Applied Energy 130 (2014) 748–756
Contents lists available at ScienceDirect
Applied Energy journal homepage: www.elsevier.com/locate/apenergy
Thermodynamic analysis of organic Rankine cycle using zeotropic mixtures Li Zhao ⇑, Junjiang Bao Key Laboratory of Efficient Utilization of Low and Medium Grade Energy, MOE, Tianjin University, No. 92 Weijin Road, 300072 Tianjin, PR China
h i g h l i g h t s A thermodynamic model mainly includes Jacob number is proposed. Ten zeotropic mixture pairs are the working fluid candidates. Heat source inlet temperature has a significant influence on the best composition of zeotropic mixtures. The extent of performance improvement has a positive correlation with temperature glide.
a r t i c l e
i n f o
Article history: Received 23 September 2013 Received in revised form 25 March 2014 Accepted 27 March 2014 Available online 21 April 2014 Keywords: Organic Rankine cycle Zeotropic mixture Jacob number Varying temperature heat source
a b s t r a c t In recent years, more and more attention has been paid to organic Rankine cycle (ORC), which is simply structured, highly reliable and easily maintainable. In order to improve the efficiency of ORC systems, zeotropic mixtures whose phase change process is variable temperature, are used as working fluids to match the temperature profiles of the heat source and heat sink. In this paper, a thermodynamic model which mainly includes Jacob number and the ratio of evaporation temperature and condensation temperature is proposed to forecast the thermal efficiency, output work and exergy efficiency of ORC system with zeotropic mixture. Furthermore, the proposed model programmed by Mablab 2010a is verified by the theoretical data. Then, for different heat source inlet temperature, using different zeotropic mixture pairs, output work that is objective function is maximized by optimizing the evaporation temperature. The results show that if the other working conditions are fixed, the heat source inlet temperature has a significant influence on the best composition of zeotropic mixtures at the optimal evaporation temperature. With the increase of heat source inlet temperature, there exists a heat source inlet temperature that pure working fluid has better system performance than zeotropic mixture. The extent of ORC system performance improvement has a positive correlation with zeotropic mixture’s temperature glide. Ó 2014 Elsevier Ltd. All rights reserved.
1. Introduction Various thermodynamic cycles, including the organic Rankine cycle (ORC), Kalina cycle ,trilateral flash cycle and supercritical Rankine cycle, have been studied for power generation [1]. Compared to other cycles, whose system structure is complex, twophase expansion is difficult or operating pressure is high, organic Rankine cycle is simply structured, highly reliable and easily maintainable [2]. Various types of heat source, including waste heat [3], solar energy [4–6], geothermal energy [7], biomass energy [8] and ocean energy [9], etc., can be utilized by the ORC systems. Meanwhile, it can be coupled with other energy equipment, such as thermoelectric generators [10], fuel cell [11], ICE (internal ⇑ Corresponding author. Tel.: +86 22 27404188. E-mail address:
[email protected] (L. Zhao). http://dx.doi.org/10.1016/j.apenergy.2014.03.067 0306-2619/Ó 2014 Elsevier Ltd. All rights reserved.
combustion engine) [12], seawater desalination system [13], Brayton cycle [14] and GT–MHR (gas turbine–modular helium reactor) [15]. As the critical component in an ORC system, an expander determines whether the whole system is relatively efficient and costeffective [2]. Expanders, can be categorized into many types, such as axial turbine [16], rotary expanders [17], scroll expanders [18] and reciprocal piston expanders [19]. The dynamic modeling [20,21] and control [19] are also very significant for ORC systems. The design methods are the guarantees of the efficient and costeffective ORC systems [22–24]. The temperature of some heat sources (such as waste heat or geothermal heat) is varying during the process; therefore the system efficiency of ORC systems with pure working fluids is quite poor. That is the result of constant-temperature evaporation and condensing for pure working fluids, which leads to bad
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
749
Nomenclatures Abbreviation ORC organic Rankine cycle GT–MHR gas turbine–modular helium reactor CHP combined heat and power CCHP combined cooling, heat and power TG temperature glide or thermoelectric generators REC ratio of evaporation temperature and condensation temperature Symbols Cp E h Ja m p Q r
specific heat at constant Pressure (kJ/kg K) exergy flux (kW) specific enthalpy (kJ/kg) Jacob number mass flow rate (kg/s) pressure (kPa) heat flux (kW) latent heat (kJ/kg)
temperature matching in the evaporator and condenser and large irreversibility. In order to improve the efficiency of such cycles, zeotropic mixtures, whose phase change process is variable temperature, are using as working fluids to match the temperature profiles of the heat source and heat sink, thus a better system performance could be obtained [2]. Li et al. [25] investigated the influence of evaporating temperature and internal heat exchanger. Three pure fluids (R123, R141b and R245ca) and one mixture (R141b/RC318) were used as working fluids. They concluded that the ORC system efficiency of the mixture R141b/RC318 would be better than that of R141b after adding an internal heat exchanger. Wang and Zhao [26] compared three different compositions (0.9/0.1, 0.65/0.35 and 0.45/0.55) of R245fa/R152a to pure R245fa at a low temperature solar ORC. For zeotropic mixtures, a significant increase of thermal efficiencies can be obtained when the outlet of evaporator is superheated with IHE. In an experimental study of by Wang et al. [4], the system efficiency of zeotropic mixtures are comparatively higher than that of R245fa in the experimental condition. In the experimental superheating period, the average power output of M3 (R245fa/ R152a, 0.7/0.3) is higher than that of M1 (R245fa) and M2 (R245fa/R152a, 0.9/0.1) by 29.10% and 28.03%, respectively. Investigating second law efficiency of subcritical cycles, Heberle et