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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Main Authors: Albert,Mary Remley, Phetteplace,Gary E
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
Format: Text
Language:English
Published: 1983
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA128793
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA128793
id ftdtic:ADA128793
record_format openpolar
spelling 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
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id 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
_version_ 1766166150879641600