Academic literature on the topic 'Reynolds Range'
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Journal articles on the topic "Reynolds Range"
Horiguchi, Hironori, Daisuke Yumiba, Yoshinobu Tsujimoto, Masaaki Sakagami, and Shigeo Tanaka. "Reynolds Number Effect on Regenerative Pump Performance in Low Reynolds Number Range." International Journal of Fluid Machinery and Systems 1, no. 1 (August 1, 2008): 101–8. http://dx.doi.org/10.5293/ijfms.2008.1.1.101.
Full textCastaing, B., and Y. Gagne. "Inertial and dissipative range intermittency at high Reynolds numbers." Physica Scripta T49A (January 1, 1993): 74–76. http://dx.doi.org/10.1088/0031-8949/1993/t49a/011.
Full textHORIGUCHI, Hironori, Daisuke YUMIBA, Yoshinobu TSUJIMOTO, Masaaki SAKAGAMI, and Shigeo TANAKA. "Reynolds Number Effect for the Performance of Regenerative Pump in the Range of Low Reynolds Number." Transactions of the Japan Society of Mechanical Engineers Series B 73, no. 735 (2007): 2260–68. http://dx.doi.org/10.1299/kikaib.73.2260.
Full textFARAZMAND, M. M., N. K. R. KEVLAHAN, and B. PROTAS. "Controlling the dual cascade of two-dimensional turbulence." Journal of Fluid Mechanics 668 (November 30, 2010): 202–22. http://dx.doi.org/10.1017/s0022112010004635.
Full textQian, J. "Inertial range and the finite Reynolds number effect of turbulence." Physical Review E 55, no. 1 (January 1, 1997): 337–42. http://dx.doi.org/10.1103/physreve.55.337.
Full textHollenberg, J. W. "Reynolds Number Effects on Regenerative Pump Performance." Journal of Engineering for Industry 109, no. 4 (November 1, 1987): 392–95. http://dx.doi.org/10.1115/1.3187144.
Full textMichna, Jan, and Krzysztof Rogowski. "Numerical Study of the Effect of the Reynolds Number and the Turbulence Intensity on the Performance of the NACA 0018 Airfoil at the Low Reynolds Number Regime." Processes 10, no. 5 (May 18, 2022): 1004. http://dx.doi.org/10.3390/pr10051004.
Full textSquire, L. C. "The accuracy of flat plate, turbulent skin friction at supersonic speeds." Aeronautical Journal 104, no. 1036 (June 2000): 257–63. http://dx.doi.org/10.1017/s0001924000091570.
Full textRamarajan, V., and S. Soundranayagam. "Scale Effects in a Mixed Flow Pump: Part 1." Proceedings of the Institution of Mechanical Engineers, Part A: Power and Process Engineering 200, no. 3 (August 1986): 173–79. http://dx.doi.org/10.1243/pime_proc_1986_200_024_02.
Full textChe Sidik, Nor Azwadi, and Siti Aisyah Razali. "Stability Condition for Single-Relaxation Time Isothermal Lattice Boltzmann Formulation." Applied Mechanics and Materials 695 (November 2014): 667–70. http://dx.doi.org/10.4028/www.scientific.net/amm.695.667.
Full textDissertations / Theses on the topic "Reynolds Range"
Symes, Joseph Alexander. "Dry inclined galloping of smooth circular cables in the critical reynolds number range." Thesis, University of Bristol, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.546204.
Full textSutkowy, Mark Louis Jr. "Relationship between Rotor Wake Structures and Performance Characteristics over a Range of Low-Reynolds Number Conditions." The Ohio State University, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=osu1534768619864476.
Full textBouratsis, Polydefkis. "Scour at the Base of Hydraulic Structures: Monitoring Instrumentation and Physical Investigations Over a Wide Range of Reynolds Numbers." Diss., Virginia Tech, 2015. http://hdl.handle.net/10919/71880.
