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Статті в журналах з теми "Boundary heat flux"
Huang, Weichao, Jiahao Li, and Ding Liu. "Research on Unsteady Inverse Heat Conduction Based on Dynamic Matrix Control." Energies 16, no. 11 (May 30, 2023): 4420. http://dx.doi.org/10.3390/en16114420.
Повний текст джерелаMiao, Wenbo, Xiaoli Cheng, Bangcheng Ai, and Yonghui Dong. "Surface Slip Effect on Thermal Environment of Hypersonic Non-Equilibrium Flows." International Journal of Computational Methods 12, no. 04 (August 2015): 1540008. http://dx.doi.org/10.1142/s0219876215400083.
Повний текст джерелаWang, Fu Qiang. "Ray-Thermal Sequential Coupled Heat Transfer ANALYSIS of Porous Media Receiver for Solar Dish Collector." Applied Mechanics and Materials 442 (October 2013): 169–75. http://dx.doi.org/10.4028/www.scientific.net/amm.442.169.
Повний текст джерелаWen, Jun, and M. M. Khonsari. "Analytical Formulation for the Temperature Profile by Duhamel’s Theorem in Bodies Subjected to an Oscillatory Heat Source." Journal of Heat Transfer 129, no. 2 (July 5, 2005): 236–40. http://dx.doi.org/10.1115/1.2424236.
Повний текст джерелаAlghamdi, A. "Inverse Estimation of Boundary Heat Flux for Heat Conduction Model." Journal of King Abdulaziz University-Engineering Sciences 21, no. 1 (2010): 73–95. http://dx.doi.org/10.4197/eng.21-1.5.
Повний текст джерелаTaylor, Robert P., Philip H. Love, Hugh W. Coleman, and M. H. Hosni. "Step heat flux effects on turbulent boundary-layer heat transfer." Journal of Thermophysics and Heat Transfer 4, no. 1 (January 1990): 121–23. http://dx.doi.org/10.2514/3.29175.
Повний текст джерелаDewar, W. K., and R. X. Huang. "Fluid flow in loops driven by freshwater and heat fluxes." Journal of Fluid Mechanics 297 (August 25, 1995): 153–91. http://dx.doi.org/10.1017/s0022112095003041.
Повний текст джерелаVoglar, Jure. "Physical Model of a Single Bubble Growth during Nucleate Pool Boiling." Fluids 7, no. 3 (February 27, 2022): 90. http://dx.doi.org/10.3390/fluids7030090.
Повний текст джерелаJi, Xuan, Nora Bailey, Daniel Fabrycky, Edwin S. Kite, Jonathan H. Jiang, and Dorian S. Abbot. "Inner Habitable Zone Boundary for Eccentric Exoplanets." Astrophysical Journal Letters 943, no. 1 (January 1, 2023): L1. http://dx.doi.org/10.3847/2041-8213/acaf62.
Повний текст джерелаJuliano, Thomas J., Jonathan Poggie, Kevin M. Porter, Roger L. Kimmel, Joseph S. Jewell, and David W. Adamczak. "HIFIRE-5b Heat Flux and Boundary-Layer Transition." Journal of Spacecraft and Rockets 55, no. 6 (November 2018): 1315–28. http://dx.doi.org/10.2514/1.a34147.
Повний текст джерелаДисертації з теми "Boundary heat flux"
Vega, Thomas. "Quantification of the Fire Thermal Boundary Condition." Thesis, Virginia Tech, 2012. http://hdl.handle.net/10919/78052.
Повний текст джерелаMaster of Science
Kharche, Sanjay. "Stefan problems with two-dimensional, linearised perturbations in their boundary geometry or boundary conditions." Thesis, University of Hull, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.327179.
Повний текст джерелаSchmid, Hans Peter Emil. "Spatial scales of sensible heat flux variability : representativeness of flux measurements and surface layer structure over suburban terrain." Thesis, University of British Columbia, 1988. http://hdl.handle.net/2429/29385.
Повний текст джерелаArts, Faculty of
Geography, Department of
Graduate
Magee, Michael P. "Thermal boundary resistance in a high temperature thin-film superconductor under varying heat flux." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1996. http://handle.dtic.mil/100.2/ADA326312.
