming furnace were made.
Applied Science, Faculty of
Mining Engineering, Keevil Institute of
Graduate
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Pettersson, Patrik. "Fluid flow in wood fiber network". Licentiate thesis, Luleå tekniska universitet, Strömningslära och experimentell mekanik, 2006. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26639.

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Cellulose material is processed to pulp suspensions and MDF boards in order to produce products such as papers, magazines, laminate floors or door skins. A critical stage of these processes is when the cellulose fiber networks are compressed to specific densities and when most of the fluid originally positioned between and inside the fibers is forced to leave the network. The fiber network is then exposed to a drag force generated by the flow. The magnitude of this force is dependent upon how easy the fluid can flow through the network, which is commonly described by its permeability. In addition to the permeability, which relates to the drag on each fiber, there is a solid network force. The response to this force from the fiber network is often termed as the compressibility of it. Hence, to be able to model and predict the compression stage in cellulose material related processes these two material properties must be known. In this thesis two equipments to measure the permeability of MDF networks and pulp suspensions are evaluated and a neat model for a part of the MDF- compression stage is developed. A reference material consisting of spherical particles and relevant fiber networks are used as test objects for the equipments enabling a comparison to theoretical models and existing experimental results. The outcome is that correct enough permeability data are obtained with respective equipment as long as Reynolds number is sufficiently low. The equipments are then used to study different materials showing, for instance, that highly compressed MDF-networks are strongly anisotropic as to permeability and that the tested hardwood pulps have an overall higher permeability compared to the softwood pulps investigated. It was also found that the permeability of the pulps was not influenced by different mechanical treatments of the fiber network, as long as the geometrical dimensions of the fibers were constants.

Godkänd; 2006; 20070109 (haneit)

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Książki na temat "Fluid flow"

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Cabrera, E., Universidad Politecnica de Valencia i Spain. Fluid Flow Modelling. Abingdon, UK: Taylor & Francis, 1992. http://dx.doi.org/10.4324/9780203213599.

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Orlandi, Paolo, red. Fluid Flow Phenomena. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-011-4281-6.

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Vad, János, Tamás Lajos i Rudolf Schilling, red. Modelling Fluid Flow. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-08797-8.

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Viscous fluid flow. Wyd. 2. New York: McGraw-Hill, 1991.

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Viscous fluid flow. Wyd. 3. New York, NY: McGraw-Hill Higher Education, 2006.

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May, Douglass H. Conduit fluid flow. [Bloomington, IN?]: AuthorHouse, 2004.

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Saad, Michel A. Compressible fluid flow. Wyd. 2. Englewood Cliffs, N.J: Prentice Hall, 1993.

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C, Georgiou Georgios, i Alexandrou Andreas N, red. Viscous fluid flow. Boca Raton, FL: CRC Press, 2000.

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Bacon, D. H. Real fluid flow. Oxford: Butterworth Heinemann, 1990.

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Compressible fluid flow. Englewood Cliffs, N.J: Prentice-Hall, 1985.

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Części książek na temat "Fluid flow"

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Parker, David F. "Fluid Flow". W Springer Undergraduate Mathematics Series, 101–31. London: Springer London, 2003. http://dx.doi.org/10.1007/978-1-4471-0019-5_6.

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Cracknell, P. S., i R. W. Dyson. "Fluid flow". W Handbook of Thermoplastics Injection Mould Design, 21–33. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-015-7209-5_3.

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Field, Robert W. "Fluid Flow". W Chemical Engineering, 52–61. London: Macmillan Education UK, 1988. http://dx.doi.org/10.1007/978-1-349-09840-8_3.

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Philipse, Albert P. "Fluid Flow". W Brownian Motion, 93–103. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-98053-9_7.

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Anandharamakrishnan, C., i S. Padma Ishwarya. "Fluid Flow". W Essentials and Applications of Food Engineering, 117–57. Boca Raton : CRC Press, Taylor & Francis Group, 2019.: CRC Press, 2019. http://dx.doi.org/10.1201/9780429430244-4.

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Nichols, Daniel H. "Fluid Flow". W Physics for Technology, 151–66. Second edition. | Boca Raton : CRC Press, Taylor & Francis: CRC Press, 2018. http://dx.doi.org/10.1201/9781351207270-9.

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Wilhelm, Luther R., Dwayne A. Suter i and Gerald H. Brusewitz. "Fluid Flow". W Food & Process Engineering Technology, 65–110. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2004. http://dx.doi.org/10.13031/2013.17552.

