Simulation of conductive‐convective heat transfer in a natural basin

The state of water flow has been modelled numerically by a three‐dimensional method of a complex investigation of heat and mass transfer. This allows examining interaction of some transfer processes in a natural cooling basin (the Drûkšiai lake): variable density of water, heat conduction in water‐...

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Main Authors: Petras Vaitiekūnas, Vladislovas Katinas, Antanas Markevičius
Format: Article
Language:English
Published: Vilnius Gediminas Technical University 2004-06-01
Series:Journal of Environmental Engineering and Landscape Management
Subjects:
Online Access:https://journals.vgtu.lt/index.php/JEELM/article/view/8077
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spelling doaj-d25f4c6e55ca4261a1727fb73bc5a6612021-07-02T09:16:37ZengVilnius Gediminas Technical UniversityJournal of Environmental Engineering and Landscape Management1648-68971822-41992004-06-0112210.3846/16486897.2004.9636818Simulation of conductive‐convective heat transfer in a natural basinPetras Vaitiekūnas0Vladislovas Katinas1Antanas Markevičius2Dept of Environmental Protection , Vilnius Gediminas Technical University , Saulëtekio al. 11, Vilnius‐40, LT‐10223, LithuaniaLithuanian Energy Institute, Renewable Energy Laboratory, Breslojaus g. 3, LT-44403 Kaunas-35, LithuaniaLithuanian Energy Institute, Renewable Energy Laboratory, Breslojaus g. 3, LT-44403 Kaunas-35, Lithuania The state of water flow has been modelled numerically by a three‐dimensional method of a complex investigation of heat and mass transfer. This allows examining interaction of some transfer processes in a natural cooling basin (the Drûkšiai lake): variable density of water, heat conduction in water‐air interface, direct and diffuse solar radiation. Combined effect of these natural actions determines the heat amount that the basin is able to dissipate to the surrounding atmospheric media in thermal equilibrium (no change in the mean water temperature). Mathematical model is simplified ignoring transient derivatives in transfer equations, and time as a variable is included in relaxation coefficients for outer iterations. Full time of calculations using this simulation mechanism for this variable is about 6 h. Basing on water stream velocity and mean temperature profiles measured in the cooling pond as well as on their time variations, suggestions are made that the mixing rate in water is caused by natural and forced convection. Comparison of experimental and numerical results showed a qualitative agreement. For a better quantitative approximation, it is necessary to have more boundary conditions variable with time and to solve unsteady set equations for transfer processes. Šilumos laidumo-konvekcinių mainų natūraliame baseine modeliavimas Santrauka Matematinis vandens srauto modelis sudarytas skaitiniam trimačių pernašos procesų vienfaziame fluide modeliavimui. Nagrinėjama įvairių veiksnių bei jų sąveikos įtaka pernašos procesams, masės ir šilumos mainams natūriniame baseine‐aušintuve: vandens tankio priklausomybė nuo temperatūros, konvekcija‐laidumas vandens masėje, šilumos laidumo mainai su oro aplinka, tiesioginė ir sklaidžioji saulės spinduliuotė. Matematinis modelis supaprastintas atmetant nenuostovumo narius pernašos lygtyse, laiko kintamąjį įvedant kaip išorinių iteracijų relaksacijos koeficientus. Skaičiavimo trukmė ‐ apie 6 h. Palyginus eksperimentinius ir teorinius rezultatus paaiškėjo kokybinis jų sutapimas. Kad kiekybiniai rezultatai sutaptų tiksliau, reikėtų turėti daugiau įvairių veiksnių ribinių sąlygų, kintančių laike, bei spręsti nenuostoviąsias pernašos lygtis. Reikšminiai žodžiai: hidrodinamika, skaičiuojamoji fluidų dinamika, skaitinis modeliavimas, trimačiai procesai, vienfaziai srautai, baseinas‐aušintuvas, šilumos mainai First Published Online: 14 Oct 2010 https://journals.vgtu.lt/index.php/JEELM/article/view/8077Computational Fluid Dynamics (CFD)numerical simulationthree‐dimensional processesone‐phase flowshydrodynamicslake as a cooler