Повний текст джерела"December 1996." Thesis advisor(s): Matthew Kelleher, Pat E. Phelan. Includes bibliographical references (p. 73-75). Also available online.
Sahlée, Erik. "Fluxes of Sensible and Latent Heat and Carbon Dioxide in the Marine Atmospheric Boundary Layer." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-8184.
Повний текст джерелаOceans cover about 70% of the earth’s surface. They are the largest source of the atmospheric water vapour and act as enormous heat reservoirs. Thus in order to predict the future weather and climate it is of great importance to understand the processes governing the exchange of water vapour and heat between the ocean and atmosphere. This exchange is to a large extent mediated by turbulent eddies. Current numerical climate and weather forecast models are unable to resolve the turbulence, which means that the turbulent exchange needs to be simplified by using parameterizations.
Tower based measurements at the Östergarnsholm Island in the Baltic Sea have been used to study the air-sea turbulent exchange of latent and sensible heat and the heat flux parameterizations. Although the measurements are made at an island, data obtained at this site is shown to represent open ocean conditions during most situations for winds coming from the east-south sector. It is found that during conditions with small air-sea temperature differences and wind speeds above 10 m s-1, the structure of the turbulence is re-organized. Drier and colder air from aloft is transported to the surface by detached eddies, which considerably enhance the turbulent heat fluxes. The fluxes where observed to be much larger than predicted by current state-of-the-art parameterizations. The turbulence regime during these conditions is termed the Unstable Very Close to Neutral Regime, the UVCN-regime.
The global increase of the latent and sensible heat fluxes due to the UVCN-regime is calculated to 2.4 W m-2 and 0.8 W m-2 respectively. This is comparable to the current increase of the radiative forcing due to anthropogenic emissions of greenhouse gases, reported in Intergovernmental Panel on Climate Change fourth assessment report (IPCC AR4). Thus the UVCN-effect could have a significant influence when predicting the future weather and climate.
Lindgren, Kristina. "The Behaviour of the Latent Heat Exchange Coefficient in the Stable Marine Boundary Layer." Thesis, Uppsala University, Department of Earth Sciences, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-9140.
Повний текст джерелаKnowledge of the turbulent fluxes at the sea surface is important for understanding the interaction between atmosphere and ocean. With better knowledge, improvements in the estimation of the heat exchange coefficients can be made and hence models are able to predict the weather and future climate with higher accuracy.
The exchange coefficients of latent and sensible heat during stable stratification vary in the literature. Therefore it is necessary to investigate the processes influencing the air-sea exchange of water vapour and heat in order to estimate these values. With measurements from a tower and a directional waverider buoy at the site Östergarnsholm in the Baltic Sea, data used in this study have been sampled from the years 2005-2007. This site represents open-ocean conditions during most situations when the wind comes from the south-east sector. The neutral exchange coefficients, CEN and CHN, have been calculated along with the non-dimensional profile functions for temperature and wind to study the dependence of stability and other parameters of relevance.
It was found that CEN increased slightly with wind speed and reached a mean value of approximately 1.45×10-3. The highest values of CEN were observed during near neutral conditions and low wave ages. CHN attained a mean value of approximately 0.77×10-3 and did not show any relation to wind speed or to wave age. No significant dependence with wind or wave direction could be shown for either CEN or CHN in the sector 80-220°. The stability correction, performed to reduce the dependence on stratification for CEN and CHN, was well performed for stabilities higher than 0.15. The stability is represented by a relationship between the height and the Obukhov-length (z/L).
Validity of the non-dimensional profile functions for temperature and wind showed that, for smaller stabilities, these functions gave higher values than the corresponding functions recommended by Högström (1996). The profile funtions for temperature was shown to have a larger scatter while the profile functions for wind was less scattered and deviated more from the functions given by Högström
Kunskap om turbulenta flöden i det marina gränsskiktet är viktigt för att förstå växelverkan mellan atmosfär och hav. Med bättre kunskap kan förbättringar i bestämningen av utbyteskoefficienterna för latent och sensibelt värme erhållas. Det medför att modeller kan prognostisera väder och framtida klimat med högre noggrannhet.