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Block, David E., i Konrad V. Miller. "Fluid Flow". W Unit Operations in Winery, Brewery, and Distillery Design, 29–76. Boca Raton: CRC Press, 2021. http://dx.doi.org/10.1201/9781003097495-3.

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Chaurasia, Ashish S. "Fluid Flow". W Computational Fluid Dynamics and Comsol Multiphysics, 143–98. Boca Raton: Apple Academic Press, 2021. http://dx.doi.org/10.1201/9781003180500-4.

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Yu, Jiyang. "Fluid Flow". W Fundamental Principles of Nuclear Engineering, 99–121. Singapore: Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-0839-1_4.

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Streszczenia konferencji na temat "Fluid flow"

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Zitha, P. L. J., i F. Wessel. "Fluid Flow Control Using Magnetorheological Fluids". W SPE/DOE Improved Oil Recovery Symposium. Society of Petroleum Engineers, 2002. http://dx.doi.org/10.2118/75144-ms.

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Harris, Scott, Richard Miles i Walter Lempert. "PHANTOMM flow tagging measurements in complex 3D flows". W Fluid Dynamics Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1996. http://dx.doi.org/10.2514/6.1996-1966.

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Myers, T. M., A. W. Marshall i H. R. Baum. "Simplified modeling of sprinkler head fluid mechanics". W MULTIPHASE FLOW 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/mpf130211.

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Zhang, Xuizhang, i Don Boyer. "Mean flow generation in a rotating homogeneous flow". W Theroretical Fluid Mechanics Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1996. http://dx.doi.org/10.2514/6.1996-2146.

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Owens, Lewis R., George B. Beeler, Ponnampalam Balakumar i Patrick McGuire. "Flow Disturbance and Surface Roughness Effects on Cross-Flow Boundary-Layer Transition in Supersonic Flows". W 44th AIAA Fluid Dynamics Conference. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2014. http://dx.doi.org/10.2514/6.2014-2638.

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Fernando, H. J. S., i G. Wang. "ENVIRONMENTAL FLUID MOTIONS". W First Symposium on Turbulence and Shear Flow Phenomena. Connecticut: Begellhouse, 1999. http://dx.doi.org/10.1615/tsfp1.20.

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Zadravec, M., M. Hriberšek i L. Škerget. "Micropolar fluid flow modelling using the boundary element method". W MULTIPHASE FLOW 2007. Southampton, UK: WIT Press, 2007. http://dx.doi.org/10.2495/mpf070311.

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El-Sadi, H., i N. Esmail. "Numerical modelling of colloidal fluid in a viscous micropump". W MULTIPHASE FLOW 2007. Southampton, UK: WIT Press, 2007. http://dx.doi.org/10.2495/mpf070321.

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Behrouzi, Parviz, i Jim McGuirk. "Jet Mixing Enhancement Using Fluid Tabs". W 2nd AIAA Flow Control Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2004. http://dx.doi.org/10.2514/6.2004-2401.

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Ruetten, Markus, i Fithawi Woldegiorgis. "Vortical Flow Structure Genesis of Lobed Nozzle Flows". W 46th AIAA Fluid Dynamics Conference. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2016. http://dx.doi.org/10.2514/6.2016-4345.

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Raporty organizacyjne na temat "Fluid flow"

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Hair. L51725 Drilling Fluids in Pipeline Installation by Horizontal Directional Drilling-Practical Applications. Chantilly, Virginia: Pipeline Research Council International, Inc. (PRCI), październik 1994. http://dx.doi.org/10.55274/r0010163.

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Drilling fluid plays a key role in the installation of a pipeline by horizontal directional drilling (HDD) and accounts for the majority of the associated environmental impact. An improper drilling fluid program can result in stuck pipe. Uncontrolled discharge of drilling fluid downhole can damage or undermine adjacent structures.The cost of drilling fluid involved with pipeline installation, particularly when disposal costs are considered, can be substantial. This manual is the principal product of PRC project PR-227-9321. Its purpose is to increase the level of technical sophistication relative to drilling fluids used in the installation of pipelines by Horizontal Directional Drilling (HDD). It is anticipated that this increase will benefit the natural gas industry through reductions in HDD installation costs and environmental impact. The manual contains six sections which address the following general topics: 1 . The HDD installation process, the specific functions of drilling fluids in pipeline installation by HDD, and the composition of drilling fluids; 2. Characteristics of drilling fluid flow, pertinent properties of drilling fluids, and calculation methods relative to drilling fluid flow circuits; 3. Standard classification of soil and rock structures and soil and rock properties relative to drilling fluid flow; 4. The behavior of soil and rock structures relative to drilling fluid flow, general drilling fluid criteria, and general solutions to drilling problems; 5. Methods for estimating drilling fluid quantities, methods for disposing of excess drilling fluids, the environmental impact of drilling fluids used in HDD, and construction specifications relative to drilling fluids; and 6. Materials used drilling fluids.
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Kirkpatrick, J. R. Fluid flow effects on electroplating. Office of Scientific and Technical Information (OSTI), wrzesień 1990. http://dx.doi.org/10.2172/6430941.