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Howlett, D. P. "Geochronological constraints on Yambah and Chewings-aged deformation at Mt Boothby in the south eastern Reynolds Range, Central Australia." Thesis, 2012. http://hdl.handle.net/2440/92257.
Full textZircon and monazite U–Pb isotope geochronology combined with structural mapping in the Mt Boothby region in the central Aileron Province in Central Australia has constrained the timing of two tectonically distinct phases of high-grade deformation and metamorphism. The first event (D1/M1) occurred at around 1790 Ma and was associated with the emplacement of a bimodal magmatic suite that underwent high-grade deformation prior to the emplacement of voluminous granite also at around 1790 Ma. The timing of D1/M1 coincides with the early stages of the Yambah Event, which is widely recognised in the southern Aileron Province, but has not previously been unequivocally shown to be associated with deformation . Subsequent pervasive reworking occurred over the interval 1600-1570 Ma, and was associated with long-lived granulite-grade metamorphism. The timing of this event coincides with the Chewings Orogeny which largely shaped the tectonic geology further west in the Reynolds and Anmatjira Ranges. During the Chewings Orogeny the c.1790 Ma D1 structures were transposed into a composite S1/S2 fabric. Map scale F2 folding is interpreted to have a shallow plunge suggesting that the S1 fabric may have originally been shallow dipping, raising the possibility that deformation was extensional in nature, and coeval with deposition of the nearby Reynolds Range Group which is constrained to the interval 1806-1785 Ma. Although inferred here to be Yambah aged, the timing constraints for D1 /M1 also overlap with the c. 1800 Ma Stafford Event which was associated with voluminous felsic magmatism, mafic magmatism and extreme geothermal gradient magmatism. This suggests that an extended period of extension, sedimentation, magmatism and deformation may have occurred at around 1800 Ma in the central Aileron Province.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2012
Then, M. "Constraints on the origin of early high-heat producing (U-Th enriched) granitic magmatism in central Australia." Thesis, 2016. http://hdl.handle.net/2440/121352.
Full textThe southern margin of central Australia is characterised by anomalous heat production, 3–5 times higher than global averages. Paleoproterozoic voluminous granitoid complexes in the region are important in the study of this anomalous heat flow. Ca.1800 Ma high-heat producing granites in Mt Boothby have A/NCK (molecular Al2O3/(CaO+Na2O+K2O)) ratios > 1, indicating a predominant origin from partial melting of metasedimentary rocks. The Boothby Orthogneiss is characterised by moderately negative Eu anomalies (Eu/Eu*: 0.03–0.43) and strong depletion in Ba, Rb, Nb and Sr. The enrichment of Ba and Rb relative to Sr and high K2O contents also support a metasedimentary source. The heat production values calculated for the Boothby Orthogneiss and the surrounding Lander formation show that the region is enriched in heat producing elements. The U-Pb zircon age data of inherited zircons in these granites are similar to the detrital zircons of the widespread outcropping; Lander formation. Nd values of -3.5 to 1.3 of the granites infer an evolved crustal source coupled with mixing of a newly mantle-derived component through lower crust assimilation. Zircon saturation temperatures calculated suggest that the Boothby intrusive complex was emplaced at 688–845oC, with a maximum temperature of 776oC, implying an arc environment with associated fluid-flux melting in the mantle wedge, ultimately controlled by subduction dynamics.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016
Bockmann, K. L. "From Greenschist to Granulite: a mineral equilibria approach to melting and melt loss." Thesis, 2015. http://hdl.handle.net/2440/117961.