al. [27] presented simulations for ORC with isobutane/isopentane and R227ea/R245fa mixtures as working fluids. The composition of mixture, heat source temperature and temperature difference of cooling water are the concerned parameters. The second law efficiency increases in the range of 4.3% and15% for mixtures compared to that of pure fluids for a heat source temperature below 120 °C. Garg et al. [28,29] respectively used isopentane/R-245fa, CO2/isopentane and CO2/propane as working fluids, and evaluated the system performance. A technique of identifying the required source temperature for a given output of the plant and the maximum operating temperature of the working fluid is developed by the authors. For the heat source temperature of 150 °C and 250 °C, when using mixtures as the working fluids of ORC systems, Chys et al. [30] found a potential increment of 16% and 6% in system efficiency respectively. The power generation at optimal condition can be increased by 20% for the low temperature heat source comparing with the pure working fluids. With mixtures of SF6– CO2 as working fluids at a geothermal power plants, Yin et al. [31] investigated both supercritical and transcritical cycles. For working fluids with SF6, the highest Brayton and Rankine cycle
s T W
g
specific entropy (kJ/kg K) temperature (K) power (kW) efficiency
Subscript 0 1, 2, 3 et exer therm c e fluid h p t net
ambient condition al. the state points of the ORC system exergy thermal cooling or condenser evaporation or evaporator working fluid heat source pump turbine the net power
efficiencies are yielded at the composition of 15 and 20 mol%, respectively. From the above survey of literatures, the researches about zeotropic mixture ORC are increasing, but it is still limited and mainly concerned with specific cases (only one or two heat source temperature and few working fluids), and meanwhile, the model to forecast the performance of ideal ORC systems using zeotropic mixtures does not exist. In this paper, a thermodynamic model is proposed to evaluate the output work, thermal efficiency and exergy efficiency of ideal ORC systems for different zeotropic mixtures. Meanwhile, the influence of the heat source temperature on the optimal mass fraction of different zeotropic mixture is emphasized. The effect of temperature glide on the performance of zeotropic ORC systems is also discussed. 2. Thermodynamic analysis of the ORC system with zeotropic mixture 2.1. System presentation The ORC system configuration is shown in Fig. 1(a), including an evaporator, an expander, a condenser and a feed pump. There is usually a storage tank for the collection of working fluids and the maintain of working fluid state at the feed pump inlet. Pumping from the storage tank by the feed pump, working fluid is heated and vaporized in the evaporator by the heat source. The high pressure and temperature vapor enters the turbine, where thermal energy is converted into mechanical energy. Meanwhile, the generator is driven and electricity is generated. After that, the exhaust vapor leaves from the expander and passes the condenser, where it is condensed into saturated or subcooled liquid. The liquid fluid passes through the tank and is pumped into the evaporator, which is the initiate of next cycle. The thermodynamic processes are illustrated on the T–s diagram in Fig.1(b) and (c) for ORC systems with pure fluid and zeotropic mixture. In general, ORC systems have four basic operational processes: liquid fluid’s pressurization process 1–2, liquid fluid’s isobaric vaporization process 2–4, gaseous fluid’s expansion process 4–5 and gaseous fluid’s isobaric liquefaction process 5–1. For the ideal case, the processes 1–2 and 4–5 are the isentropic processes 1–2s and 4–5s, respectively. The difference between pure fluids and zeotropic mixtures is that non-isothermal phase change for zeotropic mixture which will lead to better temperature matching for the varying
750
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
fluids. Due to the impossibility of wet expansion in the expander, dry working fluids are better choices and considered. In this paper, five pure working fluids including R227ea, R236fa, R236ea, R245ca and R245fa, are the basic components and ten zeotropic mixture pairs are the working fluid candidates. The fluid properties of pure fluids are shown in Table 1. About the thermal stability, from the literature [32], the three of the five working fluids including R227ea, R236fa and R245fa were reported that excellent thermal stability up to the following temperatures at which no decomposition was observable in 50–100 h: 425 °C for R227ea, 400 °C for R236fa and 300 °C for R245fa. Due to the similar atoms and structure, the other two fluids (R236ea and R245ca) could be thought as thermal stability in the investigative temperature range. The properties of the mixtures are obtained by REFPROP 9.0 [33]. 2.3. Thermodynamic model Based on the mass and energy balance, the basic equations describing the ORC systems for each individual component are listed as follows: For evaporator:
_ heatsource C p eva ðT h Qe ¼ m _ fluid ðh4 h2 Þ ¼m
in
Th
out Þ
ð1Þ
For expander:
_ fluid ðh4 h5 Þ Wt ¼ m _ fluid ðh4 h5s Þ ¼ gt m
ð2Þ
For condenser:
_ fluid ðh5 h1 Þ Qc ¼ m
ð3Þ
For pump:
_ fluid ðh2 h1 Þ Wp ¼ m ¼
ð4Þ
_ fluid ðh2s h1 Þ m
gp
With respect to the thermodynamic models to predict the thermal efficiency and net work for organic Rankine cycle using pure fluids, there been several related researches on it. Liu et al. [34] presented a thermodynamic model to calculate the thermal efficiency and total heat-recovery efficiency. Their results showed that thermal efficiency is a weak function of the critical temperature, although the thermal efficiency is lower when the critical temperature of working fluids is low. Through the thermodynamic derivation, Mikielewicz and Mikielewicz [35] proposed a performance index to predict the thermal efficiency, which defined a Jacob number. In fact, this Jacob number was not the ratio of vaporization latent heat and sensible heat, but very chose to it. Moreover, Kuo et al. [36] proposed a figure of merit defined as:
Figure of meritðFOMÞ ¼ Ja0:1
T cond T ev ap
0:8 ð5Þ
Fig. 1. The basic ORC system.
