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Relevant bibliographies by topics / Streamline density

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Journal articles

Academic literature on the topic 'Streamline density'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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Journal articles on the topic "Streamline density"

1

Cheng, Hao, Ichiro Osako, Akhil Datta-Gupta, and Michael J. King. "A Rigorous Compressible Streamline Formulation for Two and Three-Phase Black-Oil Simulation." SPE Journal 11, no. 04 (2006): 407–17. http://dx.doi.org/10.2118/96866-pa.

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Summary Streamline simulators have received increased attention in the petroleum industry because of their ability to effectively handle multimillion-cell detailed geologic models and large simulation models. The efficiency of streamline simulation has relied primarily on the decoupling of the 3D saturation equation into 1D equations along streamlines using the streamline time of flight as the spatial coordinate. Until now, this decoupling has been strictly valid for incompressible flow. Applications to compressible flow have generally lacked strong theoretical foundations, and very often yiel

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2

Hollister, Brad E., and Alex Pang. "Uncertainty Rank for Streamline Ensembles." Journal of Imaging Science and Technology 64, no. 2 (2020): 20504–1. http://dx.doi.org/10.2352/j.imagingsci.technol.2020.64.2.020504.

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Abstract Traditional spaghetti plots from ensemble data provide no explicit information as to the uncertainty of the realization flow paths. While intuitive assessment can be used when visualizing streamline density directly in such a plot, the display is often cluttered and difficult to interpret. The authors present a method to measure uncertainty and visualize member streamlines from an ensemble of vector fields. The method incorporates velocity probability density as a feature along each member streamline. The authors show visualizations of two different data sets using the proposed method

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3

Treguier, A. M., M. England, S. R. Rintoul, G. Madec, J. Le Sommer, and J. M. Molines. "Southern Ocean overturning across streamlines in an eddying simulation of the Antarctic Circumpolar Current." Ocean Science Discussions 4, no. 4 (2007): 653–98. http://dx.doi.org/10.5194/osd-4-653-2007.

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Abstract. An eddying global model is used to study the characteristics of the Antarctic Circumpolar Current (ACC) in a streamline-following framework. In the upper layers, the meridional circulation across streamlines agrees with the theoretical view: an equatorward mean flow partially cancelled by a poleward eddy mass flux. The same calculation in a zonal average gives a completely different view and underestimates the eddy effects. Two model simulations, in which the buoyancy forcing above the ACC changes from positive to negative, suggest that the relationship between the residual meridiona

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4

Cortesi, Matteo, Giorgio Gatta, Giovanni Michielon, Rocco Di Michele, Sandro Bartolomei, and Raffaele Scurati. "Passive Drag in Young Swimmers: Effects of Body Composition, Morphology and Gliding Position." International Journal of Environmental Research and Public Health 17, no. 6 (2020): 2002. http://dx.doi.org/10.3390/ijerph17062002.

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The passive drag (Dp) during swimming is affected by the swimmer’s morphology, body density and body position. We evaluated the relative contribution of morphology, body composition, and body position adjustments in the prediction of a swimmer’s Dp. This observational study examined a sample of 60 competitive swimmers (31 male and 29 female) with a mean (±SD) age of 15.4 ± 3.1 years. The swimmer’s Dp was measured using an electro-mechanical towing device and the body composition was assessed using a bioelectrical impedance analyser. Body lengths and circumferences were measured in both the sta

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5

Cherni, Emna, Benoît Champagne, Sameh Ayadi, and Vincent Liégeois. "Magnetically-induced current density investigation in carbohelicenes and azahelicenes." Physical Chemistry Chemical Physics 21, no. 27 (2019): 14678–91. http://dx.doi.org/10.1039/c9cp02071c.

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6

Treguier, A. M., M. H. England, S. R. Rintoul, G. Madec, J. Le Sommer, and J. M. Molines. "Southern Ocean overturning across streamlines in an eddying simulation of the Antarctic Circumpolar Current." Ocean Science 3, no. 4 (2007): 491–507. http://dx.doi.org/10.5194/os-3-491-2007.

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Abstract. An eddying global model is used to study the characteristics of the Antarctic Circumpolar Current (ACC) in a streamline-following framework. Previous model-based estimates of the meridional circulation were calculated using zonal averages: this method leads to a counter-intuitive poleward circulation of the less dense waters, and underestimates the eddy effects. We show that on the contrary, the upper ocean circulation across streamlines agrees with the theoretical view: an equatorward mean flow partially cancelled by a poleward eddy mass flux. Two model simulations, in which the buo

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7

Song, P., C. T. Russell, J. T. Gosling, M. Thomsen, and R. C. Elphic. "Observations of the density profile in the magnetosheath near the stagnation streamline." Geophysical Research Letters 17, no. 11 (1990): 2035–38. http://dx.doi.org/10.1029/gl017i011p02035.

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8

Cheng, Hao, Adedayo Stephen Oyerinde, Akhil Datta-Gupta, and William J. Milliken. "Compressible Streamlines and Three-Phase History Matching." SPE Journal 12, no. 04 (2007): 475–85. http://dx.doi.org/10.2118/99465-pa.

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Summary Reconciling high-resolution geologic models to field production history is still by far the most time-consuming aspect of the workflow for both geoscientists and engineers. Recently, streamline-based assisted and automatic history-matching techniques have shown great potential in this regard, and several field applications have demonstrated the feasibility of the approach. However, most of these applications have been limited to two-phase water/oil flow under incompressible or slightly compressible conditions. We propose an approach to history matching three-phase flow using a novel co

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9

WU, ZUO-BING. "STREAMLINE TOPOLOGY AND DILUTE PARTICLE DYNAMICS IN A KÁRMÁN VORTEX STREET FLOW." International Journal of Bifurcation and Chaos 13, no. 05 (2003): 1275–86. http://dx.doi.org/10.1142/s0218127403007217.

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Three types of streamline topology in a Kármán vortex street flow are shown under the variation of spatial parameters. For the motion of dilute particles in the Kármán vortex street flow, there exist a route of bifurcation to a chaotic orbit and more attractors in a bifurcation diagram for the proportion of particle density to fluid density. Along with the increase of spatial parameters in the flow field, the bifurcation process is suspended, as well as more and more attractors emerge. In the motion of dilute particles, a drag term and gravity term dominate and result in the bifurcation phenom

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10

Snyder, William H., Roger S. Thompson, Robert E. Eskridge, et al. "The structure of strongly stratified flow over hills: dividing-streamline concept." Journal of Fluid Mechanics 152 (March 1985): 249–88. http://dx.doi.org/10.1017/s0022112085000684.

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In stably stratified flow over a three-dimensional hill, we can define a dividing streamline that separates those streamlines that pass around the hill from those that pass over the hill. The height Hs of this dividing streamline can be estimated by Sheppard's simple energy argument; fluid parcels originating far upstream of a hill at an elevation above Hs have sufficient kinetic energy to rise over the top, whereas those below Hs must pass around the sides. This prediction provides the basis for analysing an extensive range of laboratory observations and measurements of stably stratified flow

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