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...
Main Authors: | , , , , |
---|---|
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 |
id |
doaj-e98f57995d774991a10548d24e8d8df1 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT pejicdraganm geothermalheatexchangerwithcoaxialflowoffluids AT stojiljkovicdragant geothermalheatexchangerwithcoaxialflowoffluids AT stojiljkovicstanisat geothermalheatexchangerwithcoaxialflowoffluids AT đurovicpetrovicmaja geothermalheatexchangerwithcoaxialflowoffluids AT miticnebojsa geothermalheatexchangerwithcoaxialflowoffluids |
_version_ |
1725678184887746560 |