Utbyteskoefficienterna för latent och sensibelt värme har för stabil skiktning olika värden i litteraturen. Detta gör det nödvändigt att undersöka de processer som påverkar utbytet av vattenånga och värme mellan luft och hav för att kunna bestämma dessa värden. Data som har använts i den här studien insamlades mellan år 2005 och 2007 från en boj och ett torn vid mätplatsen Östergarnsholm i Baltiska havet. För det flesta situationer, när vinden blåser från syd-ost, representerar mätplatsen ett förhållande likvärdigt det över öppet hav. De neutrala utbyteskoefficienterna, CEN och CHN, och de dimensionslösa profilfunktionera för temperatur och vind, och , har beräknats för att studera beroendet av stabilitet samt andra relevanta parametrar.
Beräkningarna visade att CEN ökade något med vindhastighet och hamnade på ett medelvärde av ungefär 1.45×10-3. De högsta värdena på CEN observerades vid nära neutrala förhållanden och låga vågåldrar. CHN uppmättes till att ha ett medelvärde på ungefär 0.77×10-3 och uppvisade inget beroende med vindhastighet eller vågålder. Inget märkbart beroende med vind- eller vågriktning kunde visas för CEN eller CHN i sektorn 80-220°. Stabilitetskorrektionen, utförd för att reducera beroendet av atmosfärens skiktning för CEN och CHN, var bra för stabiliteter högre än 0.15. Stabiliteten representeras av förhållandet mellan höjden och Obukhov-längden (z/L).
Utvärdering av de dimensionslösa funktionerna för temperatur och vind visade att dessa funktioner, för små stabiliteter, gav högre värden än motsvarande funktioner som rekommenderas av Högström (1996). Värdena på profilfunktionerna för temperatur hade större spridning än värdena på profilfunktionerna för vind och avvek mer från funktionerna givna av Högström.
Moosbrugger, John C. "Numerical computation of metal/mold boundary heat flux in sand castings using a finite element enthalpy model." Thesis, Georgia Institute of Technology, 1985. http://hdl.handle.net/1853/16365.
Повний текст джерелаBrunner, Daniel Frederic. "Development of probes for assessment of ion heat transport and sheath heat flux in the boundary of the Alcator C-Mod Tokamak." Thesis, Massachusetts Institute of Technology, 2013. http://hdl.handle.net/1721.1/86420.
Повний текст джерелаThis electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections.
Cataloged from student-submitted PDF version of thesis. Pages [228-229] blank.
Includes bibliographical references.
Progress towards a viable fusion reactor will require comprehensive understanding of boundary plasma physics. Knowledge in this area has been growing, yet there are critical gaps. Measurements of the sheath heat flux transmission coefficient-a fundamental physical quantity whose theoretical value is ~ 7-have varied from 2 to 20. Values below 5 are physically impossible and have challenged the understanding of this very basic theory. In addition, measurements of ion temperature are sparse and ion energy transport is poorly understood. To this end a set of new diagnostics, including a surface thermocouple, ion sensitive probe, and retarding field analyzer, have been developed that can tolerate the extreme heat fluxes in the Alcator C-Mod boundary plasma. These probes are used to asses issues of heat flux and ion energy transport. Systematic studies with these new tools reveal the following: A comparison of surface thermocouples and Langmuir probes confirms standard sheath heat flux theory in a tokamak for the first time. The measurement of unphysically low sheath heat flux transmission coefficients and an anomalous increase in measured divertor pressure by Langmuir probes, which is also unphysical, are found the be linked. Plasma-neutral simulations indicate that these artifacts are due to the Langmuir probe bias modifying the local plasma. Important space charge limits to measurements with ion sensitive probes are found experimentally and explored in depth with a 1D kinetic simulation. These results clarify the plasma conditions under which an ion sensitive probe may be used to measure ion temperature and/or plasma potential. The retarding field analyzer is demonstrated to be a viable ion temperature diagnostic up to the last closed flux surface in C-Mod. A ₁D fluid simulations is built to interpret edge ion heat transport. At high collisionality-where the fluid approximations are valid: the simulation reproduces the measured edge ion-to-electron temperature ratio (~ 2). However, at low collisionality-where fluid approximation is not valid-the simulation is not able to reproduce the experimental temperature ratio (~ 4). The addition of kinetic heat flux limiters can bring the simulated ratio into agreement with measurements. The value of heat flux limiter is found to be consistent with that expected from kinetic theory.
by Daniel Frederic Brunner.
