2012
DOI: 10.1155/2012/268371
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A Numerical Study on Flow around Nonuniform Porous Fences

Abstract: The effects of a porous fence with a nonuniform porosity on flow fields are investigated numerically. First, an experiment with a non-uniform porous fence located in a wind tunnel is performed to obtain a reference data set. Then, a numerical model that utilizes the finite volume scheme with a weakly compressible-flow method to solve the continuity and momentum equations is developed. The numerical simulation is compared to experimental measurements for validation purposes. As a result, the numerical predictio… Show more

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Cited by 14 publications
(24 citation statements)
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“…The reason for this kind of phenomenon is that the spatial structure of forest belt affecting the microclimate would change the PM mass concentration inside the shelterbelt. In general, airflow through the forest belt can be divided into two parts: when lower air flow encounters the shelterbelt, owing to a blocking effect by the shelterbelt, part of the airflow moves directly through the shelterbelt gap; the friction between the airflow and the tree consumes more energy of the flow and causes the kinetic energy of the airflow to drop, which leads to the wind speed reducing [66][67][68][69]. The reduction in wind in the shelterbelt, not conducive to the spread of PM, which is prone to settlement, eventually leads to an increase in PM mass concentration.…”
Section: Particulate Mass Concentration Variation In Different Locatimentioning
confidence: 99%
“…The reason for this kind of phenomenon is that the spatial structure of forest belt affecting the microclimate would change the PM mass concentration inside the shelterbelt. In general, airflow through the forest belt can be divided into two parts: when lower air flow encounters the shelterbelt, owing to a blocking effect by the shelterbelt, part of the airflow moves directly through the shelterbelt gap; the friction between the airflow and the tree consumes more energy of the flow and causes the kinetic energy of the airflow to drop, which leads to the wind speed reducing [66][67][68][69]. The reduction in wind in the shelterbelt, not conducive to the spread of PM, which is prone to settlement, eventually leads to an increase in PM mass concentration.…”
Section: Particulate Mass Concentration Variation In Different Locatimentioning
confidence: 99%
“…x 11.2 Background ...........................................................................................297 11.3 Study Site and Experimental Needs .....................................................300 11.4 CRP Overview ......................................................................................304 11.5 CRP Implementation ............................................................................307 11.5.1 Components customization and experimental arrangement .......307 11.5.2 Experimental protocols ...............................................................308 11.6 CRP Sensitivity and Accuracy Analysis ...............................................310 11.6.1 Effect of the density and distribution of the ground control points .. ...................................................................................................311 11.6.2 Surface texture ............................................................................312 11.6.3 CRP mapping accuracy ..............................................................313 11.7 Tracking Snow Deposition during a Strom Event ................................315 11.8 Conclusions...........................................................................................317 CHAPTER 12 CONCLUSIONS AND FUTURE WORK ..............................................333 REFERENCES ................................................................................................................337 xi LIST OF TABLES Table 2.1 Protection Index (PI) values predicted by Huang et al (2012) representing areas under contours line u/u0=0.1, 0.3 and 0.5 behind a porous fence with nonuniform porosity (see also xii LIST OF FIGURES Figure 1.1 Flow including separation and reattachment zone around an obstacle or windbreak (Raine and Stevenson, 1977). Note that for high porosities, upwind and downwind recirculation regions may be absent.…”
Section: Public Abstractmentioning
confidence: 99%
“….................47 Figure 2.9 Mean streamwise velocity (u/U0) and vertical velocity (v/U0) profiles in the wake of a porous fence (P=38.5%) with varying hole diameters d=1.4mm, d=2.1mm and d=2.8mm. From Kim and Lee (2001), where U0 is the incoming flow velocity, H is the height of .12 Mean streamline patterns around the fence design studied by Huang et al (2012), where H is the total height of the fence; i) sketch of fence design indicating the mean porosity value within the lower half of the fence (ƐL) and the mean porosity value within the upper half of the fence (ƐU) of the fence; ii) 2D mean streamline patterns for the five designs tested. .…”
Section: Public Abstractmentioning
confidence: 99%
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