Full textMelt loss during regional high-grade metamorphism has important consequences for interpreting the metamorphic evolution of the lower crust and for understanding processes leading to the chemical differentiation of the crust. However, melt loss typically modifies the protolith; making it difficult to reconstruct the conditions of prograde metamorphism and the extent to which melt loss modified the rock composition. The Reynolds Range in central Australia preserves a rare example where a single melt-prone stratigraphic unit can be traced from greenschist to granulite grade conditions. Using this as a natural laboratory, P–T mineral equilibria forward models have been calculated to explore melt loss and melt reintegration where both the protolith and the residuum compositions are preserved. Incremental melt loss modelling from the protolith composition along an isobaric heating path at 5 kbar shows that the residual granulite facies rock composition is consistent with around 18% melt loss from the protolith. Large-scale, one-step melt loss from a closed rock system that had built up 18% melt resulted in a similar residual composition to incremental melt loss. The fertility of the open (incremental) system and the closed system showed the closed system produced 5.4% more melt along a heating path from 700–800 °C. Determination of the concentrations of K–U–Th with increasing metamorphic grade shows that K and U concentrations decreased with increasing metamorphic grade. Conversely, Th concentrations increased, resulting in a slight overall increase in heat production from the protolith to the residuum, despite around 18% volume loss associated with melt extraction. An implication for this is that for melt prone rocks such as metapelites, melt loss during granulite facies metamorphism does not deplete the concentration of heat producing elements in the lower crust as is typically assumed.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2015
Weiss, S. "Constraints on the origin of the ca 1780 Ma high heat producing Napperby Gneiss, Aileron Province, Central Australia." Thesis, 2016. http://hdl.handle.net/2440/121355.
Full textThe Arunta Region of Central Australia contains Paleoproterozoic granites extremely enriched in high heat producing elements, in comparison to a global upper crustal average of 1.69 μWm-3. This study uses geochemistry, geochronology, and zircon saturation thermometry to investigate the source and tectonic environment of emplacement of the ca. 1780 Ma Napperby Gneiss. The Napperby Gneiss is peraluminous, suggesting a metasedimentary source. Samples have negative Eu anomalies ranging from 0.10 to 0.57, and show further evidence of fractionation in negative correlations of Ba and Sr with increasing SiO2. Initial εNd values are similar to surrounding exposed metasedimentary rocks and suggest a strong influence of an evolved crustal source but indicate a necessary juvenile component. Matches of inherited xenocrystic zircons from the gneiss with detrital patterns from the regional metasedimentary Lander Formation indicate that sediments similar to the Lander Formation are the source of the protolith granite. Zircon saturation temperatures suggest the granites were emplaced at 790°C – 872°C. Heat production is less than the slightly older ca 1800 ma suites of the Aileron province, and zircon saturation temperatures are higher. The Napperby was produced by dehydration melting rather than fluid flux melting, possibly in a back arc extensional environment with heat provided by upwelling mantle.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016
Books on the topic "Reynolds Range"
Pfenninger, Werner. Optimization of natural laminar flow airfoils for high section lift-to-drag ratios in the lower Reynolds number range. Washington, D. C: AIAA, 1989.
Find full textParsons, Chuck. Texas Ranger N.O. Reynolds, the intrepid. Honolulu, HI: Talei Publishers, 2005.
Find full textauthor, Brice Donaly E., ed. Texas Ranger N.O. Reynolds, the Intrepid. Denton, Texas: University of North Texas Press, 2014.
Find full textJ, Boyle R., and Lewis Research Center, eds. Aerodynamics of a transitioning turbine stator over a range of Reynolds numbers. [Cleveland, Ohio]: National Aeronautics and Space Administration, Lewis Research Center, 1998.
Find full textD, Moore Royce, United States. Army Aviation Research and Technology Activity., and United States. National Aeronautics and Space Administration., eds. Performance of two 10-lb/sec centrifugal compressors with different blade and shroud thicknesses operating over a range of Reynolds numbers. [Washington, DC]: National Aeronautics and Space Administration, 1987.
Find full textD, Moore Royce, United States. Army Aviation Research and Technology Activity., and United States. National Aeronautics and Space Administration., eds. Performance of two 10-lb/sec centrifugal compressors with different blade and shroud thicknesses operating over a range of Reynolds numbers. [Washington, DC]: National Aeronautics and Space Administration, 1987.