temperature heat source and less thermodynamic irreversibility therefore a higher system performance.
which including the Jacob number, evaporation and condensing temperature. Different from [35], this Jacob number was defined as Ja = CpDT/Hv, where CpDT was the vaporization sensible heat and Hv is vaporization latent heat. From their results, a larger ratio of
2.2. The working fluid candidates
Table 1 Fluid properties of pure fluids.
Because the system efficiency, system component sizes, expander design, the system stability, safety and environmental concerns are all affected by the selection of working fluid, working fluid selection is a very important procedure in the design process of an ORC system. Based on the slope of saturation vapor curve, the working fluids could be categorized into dry, wet and isentropic
Working fluid
Alternative name
Pcr (MPa)
Tcr (°C)
1,1,1,2,3,3,3-Heptafluoropropane 1,1,1,3,3,3-Hexafluoropropane 1,1,1,2,3,3-Hexafluoropropane 1,1,1,3,3-Pentafluoropropane 1,1,2,2,3-Pentafluoropropane
R-227ea R-236fa R-236ea R-245fa R-245ca
28.7 31.9 34.1 36.1 38.9
101 124 139 153 174
751
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
vaporization latent heat and sensible heat would result in a smaller figure of merit, therefore a larger thermal efficiency, which illuminated the results of literature [8]. From the study of Stijepovic et al. [37], a smaller the ratio of vaporization latent heat and sensible heat would lead to a larger exergy efficiency. However, they all focused on pure working fluids. Next, a thermodynamic model which mainly includes Jacob number and the ratio of evaporation temperature and condensation temperature is derived to forecast the thermal efficiency, output work and exergy efficiency of ideal ORC systems with zeotropic mixture. In order to simplify the analysis, the assumption that the expansion processes in the expander and the pressurization process in the pump are isentropic has been made in this study. It is worth noting that the assumptions of the isentropic expansion processes in the expander and the isentropic pressurization process in the pump would not affect the comparison between our model and the theoretical model for an ideal ORC system. So the Eq. (6) holds with s5s = s5. According to the state points in Fig. 1(c), the entropy change from the state point 1 to 5 (i.e. 5s) can be approximately simplified as: 3 s5 s1 s4 s3 þ s3 s1 h4Th þ C p13 ln TT 31 e
p13 ln T 3 ¼ Tre þ C T1
ð6Þ
where T e is evaporation temperature for zeotropic mixture which can be expressed as:
h4 h3 T e ¼ s4 s3
ð7Þ
The working fluid’s total absorbed heat in the evaporator can be obtained as:
_ fluid ½C p13 ðT 3 T 1 Þ þ r Qe ¼ m
ð8Þ
The working fluid’s rejected heat the in condenser can be determined as the area between the curve 5-6-1 and x-axis. In fact, compared to the area between the curve 5-6-1 and x-axis, the area of triangle 5-6-1 is so small that it can be neglected. Therefore, the area of trapezoid formed by curve 5-1 and x-axis is thought as the working fluid’s rejected heat the in the condenser, which could be expressed as:
_ fluid ½T 1 ðs5 s1 Þ þ 12 ðT 5 T 1 Þðs5 s1 Þ Qc m _ fluid ðT 1 þ T 5 Þðs5 s1 Þ m _ fluid T c ðs5 s1 Þ ¼ 1m
ð9Þ
2
where T c is condensation temperature for zeotropic mixture which can be expressed as:
h6 h1 T c ¼ s6 s1
ð10Þ
The working fluid mass flow rate is obtained based on energy conservation in evaporator:
_ fluid ¼ m
Pm _ heatsource ðT h C
in
T sat l DT PP Þ
r
W net Q e Q c Q ¼ ¼1 c Qe Qe Qe
ð12Þ
The output work can be defined as:
W net ¼ W t W p ¼ Q e Q c
gexer ¼
W net DE e
ð14Þ
where DEe is the exergy at the side of the heat source in evaporation which could be expressed as:
_ heatsource ½hh DEe ¼ m
in
h0 T 0 ðsh
in
s0 Þ
ð15Þ
Substituting Eqs. (7) and (8) into (11), the thermal efficiency can be expressed as:
gtherm ¼ 1
Ja ln REC ðREC 1Þ1 þ 1=REC 1 þ Ja
ð16Þ
where Ja is the Jacob number, defining as the ratio of sensible heat and the latent heat of evaporation, i.e.
