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Article

CO2 with Mechanical Subcooling vs. CO2 Cascade Cycles for Medium Temperature Commercial Refrigeration Applications Thermodynamic Analysis

Department of Mechanical Engineering and Construction, Jaume I University, Campus de Riu Sec s/n, Castellón de la Plana, E-12071, Spain
*
Author to whom correspondence should be addressed.
Appl. Sci. 2017, 7(9), 955; https://doi.org/10.3390/app7090955
Submission received: 24 July 2017 / Revised: 4 September 2017 / Accepted: 11 September 2017 / Published: 16 September 2017
(This article belongs to the Section Mechanical Engineering)

Abstract

:
A recent trend to spread the use of CO2 refrigeration cycles in warm regions of the world is to combine a CO2 cycle with another one using a high performance refrigerant. Two alternatives are being considered: cascade and mechanical subcooling systems. Both respond to a similar configuration of the refrigeration cycle, they being based on the use of two compressors and same number of heat exchangers. However, the compressor, heat exchanger sizes and energy performance differ a lot between them. This work, using experimental relations for CO2 and R1234yf semi-hermetic compressors analyzes in depth both alternatives under the warm climate of Spain. In general, it was concluded that the CO2 refrigeration solution with mechanical subcooling would cover all the conditions with high overall energy efficiency, thus it being recommended for further extension of the CO2 refrigeration applications.

1. Introduction

Carbon dioxide was spread out all over the world as refrigerant because it combines excellent environmental (GWP = 1) and safety properties (A1), despite its differences in regards to traditional refrigerants, such as high working pressures, low critical temperature and high densities. After the approval of the F-Gas Regulation [1] in Europe in 2014, the implication in the industry with this refrigerant was taken a step forward, especially in commercial refrigeration, whose systems are extreme energy consumers and commonly characterized by large leakage rates of refrigerant. Regarding the environmental impact, the use of CO2 practically eliminates the direct effect of the refrigeration system, thanks to its low GWP. However, the indirect impact associated with the energy consumption of the plant is an issue still under analysis and contrast among the scientific community and the industry sector. In cold regions of the planet, with low average annual temperatures below 14–15 °C, the standard CO2 cycles perform with energy efficiency levels higher than the conventional HFC-based plants [2]. However, when the environment temperature rises, the standard CO2 systems [3] are not able to reach the performance of the formers, and thus, advanced and more complex systems must be considered to be able to mitigate indirect impact of the system.
The search for improvements in CO2 standard refrigeration cycles follow two main directions: new components and the combination of CO2 cycles with other systems. Regarding new components, the CO2 expander concept is still under maturation, few experimental works were found in the literature, such as the experimental tests with a rotary vane expander of Jia et al. [4] and with a two-rolling piston expander of Hu et al. [5]. However, great progress was achieved in the last decade regarding the ejector technology; it was already implemented in many plants all over the world, where the energy improvements were experimentally demonstrated [6]. Now, research on ejector technology is focused on achieving adaptable ejectors to all the operation range of the plants, such as the multi-ejector concept of Hafner et al. [7] or the adjustable ejector concept of Lawrence and Elbel [8], among others. On the other side, scientists and industry are working on the thermal integration of CO2 refrigeration cycles with other energy systems to obtain higher overall energy efficiency to make CO2 more competitive. The attempts correspond to the integration of the CO2 refrigeration plants with water heating systems and air conditioning systems [9], desiccant wheels [10], absorption plants [11], etc.; where in all the cases important overall increases of the energy efficiency were achieved.
Another type of CO2 combined refrigeration system, widely implemented in the last decade in the commercial sector, is the cascade system using CO2 as low temperature refrigerant [12]. This combination corresponds to the thermal coupling of two single stage cycles working with different refrigerants, where the high temperature cycle keeps the CO2 low temperature cycle always in subcritical conditions, thus avoiding the high operating pressures of CO2 and the need for regulation of the high pressure in transcritical conditions [13]. As analyzed by Llopis et al. [14], this cycle overcomes the energy efficiency levels of standard CO2 refrigeration cycles and it reaches comparable coefficient of performance (COP) values than the current systems in commercial refrigeration at low evaporation levels and high environment temperatures. In addition, from the point of view of environmental impact, this system presents low values of TEWI among the solutions adapted to the new F-Gas Regulation. Similar to the cascade solution, since the operating cycle is equivalent, another CO2 combined cycle is attracting attention in the last years, the thermal joining of a CO2 cycle with a dedicated mechanical subcooling system. This option was studied from a theoretical point of view by Hafner et al. [15], Gullo el. at. [16] and Llopis et al. [17], and from an experimental point of view by Nebot-Andrés et al. [18] and Eikevik et al. [19]. This cycle is characterized by a main refrigeration cycle working with CO2 that can be operated in subcritical or transcritical modes which is helped by another vapor compression system, the dedicated mechanical subcooling cycle, providing CO2 a large subcooling at the exit of the gas-cooler/condenser. The benefits of this combination are a large increment of the cooling capacity, reductions of the optimum CO2 high working pressure and an important increment of the overall energy efficiency. Nebot-Andrés et al. [18], for an evaporation level of 0 °C, increments on cooling capacity of 34.9% were measured and, referring to COP, increments of 22.8% at 30.2 °C of heat rejection temperature. At 40 °C of heat rejection temperature, the increments are 40.7% of cooling capacity and 17.3% of COP. These increments are calculated considering a single-stage CO2 transcritical plant without internal heat exchanger as base line.
These last approaches, i.e., the cascaded CO2 and the subcooled CO2 solutions, are being considered to spread the use of CO2 in centralized refrigeration systems at a medium temperature level in medium to warm regions of the planet such as Spain or Italy. As mentioned, both refrigeration schemes have similar configuration of the refrigeration cycle: one rack of compressors for the CO2 and another for the high temperature/subcooling cycle and same number of heat exchangers. However, they have differences in the operation of the components that compose the cycle. One of the main differences, which is discussed in Section 2, is that the high-pressure CO2 heat exchangers can operate as single-phase/two-phase or two-phase/two-phase (cascade) heat exchangers, being the heat transfer rate different in each operating mode. This work aims to analyze which cycle configuration (cascade or mechanical subcooling) is recommended for different operating conditions. The analysis is based on simplified models close to reality, since they use real performances of the compressors. The comparison provides clear conclusions about the application range, advantages and disadvantages of each cycle. In the paper, first, the optimum operating conditions of each cycle are established; then for the optimum conditions, the reached COP values and the ratio of electrical consumption of the compressors are presented. Next, energy efficiency results of both solutions are merged to determine at which operating conditions each solution is the best performing system. Finally, both systems are evaluated under the different climate conditions of Spain to obtain clear conclusions about their possible implementation.

