Geothermal heat exchanger with coaxial flow of fluids

The paper deals with a heat exchanger with coaxial flow. Two coaxial pipes of the secondary part were placed directly into a geothermal boring in such a way that geothermal water flows around the outer pipe. Starting from the energy balance of the exchanger formed in this way and the assumption of a...

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Main Authors: Pejić Dragan M., Stojiljković Dragan T., Stojiljković Staniša T., Đurović-Petrović Maja, Mitić Nebojša
Format: Article
Language:English
Published: Association of Chemical Engineers of Serbia 2005-01-01
Series:Hemijska Industrija
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/0367-598X/2005/0367-598X0510275P.pdf
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spelling doaj-e98f57995d774991a10548d24e8d8df12020-11-24T22:48:54ZengAssociation of Chemical Engineers of SerbiaHemijska Industrija 0367-598X2005-01-01599-1027527810.2298/HEMIND0510275PGeothermal heat exchanger with coaxial flow of fluidsPejić Dragan M.Stojiljković Dragan T.Stojiljković Staniša T.Đurović-Petrović MajaMitić NebojšaThe paper deals with a heat exchanger with coaxial flow. Two coaxial pipes of the secondary part were placed directly into a geothermal boring in such a way that geothermal water flows around the outer pipe. Starting from the energy balance of the exchanger formed in this way and the assumption of a study-state operating regime, a mathematical model was formulated. On the basis of the model, the secondary circle output temperature was determined as a function of the exchanger geometry, the coefficient of heat passing through the heat exchange areas, the average mass isobaric specific heats of fluid and mass flows. The input temperature of the exchanger secondary circle and the temperature of the geothermal water at the exit of the boring were taken as known values. Also, an analysis of changes in certain factors influencing the secondary water temperature was carried out. The parameters (flow temperature) of the deep boring B-4 in Sijarinska Spa, Serbia were used. The theoretical results obtained indicate the great potential of this boring and the possible application of such an exchanger. http://www.doiserbia.nb.rs/img/doi/0367-598X/2005/0367-598X0510275P.pdfgeothermal energyheat exchangercoaxial flow
collection DOAJ
language English
format Article
sources DOAJ
author Pejić Dragan M.
Stojiljković Dragan T.
Stojiljković Staniša T.
Đurović-Petrović Maja
Mitić Nebojša
spellingShingle Pejić Dragan M.
Stojiljković Dragan T.
Stojiljković Staniša T.
Đurović-Petrović Maja
Mitić Nebojša
Geothermal heat exchanger with coaxial flow of fluids
Hemijska Industrija
geothermal energy
heat exchanger
coaxial flow
author_facet Pejić Dragan M.
Stojiljković Dragan T.
Stojiljković Staniša T.
Đurović-Petrović Maja
Mitić Nebojša
author_sort Pejić Dragan M.
title Geothermal heat exchanger with coaxial flow of fluids
title_short Geothermal heat exchanger with coaxial flow of fluids
title_full Geothermal heat exchanger with coaxial flow of fluids
title_fullStr Geothermal heat exchanger with coaxial flow of fluids
title_full_unstemmed Geothermal heat exchanger with coaxial flow of fluids
title_sort geothermal heat exchanger with coaxial flow of fluids
publisher Association of Chemical Engineers of Serbia
series Hemijska Industrija
issn 0367-598X
publishDate 2005-01-01
description The paper deals with a heat exchanger with coaxial flow. Two coaxial pipes of the secondary part were placed directly into a geothermal boring in such a way that geothermal water flows around the outer pipe. Starting from the energy balance of the exchanger formed in this way and the assumption of a study-state operating regime, a mathematical model was formulated. On the basis of the model, the secondary circle output temperature was determined as a function of the exchanger geometry, the coefficient of heat passing through the heat exchange areas, the average mass isobaric specific heats of fluid and mass flows. The input temperature of the exchanger secondary circle and the temperature of the geothermal water at the exit of the boring were taken as known values. Also, an analysis of changes in certain factors influencing the secondary water temperature was carried out. The parameters (flow temperature) of the deep boring B-4 in Sijarinska Spa, Serbia were used. The theoretical results obtained indicate the great potential of this boring and the possible application of such an exchanger.
topic geothermal energy
heat exchanger
coaxial flow
url http://www.doiserbia.nb.rs/img/doi/0367-598X/2005/0367-598X0510275P.pdf
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AT đurovicpetrovicmaja geothermalheatexchangerwithcoaxialflowoffluids
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