collection DOAJ
language English
format Article
sources DOAJ
author Petras Vaitiekūnas
Vladislovas Katinas
Antanas Markevičius
spellingShingle Petras Vaitiekūnas
Vladislovas Katinas
Antanas Markevičius
Simulation of conductive‐convective heat transfer in a natural basin
Journal of Environmental Engineering and Landscape Management
Computational Fluid Dynamics (CFD)
numerical simulation
three‐dimensional processes
one‐phase flows
hydrodynamics
lake as a cooler
author_facet Petras Vaitiekūnas
Vladislovas Katinas
Antanas Markevičius
author_sort Petras Vaitiekūnas
title Simulation of conductive‐convective heat transfer in a natural basin
title_short Simulation of conductive‐convective heat transfer in a natural basin
title_full Simulation of conductive‐convective heat transfer in a natural basin
title_fullStr Simulation of conductive‐convective heat transfer in a natural basin
title_full_unstemmed Simulation of conductive‐convective heat transfer in a natural basin
title_sort simulation of conductive‐convective heat transfer in a natural basin
publisher Vilnius Gediminas Technical University
series Journal of Environmental Engineering and Landscape Management
issn 1648-6897
1822-4199
publishDate 2004-06-01
description The state of water flow has been modelled numerically by a three‐dimensional method of a complex investigation of heat and mass transfer. This allows examining interaction of some transfer processes in a natural cooling basin (the Drûkšiai lake): variable density of water, heat conduction in water‐air interface, direct and diffuse solar radiation. Combined effect of these natural actions determines the heat amount that the basin is able to dissipate to the surrounding atmospheric media in thermal equilibrium (no change in the mean water temperature). Mathematical model is simplified ignoring transient derivatives in transfer equations, and time as a variable is included in relaxation coefficients for outer iterations. Full time of calculations using this simulation mechanism for this variable is about 6 h. Basing on water stream velocity and mean temperature profiles measured in the cooling pond as well as on their time variations, suggestions are made that the mixing rate in water is caused by natural and forced convection. Comparison of experimental and numerical results showed a qualitative agreement. For a better quantitative approximation, it is necessary to have more boundary conditions variable with time and to solve unsteady set equations for transfer processes. Šilumos laidumo-konvekcinių mainų natūraliame baseine modeliavimas Santrauka Matematinis vandens srauto modelis sudarytas skaitiniam trimačių pernašos procesų vienfaziame fluide modeliavimui. Nagrinėjama įvairių veiksnių bei jų sąveikos įtaka pernašos procesams, masės ir šilumos mainams natūriniame baseine‐aušintuve: vandens tankio priklausomybė nuo temperatūros, konvekcija‐laidumas vandens masėje, šilumos laidumo mainai su oro aplinka, tiesioginė ir sklaidžioji saulės spinduliuotė. Matematinis modelis supaprastintas atmetant nenuostovumo narius pernašos lygtyse, laiko kintamąjį įvedant kaip išorinių iteracijų relaksacijos koeficientus. Skaičiavimo trukmė ‐ apie 6 h. Palyginus eksperimentinius ir teorinius rezultatus paaiškėjo kokybinis jų sutapimas. Kad kiekybiniai rezultatai sutaptų tiksliau, reikėtų turėti daugiau įvairių veiksnių ribinių sąlygų, kintančių laike, bei spręsti nenuostoviąsias pernašos lygtis. Reikšminiai žodžiai: hidrodinamika, skaičiuojamoji fluidų dinamika, skaitinis modeliavimas, trimačiai procesai, vienfaziai srautai, baseinas‐aušintuvas, šilumos mainai First Published Online: 14 Oct 2010
topic Computational Fluid Dynamics (CFD)
numerical simulation
three‐dimensional processes
one‐phase flows
hydrodynamics
lake as a cooler
url https://journals.vgtu.lt/index.php/JEELM/article/view/8077
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AT vladislovaskatinas simulationofconductiveconvectiveheattransferinanaturalbasin
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