Ph. D.
Nilsson, Erik. "Flux Attenuation due to Sensor Displacement over Sea." Thesis, Uppsala University, Department of Earth Sciences, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-8024.
Повний текст джерелаIn this study the flux attenuation due to sensor displacement has been investigated over sea using an extensive set of data from the "Ocean Horizontal Array Turbulence Study". All previous investigations of the flux attenuation have been performed over land.
A function developed for correcting fluxes in the homogenous surface layer was compared to measured flux attenuation. This investigation revealed the possibility to find new functions describing the flux attenuation when measurements are carried out over sea. From the measured flux attenuation studied here a change in the form of correction functions was required to improve the estimated flux loss. The most significant difference found in this report compared to the previous landbased study Horst (2006) is for stable conditions, where significantly less flux loss is found over sea. Two new functions describing the attenuation due to sensor displacement over sea have been constructed.
One of these expressions has a discontinuity at z/L = 0. This is supported by measured flux attenuation. A reasonable interpretation is; however, that this discontinuity is caused by two separate turbulence regimes near neutrality on the stable and unstable side respectively. The discontinuity is thus not believed to be an effect merely of stability. A second correction function which is continuous over all stabilities has therefore also been constructed. These two functions and the correction function from Horst (2006) have been compared to measured flux loss. Based on this comparison the continuous correction function is recommended for correcting scalar fluxes measured over sea. It should be noted, however, that this expression only describes the mean attenuation and has been constructed from measurements at 5 and 5.5 m above mean sea level.
The theoretical basis used in the development of the function for flux attenuation over land allows for a direct link between a spectral shape and the attenuation expression. This link has been preserved for the new expressions presented in this report. The spectral shape corresponding to the continuous correction function has been compared to measured mean cospectra and also to the cospectra from Horst (2006) corresponding to crosswind displacements.
At a height of 10 m and a sensor displacement of 0.2 m the mean flux attenuation is about 1.3-4% in the stability interval −1 < z/L < 1.5 when using the new correction functions presented in this report.
Lammert, Andrea, and Armin Raabe. "Berechnung sensibler Wärmeströme mit der Surface Renewal Analysis und der Eddy - Korrelations - Methode." Universitätsbibliothek Leipzig, 2016. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-215495.
Повний текст джерелаThe Surface Renewal Analysis was used to estimate the sensible heat flux density in the ground near area of the boundary layer. The results were compared with eddy correlation method. For it both methods were used to analyse temperature- and vertical velocity-data, which were simulated by the application of structure functions. Time series of high frequency temperature- and vertical velocity-data over two different canopies (meadow and dune) were measured to examine the results. The data were analysed with surface renewal analysis and eddy correlation
Книги з теми "Boundary heat flux"
Zaman, K. B. M. O., Reshotko Eli, and United States. National Aeronautics and Space Administration., eds. Turbulent heat flux measurements in a transitional boundary layer. [Washington, DC]: National Aeronautics and Space Administration, 1992.
Знайти повний текст джерелаZaman, K. B. M. Q., Reshotko E, and United States. National Aeronautics and Space Administration., eds. Turbulent heat flux measurements in a transitional boundary layer. [Washington, DC]: National Aeronautics and Space Administration, 1992.
Знайти повний текст джерелаBradley, E. F. A guide to making climate quality meteorological and flux measurements at sea. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Office of Oceanic and Atmospheric Research, Earth System Research Laboratory, Physical Sciences Division, 2007.
Знайти повний текст джерелаBradley, E. F. A guide to making climate quality meteorological and flux measurements at sea. Boulder, CO: National Oceanic and Atmospheric Administration, Office of Oceanic and Atmospheric Research, Earth System Research Laboratory, Physical Sciences Division, 2006.
Знайти повний текст джерелаMichels, Berenice I. Fluxes of heat and water vapour in a convective mixed layer during EFEDA. Köln: Deutsche Forschungsanstalt für Luft- und Raumfahrt, 1992.
Знайти повний текст джерелаJankovsky, Robert S. High-area-ratio rocket nozzle at high combustion chamber pressure--experimental and analytical validation. [Cleveland, Ohio]: National Aeronautics and Space Administration, Glenn Research Center, 1999.