p13 ðT 3 T 1 Þ=r Ja ¼ C
ð17Þ
REC is the ratio of evaporation and condensation temperature and can be obtained as:
T e REC ¼ Tc
ð18Þ
Due to the small different between temperature glides in the evaporator and condenser, with the approximation of arithmetic average evaporation temperature equals to the thermodynamic average evaporation temperature, the radio of T3 and T1 can be simplified as follows: T 4 þT 3 3 T e 12 TGe T e T 4 T T3 2 2 ¼ T þT ¼ REC T T 6 1 6 1 T1 T c 12 TGc T c 2 2
ð19Þ
Substituting Eqs. (7)–(9) into (12), the output work of an ideal ORC is obtained as:
Pm _ heatsource T h in T sat l DT PP Þ½Jað1 lnREC ðREC 1Þ1 W net ¼ C þ 1 1=REC ð20Þ Substituting Eqs. 7, 8, 9, and (14) into (13), the exergy efficiency can be simplified as:
gexer ¼
P ðT h in T sat l DT PP Þ½Jað1 ln REC ðREC 1Þ1 Þ þ 1 1=REC C hh in h0 T 0 ðsh in s0 Þ
ð21Þ
The detail explanations of Eqs. (16), (20), and (21) could be found in Appendix A. Based on the above equations, a program is carried out by MATLAB 2010a with a function calling REFPROP 9.0. Table 2 presents all the input system parameters. To simplify the calculation, it has been made the following assumptions in this paper: the heat and pressure losses in all heat exchangers are neglected; the irreversibilities in the pipes are small and negligible; the organic working
ð11Þ
where DT PP is the pinch point temperature difference and T sat l is the temperature of the saturation liquid when the evaporation begins. The thermal efficiency can be expressed as:
gtherm ¼
The exergy efficiency can be expressed as:
ð13Þ
Table 2 Input system parameters. Initial system parameter
Value
Heat source air inlet temperature (K) Heat source air inlet mass flow (kg/s) Heat source air pressure (bar) Heat sink water inlet temperature (K) Pinch point in the evaporator (K) Pinch point in the condenser (K) Isentropic pump efficiency Isentropic turbine efficiency
423.15 25 1 293.15 30 5 65% 70%
752
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
Table 3 The calculated results of comparison between this work and Chys et al. work [30]. Medium
Pgen (kW)
R245fa-R365mfc R245fa-isopentane Isobutane-isopentane R245fa-pentane
gcycle (%)
Ppump (kW)
[30]
This work
[30]
This work
[30]
This work
5.0 6.3 6.6 5.4
4.99 6.24 6.61 5.31
109.5 110.8 112.8 112.7
109.9 111.6 112.5 111.4
10.82 10.82 10.99 11.12
10.88 10.82 10.99 11.12
Table 4 The calculated results of comparison between this work and Ref. [27] with isobutane/ isopentane (0.5:0.5, by mass).
353.15 363.15 373.15 383.15 393.15 403.15 413.15 423.15 433.15 443.15 453.15
0.210
Exergy efficiency (%) [27]
This work
29.2 31.4 33.2 35 36.7 38.3 40.1 41.6 43.1 45.1 47.8
29.4 31.5 33.5 34.9 36.6 38.1 40.2 41.8 43.0 45.3 47.7
Output Work [MW]
Geothermal water inlet temperature (K)
0.205 0.200 0.195 0.190 0.185 330
R236fa/R236ea
335
340
345
350
355
360
365
Evaporation Temperature [K]
(a) fluid is heated into saturated vapor in the evaporator and cooled to saturated liquid in the condenser.
Mass flow rate [Kg/s]
Using the same input conditions as those in Chys et al. [30] that is a theoretical research, a thermodynamic calculation is carried out to validate the programme. The heat source with inlet temperature of 423.15 K, outlet temperature of 408.15 K and mass flow of 15 kg/s is water at 5 bar, while the heat sink with inlet temperature of 298.15 K and outlet temperature of 308.15 K is water at 4 bar. The efficiencies of pump, turbine and generator are respectively 80% ,60% and 97%. The pinch points in the evaporator and condenser are severally 20 K and 10 K. The results of comparison are listed in Table 3. From that, it shows excellent agreement between the calculated results this paper and Ref. [30]. In an another theoretical research [27], the heat source is the geothermal water of inlet temperature between 353.15 K and 453.15 K, the exergy efficiency is calculated and the other details
0.028 11
0.026 0.024
10
0.022
9
0.020 8 0.018 7 330
0.016 335
340
345
350
355
360
Specific Output Work [Kj/Kg]
2.4. Validation
12
365
Evaporation Temperature [K]
(b) Fig. 2. Effect of evaporation temperature on (a) output work, and (b) mass flow rate and specific output work.