2. Refrigeration Cycles, Models and Assumptions

The cascade refrigeration cycle and the mechanical subcooling (MS) cycle can be represented by the refrigeration scheme detailed in Figure 1. Essentially, both systems include these main components with the following operating characteristics:
  • A main cycle, working with CO2 as refrigerant, which absorbs energy from the cold source.
  • A CO2 compressor, subcritical-rated for the cascade configuration and transcritical-rated for the MS configuration.
  • A CO2 gas-cooler, which performs heat rejection to the hot sink.
  • A second CO2 heat exchanger acting as CO2 condenser for the cascade system and as CO2 subcooler for the MS configuration.
  • An expansion system: composed of the ‘vessel + expansion valve’ for the cascade configuration and of a ‘back-pressure + vessel + expansion valve’ for the MS cycle.
  • An auxiliary single-stage refrigeration cycle: working with another refrigerant (HCs, HFOs, NH3, HFCs) as high temperature cycle in the cascade configuration and as dedicated mechanical subcooling cycle for the MS configuration. The auxiliary system, whose refrigerant is not distributed to the cooling appliances, absorbs heat from the intermediate temperature level and performs heat rejection to the same hot sink as the main cycle. In the cascade configuration, the auxiliary cycle performs CO2 condensation and in the MS it only subcools the CO2 at the exit of the gas-cooler.
The operation of the cycle of Figure 1 as cascade or as MS cycle will depend on the hot sink temperature (TH) and on the high-pressure fixed by the back-pressure valve (Phigh), as detailed in the following subsections.