Знайти повний текст джерелаD, Smith Timothy, Pavli Albert J, and NASA Glenn Research Center, eds. High-area-ratio rocket nozzle at high combustion chamber pressure--experimental and analytical validation. [Cleveland, Ohio]: National Aeronautics and Space Administration, Glenn Research Center, 1999.
Знайти повний текст джерелаD, Smith Timothy, Pavli Albert J, and NASA Glenn Research Center, eds. High-area-ratio rocket nozzle at high combustion chamber pressure--experimental and analytical validation. [Cleveland, Ohio]: National Aeronautics and Space Administration, Glenn Research Center, 1999.
Знайти повний текст джерелаD, Smith Timothy, Pavli Albert J, and NASA Glenn Research Center, eds. High-area-ratio rocket nozzle at high combustion chamber pressure--experimental and analytical validation. [Cleveland, Ohio]: National Aeronautics and Space Administration, Glenn Research Center, 1999.
Знайти повний текст джерелаFoken, Th. Turbulenter Energieaustausch zwischen Atmosphäre und Unterlage: Methoden, messtechnische Realisierung sowie ihre Grenzen und Anwendungsmöglichkeiten. Offenbach am Main: Selbstverlag des Deutschen Wetterdienstes, 1990.
Знайти повний текст джерелаЧастини книг з теми "Boundary heat flux"
Burton, Ralph A. "Coupling of Waviness and Boundary Heat Flux in Reynolds Flow." In Heat, Bearings, and Lubrication, 90–97. New York, NY: Springer New York, 2000. http://dx.doi.org/10.1007/978-1-4612-1248-5_12.
Повний текст джерелаDesjardins, R. L., J. I. Macpherson, P. H. Schuepp, and F. Karanja. "An Evaluation of Aircraft Flux Measurements of CO2, Water Vapor and Sensible Heat." In Boundary Layer Studies and Applications, 55–69. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0975-5_5.
Повний текст джерелаAmar, M., D. Andreucci, R. Gianni, and C. Timofte. "Homogenization of a Heat Conduction Problem with a Total Flux Boundary Condition." In Lecture Notes in Mechanical Engineering, 1475–87. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-41057-5_119.
Повний текст джерелаHasebe, Norio. "Thermal Stress for Mixed Heat Conduction Boundary Around an Arbitrarily Shaped Hole Under Uniform Heat Flux." In Encyclopedia of Thermal Stresses, 5204–8. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-2739-7_117.
Повний текст джерелаHelmig, Thorsten, Hui Liu, Simon Winter, Thomas Bergs, and Reinhold Kneer. "Development of a Tool Temperature Simulation During Side Milling." In Lecture Notes in Production Engineering, 308–17. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-34486-2_22.
Повний текст джерелаVaka, Ananda S., Pedduri Jayakrishna, Saurav Chakraborty, Suvankar Ganguly, and Prabal Talukdar. "Application of Inverse Heat Transfer Technique in Thin Slab Continuous Casting for Estimating the Interfacial Boundary Heat Flux." In Lecture Notes in Mechanical Engineering, 385–98. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-7214-0_32.
Повний текст джерелаFerdows, M., and Sakawat Hossain. "Local Non-similar Solution of Induced Magnetic Boundary Layer Flow with Radiative Heat Flux." In Flow and Transport in Subsurface Environment, 343–65. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-8773-8_12.
Повний текст джерелаFuselier, S. A., W. C. Feldman, S. J. Bame, E. J. Smith, and F. L. Scarf. "Heat Flux Observations and the Location of The Transition Region Boundary of Giacobini-Zinner." In Special Publications, 1. Washington, D.C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/sp027p0165.
Повний текст джерелаPrajapati, Ravi, Viral Thakkar, Sanil Shah, and Ajit Kumar Parwani. "Estimation of Transient Boundary Heat Flux Using Modified JAYA Algorithm in Laminar Duct Flow." In Recent Advances in Mechanical Infrastructure, 331–42. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-4176-0_29.
Повний текст джерелаSathavara, Parth, Ajit Kumar Parwani, Maulik Panchal, and Paritosh Chaudhuri. "Estimation of Boundary Heat Flux with Conjugate Gradient Method by Experimental Transient Temperature Data." In Recent Advances in Mechanical Infrastructure, 343–52. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-4176-0_30.
