Computer Models for Two-Dimensional Steady-State Heat Conduction
This report outlines the development and verification of two computer models of two-dimensional steady-state heat conduction a variety of boundary conditions. One is a finite difference program and the other is a finite element program. The results of each program are compared to two analytic soluti...
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ftdtic:ADA128793 2023-05-15T17:57:40+02:00 Computer Models for Two-Dimensional Steady-State Heat Conduction Albert,Mary Remley Phetteplace,Gary E COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1983-04 text/html http://www.dtic.mil/docs/citations/ADA128793 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA128793 en eng http://www.dtic.mil/docs/citations/ADA128793 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Numerical Mathematics Computer Programming and Software Thermodynamics *COMPUTER PROGRAMS *STEADY STATE *FINITE ELEMENT ANALYSIS *FINITE DIFFERENCE THEORY *CONDUCTION(HEAT TRANSFER) MATHEMATICAL MODELS PIPES NODES TEMPERATURE GRADIENTS RECTANGULAR BODIES DIFFERENTIAL EQUATIONS FROST BURIED OBJECTS HEAT FLUX THERMAL BOUNDARY LAYER WAVE EQUATIONS PERMAFROST DERIVATIVES(MATHEMATICS) Semi infinite boundaries PE62730A AST42 WU017 Text 1983 ftdtic 2016-02-20T22:34:28Z This report outlines the development and verification of two computer models of two-dimensional steady-state heat conduction a variety of boundary conditions. One is a finite difference program and the other is a finite element program. The results of each program are compared to two analytic solutions, and to one another. Sample input and output, and user instructions for each program are included. The programs have the same accuracy when modeling problems involving rectangular boundaries. The finite element method is better able to model curved boundaries, while the finite difference program is easier to use. Text permafrost Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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ftdtic |
language |
English |
topic |
Numerical Mathematics Computer Programming and Software Thermodynamics *COMPUTER PROGRAMS *STEADY STATE *FINITE ELEMENT ANALYSIS *FINITE DIFFERENCE THEORY *CONDUCTION(HEAT TRANSFER) MATHEMATICAL MODELS PIPES NODES TEMPERATURE GRADIENTS RECTANGULAR BODIES DIFFERENTIAL EQUATIONS FROST BURIED OBJECTS HEAT FLUX THERMAL BOUNDARY LAYER WAVE EQUATIONS PERMAFROST DERIVATIVES(MATHEMATICS) Semi infinite boundaries PE62730A AST42 WU017 |
spellingShingle |
Numerical Mathematics Computer Programming and Software Thermodynamics *COMPUTER PROGRAMS *STEADY STATE *FINITE ELEMENT ANALYSIS *FINITE DIFFERENCE THEORY *CONDUCTION(HEAT TRANSFER) MATHEMATICAL MODELS PIPES NODES TEMPERATURE GRADIENTS RECTANGULAR BODIES DIFFERENTIAL EQUATIONS FROST BURIED OBJECTS HEAT FLUX THERMAL BOUNDARY LAYER WAVE EQUATIONS PERMAFROST DERIVATIVES(MATHEMATICS) Semi infinite boundaries PE62730A AST42 WU017 Albert,Mary Remley Phetteplace,Gary E Computer Models for Two-Dimensional Steady-State Heat Conduction |
topic_facet |
Numerical Mathematics Computer Programming and Software Thermodynamics *COMPUTER PROGRAMS *STEADY STATE *FINITE ELEMENT ANALYSIS *FINITE DIFFERENCE THEORY *CONDUCTION(HEAT TRANSFER) MATHEMATICAL MODELS PIPES NODES TEMPERATURE GRADIENTS RECTANGULAR BODIES DIFFERENTIAL EQUATIONS FROST BURIED OBJECTS HEAT FLUX THERMAL BOUNDARY LAYER WAVE EQUATIONS PERMAFROST DERIVATIVES(MATHEMATICS) Semi infinite boundaries PE62730A AST42 WU017 |
description |
This report outlines the development and verification of two computer models of two-dimensional steady-state heat conduction a variety of boundary conditions. One is a finite difference program and the other is a finite element program. The results of each program are compared to two analytic solutions, and to one another. Sample input and output, and user instructions for each program are included. The programs have the same accuracy when modeling problems involving rectangular boundaries. The finite element method is better able to model curved boundaries, while the finite difference program is easier to use. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Albert,Mary Remley Phetteplace,Gary E |
author_facet |
Albert,Mary Remley Phetteplace,Gary E |
author_sort |
Albert,Mary Remley |
title |
Computer Models for Two-Dimensional Steady-State Heat Conduction |
title_short |
Computer Models for Two-Dimensional Steady-State Heat Conduction |
title_full |
Computer Models for Two-Dimensional Steady-State Heat Conduction |
title_fullStr |
Computer Models for Two-Dimensional Steady-State Heat Conduction |
title_full_unstemmed |
Computer Models for Two-Dimensional Steady-State Heat Conduction |
title_sort |
computer models for two-dimensional steady-state heat conduction |
publishDate |
1983 |
url |
http://www.dtic.mil/docs/citations/ADA128793 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA128793 |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA128793 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766166150879641600 |