Find full textPerformance of two 10-lb/sec centrifugal compressors with different blade and shroud thicknesses operating over a range of Reynolds numbers. [Washington, DC]: National Aeronautics and Space Administration, 1987.
Find full textR, Whetstone James, and National Institute of Standards and Technology (U.S.), eds. Measurements of coefficients of discharge for concentric flange-tapped square-edged orifice meters in water over the Reynolds number range 600 to 2,700,000. Gaithersburg, MD: U.S. Dept. of Commerce, National Institute of Standards and Technology, 1989.
Find full textMeasurements of coefficients of discharge for concentric flange-tapped square-edged orifice meters in natural gas over the Reynolds number range 25,000 to 16,000,000. Gaithersburg, MD: U.S. Dept. of Commerce, National Institute of Standards and Technology, 1989.
Find full textBiewener, Andrew A., and Shelia N. Patek, eds. Movement in Water. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198743156.003.0005.
Full textBook chapters on the topic "Reynolds Range"
Danjkov, B. N., E. S. Kornienko, and V. V. Kudrjavtsev. "Supersonic Separation Zone Pressure Fluctuations for Wide Range of Reynolds Number." In Separated Flows and Jets, 237–43. Berlin, Heidelberg: Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-84447-8_34.
Full textČorbo, Tarik, Almin Halač, and Muris Torlak. "Computation of the Fluid Flow Around Octahedral Bodies for a Wide Reynolds Number Range." In Lecture Notes in Networks and Systems, 645–50. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-90055-7_51.
Full textKönig, M., and H. Eckelmann. "An Experimental Study of the Three-Dimensional Structure of the Wake of Circular Cylinders in the Laminar and Transitional Reynolds Number Range." In Bluff-Body Wakes, Dynamics and Instabilities, 341–44. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-662-00414-2_73.
Full textBragg, Don C., and Michael G. Shelton. "The Value of Old Forests: Lessons from the Reynolds Research Natural Area." In USDA Forest Service Experimental Forests and Ranges, 61–84. New York, NY: Springer New York, 2014. http://dx.doi.org/10.1007/978-1-4614-1818-4_3.
Full textIshida, Takahiro, Takahiro Tsukahara, and Yasuo Kawaguchi. "DNS of Rotating Turbulent Plane Poiseuille Flow in Low Reynolds- and Rotation-Number Ranges." In Progress in Turbulence V, 177–82. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-01860-7_28.
Full textSpeziale, Charles G. "Modeling Of Turbulent Transport Equations." In Simulation and Modeling of Turbulent Flows. Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195106435.003.0009.
Full textB. Dehankar, Prashant. "Assessment of Augmentation Techniques to Intensify Heat Transmission Power." In Heat Exchangers. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.101670.
Full textDeHart, Jason D. "Situating Cultural Awareness Through Comics." In Advances in Early Childhood and K-12 Education, 1–14. IGI Global, 2022. http://dx.doi.org/10.4018/978-1-6684-4215-9.ch001.
Full textChen, Lin. "Principles, Experiments, and Numerical Studies of Supercritical Fluid Natural Circulation System." In Advanced Applications of Supercritical Fluids in Energy Systems, 136–87. IGI Global, 2017. http://dx.doi.org/10.4018/978-1-5225-2047-4.ch005.
Full textChen, Lin. "Principles, Experiments, and Numerical Studies of Supercritical Fluid Natural Circulation System." In Handbook of Research on Advancements in Supercritical Fluids Applications for Sustainable Energy Systems, 219–69. IGI Global, 2021. http://dx.doi.org/10.4018/978-1-7998-5796-9.ch007.
Full textConference papers on the topic "Reynolds Range"
Albrecht, Mitchell B., David A. Olson, Ahmed M. Naguib, and Manoochehr Koochesfahani. "Reynolds Number and Freestream Shear Effects on a NACA 0012 Airfoil in the Reynolds Number Range 10,000-30,000." In AIAA SCITECH 2022 Forum. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2022. http://dx.doi.org/10.2514/6.2022-1055.