Table 5 Results for zeotropic mixtures with mass fraction ratio 1:1 using different methods.
a b c d e
Fluids
Ja
gtherma (%)
Wneta (MW)
gexera (%)
gthermb (%)
Wnetb (MW)
gexerb (%)
TGe (K)
RDc (%)
RDd (%)
RDe (%)
R227ea/R236fa R227ea/R236ea R236ea/R236fa R245fa/R227ea R245fa/R236fa R245ca/R227ea R245fa/R236ea R236fa/R245ca R245ca/R236ea R245fa/R245ca
1.22 0.97 0.86 0.83 0.75 0.71 0.71 0.67 0.65 0.61
13.35 13.51 13.99 13.59 14.21 13.45 14.38 14.14 14.36 14.69
0.229 0.211 0.199 0.207 0.194 0.208 0.188 0.194 0.188 0.182
40.44 37.21 35.11 36.59 34.20 36.68 33.23 34.27 33.13 32.11
13.30 13.79 14.04 14.10 14.32 14.42 14.43 14.54 14.61 14.75
0.228 0.215 0.200 0.215 0.195 0.223 0.189 0.200 0.191 0.183
40.30 37.97 35.22 37.94 34.48 39.31 33.35 35.23 33.70 32.24
0.95 2.51 0.34 5.63 1.56 10.99 0.46 4.73 2.54 0.84
0.37 2.07 0.36 3.75 0.77 7.21 0.35 2.83 1.74 0.41
0.35 2.07 0.33 3.68 0.81 7.19 0.37 2.79 1.71 0.40
0.35 2.04 0.31 3.69 0.82 7.17 0.36 2.80 1.72 0.40
The The The The The
theoretical data. results obtained by our model. relative deviation of gtherm calculated by different methods. relative deviation of Wnet calculated by different methods. relative deviation of gexer calculated by different methods.
753
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
can be found in Ref. [27]. The results of comparison are listed in Table 4. It also shows reasonable accuracy.
obtained by our model is increasing, however, the real value of thermal efficiency of theoretical data is not always increasing. For example, the results of r245fa/r227ea and r245ca/r227ea
3. Results and discussion 3.2. The determination of the optimal evaporation temperature 3.1. Comparison between our model and theoretical data At the heat source air inlet temperature of 423.15 K, evaporation temperature of 363.15 K and condensation temperature of 298.15 K, the thermal efficiency, net work and exergy efficiency for zeotropic mixtures with mass fraction ratio 1:1 (i.e., 50%/50%, by mass fraction) calculated by different methods are presented in Table 5. Our model are Eqs. 16, 19, and 20, while the theoretical data is based on the mass and energy balance, for example, Eqs. (1)–(4) and Eqs. (12)–(14). The RD (relative deviation) is given by:
RD ¼
xn xt 100% xn
ð22Þ
where xn is the theoretical data while xt is the value obtained by our model. The maximum RD of all the zeotropic mixtures is 7.21% for R245ca/R227ea with a temperature glide larger than 10 K in the evaporator. Besides this, other mixtures have a rather high accuracy less than 4%. It is applicable to determine the thermal efficiency, net work and exergy efficiency. Refs. [36,38] mentioned that the thermal efficiency has a negative correlation with Jacob number for the fixed evaporation temperature and condensation temperature. However, this conclusion is not suitable for zeotropic mixture. It can been seen from Table 4 that with the decrease of the Jacob number, the thermal efficiency
In this part, output work is used as objective function, which is usually the optimizing index in the waste recovery or geothermal plant. The input system parameters are listed in Table 3, of which, the heat source inlet temperature is fixed as 423.15 K. The working fluid studied is R236fa/R236ea (0.5/0.5, by mass fraction) and the evaporation temperature is varying from 333.15 K to 363.15 K. As shown in Fig. 2(a), with the increase of evaporation temperature, the output work increases firstly, and then decrease, i.e., there is a maximum output work corresponding to an optimal evaporation temperature. For R236fa/R236ea, this value is 350 K. This law also exists in the ORCs with pure working fluids [39]. The direct reason is, as presented in Fig. 2(b), when evaporation temperature increases, the mass flow rate will decrease while specific net work will increase, and this combined effect results in the maximum of output work. 3.3. Effect of the heat source inlet temperature on optimal output work In this section, with the method of evaporation temperature optimization previously, the influence of the heat source inlet temperature on the optimal output work for different zeotropic mixtures are shown in Figs. 3 and 4. It can be seen from Fig. 3(a) that at the heat source inlet temperature of 398.15 K, using R245ca/R236ea as working fluid, the optimal output work firstly increase and then decrease with the increase of R245ca mass frac-
0.324 0.098
Output Work [MW]
Output Work [kW]
0.320 0.096 0.094 0.092 0.090
0.316 0.312 0.308 0.304 0.300
Output Work of R245ca/R236ea
Output Work of R245ca/R236ea
0.088 0.0
0.2
0.4
0.6
0.8
0.0
1.0
0.2
0.4
0.6
0.8
Mass fraction of R245ca
Mass fraction of R245ca
(a) 398.15K
(c) 453.15K
1.0
0.246 0.360 0.355
Output Work [MW]
Output Work [MW]
0.243 0.240 0.237 0.234 0.231 0.228
Output Work of R245ca/R236ea
0.0
0.2
0.4
0.6
0.350 0.345 0.340 0.335 0.330 Output Work of R245ca/R236ea
0.325
0.8
1.0
0.0
0.2
0.4
0.6
0.8
Mass fraction of R245ca
Mass fraction of R245ca
(b) 438.15K
(d) 458.15K
1.0
Fig. 3. The output work of R245ca/R236ea at different mass fractions for the different heat source inlet temperature (a) 398.15 K, (b) 438.15 K, (c) 453.15 K, and (d) 458.15 K.