Повний текст джерелаТези доповідей конференцій з теми "Boundary heat flux"
Juliano, Thomas J., Jonathan Poggie, Kevin Porter, Roger L. Kimmel, Joseph S. Jewell, and David Adamczak. "HIFiRE-5b Heat Flux and Boundary-Layer Transition." In 47th AIAA Fluid Dynamics Conference. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2017. http://dx.doi.org/10.2514/6.2017-3134.
Повний текст джерелаSaidi, Arash, and Jungho Kim. "Heat Flux Sensor With Minimal Impact on Boundary Conditions." In ASME 2003 Heat Transfer Summer Conference. ASMEDC, 2003. http://dx.doi.org/10.1115/ht2003-47567.
Повний текст джерелаWalsh, P. A., E. J. Walsh, and Y. S. Muzychka. "Laminar Slug Flow: Heat Transfer Characteristics With Constant Heat Flux Boundary." In ASME 2009 Heat Transfer Summer Conference collocated with the InterPACK09 and 3rd Energy Sustainability Conferences. ASMEDC, 2009. http://dx.doi.org/10.1115/ht2009-88428.
Повний текст джерелаWu, Zhijian, Jing Feng, Xueyan Zhang, and Aixia Zhou. "Study on Reconstruction of Heat Flux in Moving Boundary." In 2012 National Conference on Information Technology and Computer Science. Paris, France: Atlantis Press, 2012. http://dx.doi.org/10.2991/citcs.2012.203.
Повний текст джерелаMolavi, Hosein, Ali Hakkaki-Fard, Alireza Pourshaghaghy, Mehdi Molavi, and Ramin K. Rahmani. "Heat Flux Estimation in a Nonlinear Inverse Heat Conduction Problem With Moving Boundary." In ASME 2009 Heat Transfer Summer Conference collocated with the InterPACK09 and 3rd Energy Sustainability Conferences. ASMEDC, 2009. http://dx.doi.org/10.1115/ht2009-88501.
Повний текст джерелаPark, Chul. "Radiative to Convective Heat Flux Conversion by Boundary Layer Absorption." In 47th AIAA Aerospace Sciences Meeting including The New Horizons Forum and Aerospace Exposition. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2009. http://dx.doi.org/10.2514/6.2009-1583.
Повний текст джерелаBreidenthal, R. E. "Wall Heat Flux Under Persistent Vortices." In ASME 2002 Joint U.S.-European Fluids Engineering Division Conference. ASMEDC, 2002. http://dx.doi.org/10.1115/fedsm2002-31244.
Повний текст джерелаWang, Q. W., Q. W. He, X. N. Suo, and Y. N. Wu. "GASEOUS FLOW AND HEAT TRANSFER IN MICRO-CHANNEL WITH HEAT FLUX SPECIFIED BOUNDARY CONDITION." In Annals of the Assembly for International Heat Transfer Conference 13. Begell House Inc., 2006. http://dx.doi.org/10.1615/ihtc13.p14.130.
Повний текст джерелаLee, Man, Luthur Siu Lun Cheung, Yi-Kuen Lee, and Yitshak Zohar. "Two-Phase Flow in Microchannel Heat Sink with Nearly Uniform Heat Flux Boundary Condition." In 2006 1st IEEE International Conference on Nano/Micro Engineered and Molecular Systems. IEEE, 2006. http://dx.doi.org/10.1109/nems.2006.334888.
Повний текст джерелаLu, Wen-Qiang, and Qing-Mei Fan. "Non-Fourier Heat Conduction Phenomena Applied Different Temperature and Heat Flux Pulses on Boundary." In ASME 2008 First International Conference on Micro/Nanoscale Heat Transfer. ASMEDC, 2008. http://dx.doi.org/10.1115/mnht2008-52287.
Повний текст джерелаЗвіти організацій з теми "Boundary heat flux"
Mahrt, Larry, and Jielun Sun. A New Heat Flux Formulation Based on Effective Surface Temperatures, With Extension to the Nocturnal Boundary Layer. Fort Belvoir, VA: Defense Technical Information Center, August 1999. http://dx.doi.org/10.21236/ada369931.
Повний текст джерела