Full textSmith, Adam E., Stanislav Gordeyev, Theresa Saxton-Fox, and Beverley J. McKeon. "Subsonic Boundary-Layer Wavefront Spectra for a Range of Reynolds Numbers." In 45th AIAA Plasmadynamics and Lasers Conference. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2014. http://dx.doi.org/10.2514/6.2014-2491.
Full textKogiso, Nozomu, Tatsurou Tsushima, and Yoshisada Murotsu. "Wing planform optimization of human powered aircraft in low Reynolds number range." In 8th Symposium on Multidisciplinary Analysis and Optimization. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2000. http://dx.doi.org/10.2514/6.2000-4739.
Full textBoyle, R. J., B. L. Lucci, V. G. Verhoff, W. P. Camperchioli, and H. La. "Aerodynamics of a Transitioning Turbine Stator Over a Range of Reynolds Numbers." In ASME 1998 International Gas Turbine and Aeroengine Congress and Exhibition. American Society of Mechanical Engineers, 1998. http://dx.doi.org/10.1115/98-gt-285.
Full textBRASSEUR, J. "Evolution characteristics of vortex rings over a wide range of Reynolds numbers." In 4th Joint Fluid Mechanics, Plasma Dynamics and Lasers Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1986. http://dx.doi.org/10.2514/6.1986-1097.
Full textCatrakis, Haris, Roberto Aguirre, and Jennifer Nathman. "Large-Reynolds-Number Turbulent Fluid Interfaces and the Upper Range of Scales." In 42nd AIAA Aerospace Sciences Meeting and Exhibit. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2004. http://dx.doi.org/10.2514/6.2004-1113.
Full textMorse, Daniel R., and James A. Liburdy. "Vortex Detection and Characterization in Low Reynolds Number Separation." In ASME 2007 International Mechanical Engineering Congress and Exposition. ASMEDC, 2007. http://dx.doi.org/10.1115/imece2007-43011.
Full textChauhan, Kapil, Ivan Marusic, and Nick Hutchins. "Organised motions in turbulent boundary layers over a wide range of Reynolds number." In 6th AIAA Theoretical Fluid Mechanics Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2011. http://dx.doi.org/10.2514/6.2011-3932.
Full textMironov, S. G., V. M. Aniskin, and A. A. Maslov. "Flowing of supersonic underexpanded micro-jets in the range of moderate Reynolds numbers." In PROCEEDINGS OF THE XXV CONFERENCE ON HIGH-ENERGY PROCESSES IN CONDENSED MATTER (HEPCM 2017): Dedicated to the 60th anniversary of the Khristianovich Institute of Theoretical and Applied Mechanics SB RAS. Author(s), 2017. http://dx.doi.org/10.1063/1.5007610.
Full textOgata, Satoshi, Keizo Watanabe, and Yoshihisa Osano. "Drag of a Circular Cylinder in Surfactant Solutions at Intermediate Reynolds Number Range." In ASME/JSME 2003 4th Joint Fluids Summer Engineering Conference. ASMEDC, 2003. http://dx.doi.org/10.1115/fedsm2003-45768.
Full textReports on the topic "Reynolds Range"
Whetstone, James R. Measurements of coefficients of discharge for concentric flange-tapped square-edged orifice meters in water over the Reynolds number range 600 to 2,700,000. Gaithersburg, MD: National Bureau of Standards, 1989. http://dx.doi.org/10.6028/nist.tn.1264.
Full textWhetstone, James R. Measurements of coefficients of discharge for concentric flange-tapped square-edged orifice meters in natural gas over the Reynolds number range 25,000 to 16,000,000. Gaithersburg, MD: National Bureau of Standards, 1989. http://dx.doi.org/10.6028/nist.tn.1270.
Full text