754
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
0.28
0.24
0.18
0.22 398.15K 403.15K 408.15K 413.15K 418.15K 423.15K 428.15K 433.15K
0.20 0.18 0.16 0.14 0.12 0.10
Output Work [MW]
Output Work [MW]
R245fa 10/90 20/80 30/70 40/60 50/50 60/40 70/30 80/20 90/10 R236ea
0.20
0.26
0.08
0.16 0.14 0.12 0.10
0.0
0.2
0.4
0.6
0.8
1.0
Mass fraction of R245ca
0.08
395
Fig. 4. The output work of R245ca/R227ea at different mass fractions for the different heat source inlet temperature.
400
405
410
415
420
425
430
Mass fraction of R245fa Fig. 6. The output work of R245fa/R236ea for the heat source inlet temperature from 398.15 K to 428.15 K at different mass fraction.
14
R245ca/R227ea R245ca/R236ea R245fa/R236ea
0.40
10
R245ca 10/90 20/80 30/70 40/60 50/50 60/40 70/30 80/20 90/10 R236ea
0.35
8
Output Work [MW]
Temperature Glide [K]
12
6 4 2
0.30 0.25 0.20 0.15
0 0.10 0.0
0.2
0.4
0.6
0.8
1.0
Mass fraction of the higher boiling point component
0.05 390
Fig. 5. The temperature glides for different zeotropic mixtures at the heat source inlet temperature 428.15 K.
tion. When the mass fraction of R245ca is 0.6, there exists a maximum value for the optimal output work. When the heat source inlet temperature increase, the optimal output work at different R245ca mass fraction will all increase. However, the R245ca mass fraction corresponding to the maximum optimal output work will decrease from 0.6 (Fig. 3(a)) to 0.3 (Fig. 3(c)). Furthermore, when the heat source inlet temperature reaches 458.15 K, the output work of pure R245ca is larger than R245ca/R236ea. As presented in Fig. 4, when using other zeotropic mixtures, the same tendency is found. This results declare that the superiority of ORCs with zeotropic mixtures has close connections with the heat source inlet temperature, which means that when the heat source inlet temperature is higher than some value, ORCs with zeotropic mixtures are not as good as those with pure working fluids. At the same time, compared Fig. 3 with Fig. 4, it can be found that the heat source inlet temperature at which ORCs with zeotropic mixtures are not as good as those with pure working fluids is not the same for different zeotropic mixtures. For example, when using R245ca/R236ea, ORCs with pure R245ca have better system performance than those with R245ca/R236ea at the heat source inlet temperature 458.15 K, while for R245ca/R227ea, this temperature is 428.15 K. The mixtures considered have fluids which are quite similar in terms of thermodynamic properties. In order to remove the effect of similar working fluids on the results, the research about hydrocarbons in Ref. [40] is also reviewed for comparison. In this
400
410
420
430
440
450
460
The heat source inlet temperature [K] Fig. 7. The output work of R245ca/R236ea for the heat source inlet temperature from 398.15 K to 458.15 K at different mass fraction.
paper, with the geothermal resource of 280 °F(410.93 K) and 360 °F(455.37 K), the optimal composition of Isopentane/isobutane changed from 42%/58% to 35%/65%. This result showed that the influence of heat source inlet temperature on the optimal composition of zeotropic mixture for ORC systems is independent of the working fluid’s type. 3.4. Effect of the temperature glide for different zeotropic mixtures In this part, the effect of the temperature glide on the optimal output work is discussed. The temperature glides for different zeotropic mixtures at the heat source inlet temperature 428.15 K are plotted in Fig. 5. It can be seen from Fig. 5 that due to the largest difference of boiling point, R245ca/R227ea has the largest temperature glide, while R245fa/R236ea stays lowest. The optimal output work for different heat source inlet temperature with various zeotropic mixtures are presented in Figs. 6–8. Compared with these three figures, it can be found that larger temperature glide means greater improvement for the optimal output work at the different mass fractions. Ref. [38] found that the optimal output work is closely linked with the heat source inlet temperature and it is a weak function of working fluids. From current results, it only holds true for the zeotropic mixture with small temperature glide.
755
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
The Eq. (17) could be turned into:
0.30
Output Work [MW]
0.27 0.24
R245ca 10/90 20/80 30/70 40/60 50/50 60/40 70/30 80/20 90/10 R227ea
0.21 0.18 0.15 0.12 0.09 395
400
405
410
415
420
425
430
p13 Ja C ¼ T3 T1 r Substituting Eq. (24) into (23), it could be expressed as: Ja
gtherm ¼ 1 T 3 T 1 ¼1
Mass fraction of R245ca
ð25Þ
T1
1þ
C p13 ðT 3 T 1 Þ r
Substituting Eqs. (17)–(19) into (25) and with the approximation of T c =T 1, the thermal efficiency can be expressed as:
gtherm ¼ 1 4. Conclusions
T c ln TT 31 þ TTec
C ðT T Þ 1 þ p13 r 3 1 T c JaT 1 ln TT 31 þ TTec T 1 T 3 T 1 C ðT T Þ 1 þ p13 r 3 1 T c Ja ln TT 31 þ TTec T 1 T 3 1
¼1
435
Fig. 8. The output work of R245ca/R227ea for the heat source inlet temperature from 398.15 K to 433.15 K at different mass fractions.