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Holub, Oleksandr, Mykhailo Moiseienko i Natalia Moiseienko. Fluid Flow Modelling in Houdini. [б. в.], listopad 2020. http://dx.doi.org/10.31812/123456789/4128.

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The modern educational environment in the field of physics and information technology ensures the widespread use of visualization software for successful and deep memorization of material. There are many software for creating graphic objects for presentations and demonstrations, the most popular of which were analyzed. The work is devoted to the visualization of liquids with different viscosity parameters. The article describes the development of a fluid model in the form of a particle stream. The proposed methodology involves using the Houdini application to create interactive models. The developed model can be used in the educational process in the field of information technology.
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Kingston, A. W., i O. H. Ardakani. Diagenetic fluid flow and hydrocarbon migration in the Montney Formation, British Columbia: fluid inclusion and stable isotope evidence. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330947.

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The Montney Formation in Alberta and British Columbia, Canada is an early Triassic siltstone currently in an active diagenetic environment at depths greater than 1,000 m, but with maximum burial depths potentially exceeding 5,000 m (Ness, 2001). It has undergone multiple phases of burial and uplift and there is strong evidence for multiple generations of hydrocarbon maturation/migration. Understanding the origin and history of diagenetic fluids within these systems helps to unravel the chemical changes that have occurred since deposition. Many cores taken near the deformation front display abundant calcite-filled fractures including vertical or sub-vertical, bedding plane parallel (beefs), and brecciated horizons with complex mixtures of vertical and horizontal components. We analyzed vertical and brecciated horizons to assess the timing and origin of fluid flow and its implications for diagenetic history of the Montney Fm. Aqueous and petroleum bearing fluid inclusions were observed in both vertical and brecciated zones; however, they did not occur in the same fluid inclusion assemblages. Petroleum inclusions occur as secondary fluid inclusions (e.g. in healed fractures and along cleavage planes) alongside primary aqueous inclusions indicating petroleum inclusions post-date aqueous inclusions and suggest multiple phases of fluid flow is recorded within these fractures. Raman spectroscopy of aqueous inclusions also display no evidence of petroleum compounds supporting the absence or low abundance of petroleum fluids during the formation of aqueous fluid inclusions. Pressure-corrected trapping temperatures (&amp;gt;140°C) are likely associated with the period of maximum burial during the Laramide orogeny based on burial history modelling. Ice melt temperatures of aqueous fluid inclusions are consistent with 19% NaCl equiv. brine and eutectic temperatures (-51°C) indicate NaCl-CaCl2 composition. Combined use of aqueous and petroleum fluid inclusions in deeply buried sedimentary systems offers a promising tool for better understanding the diagenetic fluid history and helps constrain the pressure-temperature history important for characterizing economically important geologic formations.
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Gibson, J. S. Joint Research on Computational Fluid Dynamics and Fluid Flow Control. Fort Belvoir, VA: Defense Technical Information Center, listopad 1995. http://dx.doi.org/10.21236/ada308103.

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Cortez, Ricardo. Impulse-based methods for fluid flow. Office of Scientific and Technical Information (OSTI), maj 1995. http://dx.doi.org/10.2172/87798.

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Garabedian, Paul R. Computational Fluid Dynamics and Transonic Flow. Fort Belvoir, VA: Defense Technical Information Center, październik 1994. http://dx.doi.org/10.21236/ada288962.

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Kodres, Cal, i Gene Cooper. Solve Fluid Flow Problems With PHOENICS. Fort Belvoir, VA: Defense Technical Information Center, listopad 1993. http://dx.doi.org/10.21236/ada289702.

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Garabedian, Paul R. Computational Fluid Dynamics and Transonic Flow. Fort Belvoir, VA: Defense Technical Information Center, październik 1994. http://dx.doi.org/10.21236/ada292797.

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Patnaik, Soumya S., Eugeniya Iskrenova-Ekiert i Hui Wan. Multiscale Modeling of Multiphase Fluid Flow. Fort Belvoir, VA: Defense Technical Information Center, sierpień 2016. http://dx.doi.org/10.21236/ad1016834.

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