2.1. CO2 Refrigeration Cycle with Mechanical Subcooling (MS Cycle)

Essentially, the CO2 refrigeration cycle with mechanical subcooling corresponds to a main CO2 single-stage cycle that uses an auxiliary cycle, with small capacity, to provide subcooling at the exit of the gas-cooler/condenser [17]. This cycle operates in subcritical or transcritical conditions depending on the heat rejection temperature (TH) and on the high-pressure established by the back-pressure valve (Phigh).
The transition from subcritical to transcritical conditions was investigated by Ge et al. [20], Shao et al. [21], Tsamos el at. [22] and Sanchez et al. [23] for standard CO2 refrigeration cycles, however, no reference for the transition was found when the CO2 cycle uses a mechanical subcooling system. For the analysis of the MS cycle, the transition from transcritical to subcritical was established in terms of the maximum COP value reached by each operating mode although this transition in real plants would be difficult. The considerations are the following:
If saturation pressure of CO2 at TH is lower than the pressure fixed by the back-pressure (Phigh) and this last is lower than the critical pressure of CO2 (73.773 bar), the optimum operation conditions will be in subcritical-mode with liquid subcooling. These boundary conditions are detailed by Equation (1), and the corresponding pressure-enthalpy diagram of CO2 represented in Figure 2. In this type of operation, the first CO2 heat exchanger acts as condenser (point 2 to 3) and the subcooler subcools liquid CO2 (points 3 to 4). The case of partial condensation in the CO2 heat exchanger (point 2 to 3*) is possible, but the best energy results are obtained for complete condensation.
P sat , CO 2 ( T H ) < P high P crit , CO 2  
P high > P crit , CO 2  
For pressures fixed by the back-pressure (Phigh) higher than the critical pressure, Equation (2), the optimum operating conditions are in transcritical mode, as represented by Figure 3. For this mode of operation, the first CO2 heat exchanger acts as gas-cooler (point 2 to 3) and the subcooler subcools gas or liquid depending on the high-pressure and TH temperature (in red). The intermediate temperature (TI) corresponds to the evaporating level of the high pressure cicle, in green, and is always lower than TH.

2.2. Cascade Refrigeration Cycle

Cascade refrigeration cycle corresponds to the combination of two main refrigeration cycles, one cycle working with CO2 in the low temperature level, which is condensed and maintained in subcritical, by another cycle that uses a refrigerant with good performance at high evaporation temperatures. In this case, both cycles are necessary, since the operation of the low temperature cycle depends on the operation of the high temperature cycle. In addition in this case, the high temperature cycle has similar or higher cooling capacity than the low temperature cycle.
Figure 4 represents the operation of the CO2 cycle in a cascade system. This is the mode of operation if the condition established by Equation (3) or Equation (4) is satisfied. That is, when the pressure established by the back-pressure (if present) or by the thermal equilibrium of condensation (Phigh) is lower than the CO2 saturation pressure at TH, Equation (3). As established in Equation (4), if TH is higher than the critical temperature of CO2, the high-pressure (Phigh) must be lower than the critical one to satisfy the condition.
P high < P sat , CO 2 ( T H )   if   T H T crit , CO 2 ,   OR  
P high < P crit , CO 2   if   T H > T crit , CO 2
In the subcritical mode, the gas-cooler performs a small heat rejection to TH and then the high-temperature cycle condenses CO2 until saturated liquid. Subcooling is possible, but it offers worse results than the exit in saturation conditions because the intermediate temperature will need to descend.
This cycle was experimentally investigated by Dopazo et al. [24] using NH3/CO2 and Sanz et al. [12] using HFC134a/CO2.

2.3. Calculation Models and Assumptions

We performed the analysis of the MS and the cascade cycles using simplified but realistic models, which assumptions are detailed then.
CO2 compressor for both configurations is modeled using the overall efficiency as a linear relation with the compression ratio, as detailed by Equation (5). We fitted this relation using experimental data of a semi-hermetic single-stage CO2 compressor able to operate in subcritical or transcritical [23].
η G , CO 2 = 0.7359 0.0517 t CO 2
For either the MS and cascade configurations, an approach temperature in gas-cooler of 5 K regards the environment temperature and 10 K of superheating degree in evaporator are chosen. For the MS configuration, when working in transcritical conditions, the high-pressure is established by the back-pressure. The tunable parameters are the high-pressure and the subcooling degree in subcooler (SUB = T3 − T4). Both parameters are optimized to obtain the best performing conditions. When working in subcritical, high pressure is computed as saturation temperature of CO2 at the environment temperature plus a temperature difference in condenser of 5 K, to maintain the same reference level as in transcritical. The exit of the condenser is considered in saturation. Only the subcooling degree in the subcooler is free, it being optimized in the calculations. For the cascade configuration, the tunable variable is the temperature of the intermediate level, being the CO2 condensing temperature taken as reference and optimized in the calculations. In this case, the exit condition of CO2 of the cascade heat exchanger is considered in saturation. For both cycles, the lamination processes are assumed isenthalpic and pressure losses and heat transfer to the environment in the lines are neglected.
Regarding the secondary refrigerant, R1234yf is selected for the MS cycle and for the high-temperature cycle. This HFO is one of the new generation of refrigerants introduced to the market with the aim of substitute the R134, being an alternative with low GWP but light inflammable (A2L), that can perform as drop-in replacement. Aprea et al. [25] find out that this drop-in allows increasing the cooling capacity, being a refrigerant suitable for new plants and plants that are already working.
The overall efficiency of the compressor is also adjusted as a linear relation with the compression ratio, as detailed by Equation (6), in this case fitted from experimental data of a semi-hermetic compressor [26].
η G , R 1234 yf = 0.9721 0.0533 t R 1234 yf
The high-temperature cycle or dedicated mechanical subcooling cycle, is thermally linked to the CO2 cycle using two different approaches: when working as condenser in the cascade configuration, the evaporation temperature of R1234yf is considered to be 5 K below the CO2 condensing temperature [12], thus being optimized during the calculation. On the other hand, when this cycle operates as mechanical subcooler, its evaporation temperature is computed considering a thermal effectiveness of the subcooler of 60%, Equation (7), being this effectiveness the average value measured in [27]. This temperature is indirectly optimized by tuning of the optimum subcooling degree in the CO2 cycle.
T o , R 1234 yf , MS = T 3 SUB ε = T 3 T 3 T 4 ε
For this cycle, a degree of superheat in the evaporator of 5 K is chosen. The exit of the condenser is in saturation and the expansion process is isenthalpic. Also, pressure losses and heat transfer to the environment in pipes are neglected.
The relation between the refrigerant mass flow rates of both cycles is obtained through the energy balance in the subcooler/cascade HX as established by Equation (8) according to nomenclature of Figure 1.
m ˙ R 1234 yf m ˙ CO 2 = h 3 h 4 h a h b
Using relation (8), the main energy parameters can be expressed as a function of the refrigerant enthalpies and the overall efficiencies of the compressors. Equation (9) expresses the overall COP of the cycle combination as quotient between the cooling capacity of the CO2 cycle and the sum of power consumptions of both compressors. Equation (10) establishes the relation between the power consumption of the MS/cascade compressor regards the power consumption of the CO2 compressor, it being an indicative of the size of the auxiliary cycle.
COP = Q ˙ O P C , CO 2 + P C , R 1234 yf = h 1 h 4 h 2 , s h 1 η G , CO 2 + h 3 h 4 h a h b × h c , s h a η G , R 1234 yf
P C , R 1234 yf P C , CO 2 = ( h 3 h 4 ) × ( h c , s h a ) ( h a h b ) × ( h 2 , s h 1 ) × η G , CO 2 η G , R 1234 yf
All the thermophysical properties of the refrigerants have been calculated using Refprop database [28].