ð24Þ
Ja ln REC ðREC 1Þ1 þ 1=REC 1 þ Ja
ð26Þ
For output work:
In this paper, the thermodynamic analysis of organic Rankine cycle using zeotropic mixture is presented. The following conclusions can be drawn: (1) A thermodynamic model is proposed to forecast the thermal efficiency, output work and exergy efficiency of an ideal ORC system with zeotropic mixuture. There is not a rigorously negative correlation between the thermal efficiency and Jacob number. (2) When the other system parameters are fixed, there exists an optimal evaporation temperature corresponding to a maximum output work. (3) At fixed other working conditions, for the optimal evaporation temperature, the heat source inlet temperature has a significant influence on the best composition of zeotropic mixtures. With the increase of heat source inlet temperature, there exists a heat source inlet temperature that pure working fluid has better system performance than zeotropic mixture. (4) The extent of performance improvement with zeotropic mixtures as working fluids has a positive correlation with its temperature glide.
W net ¼ W t W p ¼ Q e Q c _ fluid ½C p13 ðT 3 T 1 Þ þ r m _ fluid T c ðs5 s1 Þ ¼m p13 ln T 3 Þ _ fluid ½C p13 ðT 3 T 1 Þ þ r T c ðTr þ C ¼m T1 e h i m C P _ heatsource ðT h in T sat l DT PP Þ p13 ln T 3 ¼ C p13 ðT 3 T 1 Þ þ r T c Tre þ C r T1 h i _ heatsource ðT h in T sat l DT PP Þ 1 þ C p13 ðTr 3 T 1 Þ C p13 T c ln TT 31 TTec ¼ C P m r " # _ heatsource ðT h in T sat l DT PP Þ 1 þ Cp13 ðT 3 T 1 Þ Tc T Ja ln T 3 Tc ¼ C P m r
T1
3 1 T1
T1
Te
ð27Þ Substituting Eqs. ()()()(17)–(19) into (27), the output work of an ideal ORC is obtained as:
Pm _ heatsource ðT h W net ¼ C
in
T sat l DT PP Þ½Jað1 ln REC
ðREC 1Þ1 Þ þ 1 1=REC
ð28Þ
Substituting Eqs. (27) and (14) into (13), the exergy efficiency can be simplified as
gexer ¼
P ðT h in T sat l DT PP Þ½Jað1 lnREC ðREC 1Þ1 Þ þ 1 1=REC C hh in h0 T 0 ðsh in s0 Þ ð29Þ
Acknowledgement This study was supported by National Natural Science Foundation of China (No. 51276123). Appendix A. The demonstration of Eqs. (16), (20), and (21) is listed as follows:
gtherm ¼ WQnete ¼ Q eQQe c ¼ 1 QQ ce ¼1
¼1 ¼1
_ fluid T c ðs5 s1 Þ m _ fluid ½C p13 ðT 3 T 1 Þ þ r m T c Tre þ C p13 ln TT 31 C p13 ðT 3 T 1 Þ þ C p13 T c ln TT 31 þ TT ce r C ðT T Þ 1 þ p13 r 3 1
r
ð23Þ
References [1] Chen H, Goswami DY, Stefanakos EK. A review of thermodynamic cycles and working fluids for the conversion of low-grade heat. Renew Sustain Energy Rev 2010;14:3059–67. [2] Bao J, Zhao L. A review of working fluid and expander selections for organic Rankine cycle. Renew Sustain Energy Rev 2013;24:325–42. [3] Hung TC, Shai TY, Wang SK. A review of organic Rankine cycles (ORCs) for the recovery of low-grade waste heat. Energy 1997;22:661–7. [4] Wang JL, Zhao L, Wang XD. A comparative study of pure and zeotropic mixtures in low-temperature solar Rankine cycle. Appl Energy 2010;87:3366–73. [5] Wang JL, Zhao L, Wang XD. An experimental study on the recuperative low temperature solar Rankine cycle using R245fa. Appl Energy 2012;94:34–40. [6] He Y, Mei D, Tao W, Yang W, Liu H. Simulation of the parabolic trough solar energy generation system with organic Rankine cycle. Appl Energy 2012;97:630–41. [7] Shengjun Z, Huaixin W, Tao G. Performance comparison and parametric optimization of subcritical organic Rankine cycle (ORC) and transcritical power cycle system for low-temperature geothermal power generation. Appl Energy 2011;88:2740–54. [8] Drescher U, Brüggemann D. Fluid selection for the organic Rankine cycle (ORC) in biomass power and heat plants. Appl Therm Eng 2007;27:223–8.
