Experimental investigation of a forced convection heat transfer of the organic fluid r-125 at supercritical pressures and under organic rankine cycle conditions

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dc.contributor.author Lazova, M. en
dc.contributor.author Kaya, A. en
dc.contributor.author Billiet, M. en
dc.contributor.author Lecompte, S. en
dc.contributor.author De Paepe, M. en
dc.date.accessioned 2017-09-19T12:48:25Z
dc.date.available 2017-09-19T12:48:25Z
dc.date.issued 2017 en
dc.description Papers presented at the 13th International Conference on Heat Transfer, Fluid Mechanics and Thermodynamics, Portoroz, Slovenia on 17-19 July 2017 . en
dc.description.abstract The organic Rankine cycle (ORC) is a suitable technology for utilizing low-grade temperature heat sources of ~100 °C from various industry processes. In the ORC cycle an organic fluid with a lower boiling point is used as a working medium. The performance of the ORCs has advanced significantly in the last decades. However, there is still a possibility of improving the efficiency of this cycle. The supercritical heat transfer in the heat exchanger ensures better thermal match between the heating and working fluids temperatures glides in the heat exchanger. Hence, better understanding of the heat transfer phenomena to a fluid at supercritical state in a horizontal flow and in a large diameter tube is of great importance. Therefore, the tests are performed in a counter-current tube-in-tube test section positioned horizontally with a total length of 4 m and a tube diameter of 0.0286 m. R-125 is used as a working fluid in the experiments. During the measurements the temperature of the heating fluid was 90 °C, the mass flow rate and the pressure of the working fluid R-125 was in the range of 0.2–0.3 kg/s and 38–55 bar respectively. Furthermore, results from the pressure and temperature measurements obtained at the inlet and at the outlet of the test section are reported. The results show that the overall heat transfer coefficient is influenced by the mass flow rate of the organic fluid. At pressures close to the critical pressure of R-125 higher values of the overall heat transfer coefficients are determined. Deteriorated heat transfer is not likely to occur at these operating conditions because the critical heat flux is higher than the one obtained from the measurements. A comparison between the experimental Nusselt number with heat transfer (Nusselt) correlations from the literature is done and the measurement points fall within the uncertainty ranges of both heat transfer correlations. en
dc.description.sponsorship International centre for heat and mass transfer. en
dc.description.sponsorship American society of thermal and fluids engineers. en
dc.format.extent 7 pages en
dc.format.medium PDF en
dc.identifier.uri http://hdl.handle.net/2263/62349
dc.language.iso en en
dc.publisher HEFAT en
dc.rights University of Pretoria en
dc.subject Forced convection heat transfer en
dc.subject Organic fluid r-125 en
dc.subject Supercritical pressures en
dc.subject Organic rankine cycle conditions en
dc.title Experimental investigation of a forced convection heat transfer of the organic fluid r-125 at supercritical pressures and under organic rankine cycle conditions en
dc.type Presentation en


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