756
L. Zhao, J. Bao / Applied Energy 130 (2014) 748–756
[9] Sun F, Ikegami Y, Jia B, Arima H. Optimization design and exergy analysis of organic Rankine cycle in ocean thermal energy conversion. Appl Ocean Res 2012;35:38–46. [10] De Pascale A, Ferrari C, Melino F, Morini M, Pinelli M. Integration between a thermophotovoltaic generator and an organic Rankine cycle. Appl Energy 2012;97:695–703. [11] Zhao P, Wang J, Gao L, Dai Y. Parametric analysis of a hybrid power system using organic Rankine cycle to recover waste heat from proton exchange membrane fuel cell. Int J Hydrogen Energy 2012;37:3382–91. [12] Vaja I, Gambarotta A. Internal combustion engine (ICE) bottoming with organic Rankine cycles (ORCs). Energy 2010;35:1084–93. [13] Sharaf MA, Nafey AS, García-Rodríguez L. Exergy and thermo-economic analyses of a combined solar organic cycle with multi effect distillation (MED) desalination process. Desalination 2011;272:135–47. [14] Garcia RF. Efficiency enhancement of combined cycles by suitable working fluids and operating conditions. Appl Therm Eng 2012;42:25–33. [15] Yari M, Mahmoudi SMS. Utilization of waste heat from GT-MHR for power generation in organic Rankine cycles. Appl Therm Eng 2010;30:366–75. [16] Fiaschi D, Manfrida G, Maraschiello F. Thermo-fluid dynamics preliminary design of turbo-expanders for ORC cycles. Appl Energy 2012;97:601–8. [17] Antonelli M, Baccioli A, Francesconi M, Desideri U, Martorano L. Operating maps of a rotary engine used as an expander for micro-generation with various working fluids. Appl Energy 2014;113:742–50. [18] Clemente S, Micheli D, Reini M, Taccani R. Energy efficiency analysis of Organic Rankine Cycles with scroll expanders for cogenerative applications. Appl Energy 2012;97:792–801. [19] Zhang J, Zhou Y, Li Y, Hou G, Fang F. Generalized predictive control applied in waste heat recovery power plants. Appl Energy 2013;102:320–6. [20] Xie H, Yang C. Dynamic behavior of Rankine cycle system for waste heat recovery of heavy duty diesel engines under driving cycle. Appl Energy 2013;112:130–41. [21] Bamgbopa MO, Uzgoren E. Numerical analysis of an organic Rankine cycle under steady and variable heat input. Appl Energy 2013;107:219–28. [22] Lecompte S, Huisseune H, van den Broek M, De Schampheleire S, De Paepe M. Part load based thermo-economic optimization of the Organic Rankine Cycle (ORC) applied to a combined heat and power (CHP) system. Appl Energy 2013;111:871–81. [23] DiGenova KJ, Botros BB, Brisson JG. Method for customizing an organic Rankine cycle to a complex heat source for efficient energy conversion, demonstrated on a Fischer Tropsch plant. Appl Energy 2013;102:746–54. [24] Chen Q, Xu J, Chen H. A new design method for organic Rankine cycles with constraint of inlet and outlet heat carrier fluid temperatures coupling with the heat source. Appl Energy 2012;98:562–73.
[25] Li W, Feng X, Yu LJ, Xu J. Effects of evaporating temperature and internal heat exchanger on organic Rankine cycle. Appl Therm Eng 2011;31:4014–23. [26] Wang XD, Zhao L. Analysis of zeotropic mixtures used in low-temperature solar Rankine cycles for power generation. Sol Energy 2009;83:605–13. [27] Heberle F, Preißinger M, Brüggemann D. Zeotropic mixtures as working fluids in organic Rankine cycles for low-enthalpy geothermal resources. Renew Energy 2012;37:364–70. [28] Garg P, Kumar P, Srinivasan K, Dutta P. Evaluation of carbon dioxide blends with isopentane and propane as working fluids for organic Rankine cycles. Appl Therm Eng 2013;52:439–48. [29] Garg P, Kumar P, Srinivasan K, Dutta P. Evaluation of isopentane, R-245fa and their mixtures as working fluids for organic Rankine cycles. Appl Therm Eng 2013;51:292–300. [30] Chys M, van den Broek M, Vanslambrouck B, De Paepe M. Potential of zeotropic mixtures as working fluids in organic Rankine cycles. Energy 2012;44:623–32. [31] Yin H, Sabau AS, Conklin JC, McFarlane J, Qualls AL. Mixtures of SF6–CO2 as working fluids for geothermal power plants. Appl Energy 2013;106:243–53. [32] Angelino G, Invernizzi C. Experimental investigation on the thermal stability of some new zero ODP refrigerants. Int J Refrig 2003;26:51–8. [33] Lemmon EW, McLinden MO, Huber ML. NIST reference fluid thermodynamic and transport properties – REFPROP. 9.0 ed: NIST Standard Reference, Database 23, 2012. [34] Liu B, Chien K, Wang C. Effect of working fluids on organic Rankine cycle for waste heat recovery. Energy 2004;29:1207–17. [35] Mikielewicz D, Mikielewicz J. A thermodynamic criterion for selection of working fluid for subcritical and supercritical domestic micro CHP. Appl Therm Eng 2010;30:2357–62. [36] Kuo C, Hsu S, Chang K, Wang C. Analysis of a 50 kW organic Rankine cycle system. Energy 2011;36:5877–85. [37] Stijepovic MZ, Linke P, Papadopoulos AI, Grujic AS. On the role of working fluid properties in organic rankine cycle performance. Appl Therm Eng 2012;36:406–13. [38] Wang D, Ling X, Peng H, Liu L, Tao L. Efficiency and optimal performance evaluation of organic Rankine cycle for low grade waste heat power generation. Energy 2013;50:343–52. [39] He C, Liu C, Gao H, Xie H, Li Y, Wu S, et al. The optimal evaporation temperature and working fluids for subcritical organic Rankine cycle. Energy 2012;38:136–43. [40] Demuth OJ. Analyses of mixed hydrocarbon binary thermodynamic cycles for moderate temperature geothermal resources. Idaho Falls (USA): Technical Report of EG&G Idaho Inc.; 1981.