3. Results

This section establishes the optimum operating conditions of the CO2 refrigeration cycle with mechanical subcooling (Section 3.1) and of the cascade cycle using CO2 as low temperature fluid (Section 3.2) using the model detailed in Section 2. The evaluation was made considering environment temperatures from 15 to 40 °C and evaporating levels from 5 to −20 °C. No lower evaporating levels were analyzed because −20 °C corresponds to the lowest evaporating temperature at which the CO2 compressor used to build the correlations can be operated. For lower evaporating levels, two stage solutions should be considered.

3.1. Operating Conditions of the CO2 Cycle with Mechanical Subcooling

As mentioned, the operating parameters to be tuned to obtain the best performing conditions of the CO2 cycle with mechanical subcooling are the pressure at the gas-cooler (Phigh) and the degree of subcooling provided by the auxiliary system (SUB). To illustrate the behavior of this cycle, the dependence of the overall COP, Equation (9), versus the environment temperature and the subcooling degree for an evaporating level of 0 °C is presented in Figure 5. Data of Figure 5 are evaluated for the optimum gas-cooler pressures. For environment temperatures below 25 °C the best results are in subcritical operation and for warmer temperatures in transcritical. As it can be observed, for any environment temperature, an optimum degree of subcooling exists, maximizing the overall COP. Furthermore, it is observed that the subcooling degree increases when going to warmer temperatures.
Maximum COP for the considered range and the corresponding optimum subcooling degrees are detailed in Figure 6 and Figure 7, respectively, for all the considered range. As it can be observed in Figure 6, the transition between subcritical to transcritical operation occurs, from a theoretical energy point of view, at an environment temperature of 25.3 ± 0.2 °C. Since this temperature is commonly reached in any location, the plant must be designed to be able to operate in subcritical conditions when possible, since forcing it to operate in transcritical would result in reductions of COP. That means that the first CO2 heat exchanger must be sized as condenser, but it must be ready to operate also as gas-cooler. The trend is the same as in pure CO2 transcritical systems, as it can be observed in the work presented by Sanchez D. et al. [23]. Another important aspect is that the presence of the optimum subcooling degree disappears when temperature difference between TC and TH is high. It can be observed for the operation at −5 °C and below. It will be mentioned later, but the reason is that at a high temperature lift the MS cycle is overcome by the cascade solution.
Finally, the ratio between the power consumption of the auxiliary cycle (R1234yf) and the main compressor (CO2), Equation (10), are represented in percentage for the optimum operating conditions in Figure 8. For the considered range, the needed power consumption of the auxiliary compressor ranges from 4% at an evaporation of 5 °C and environment temperature of 15 °C to 21% approximately for 5 °C at 40 °C. The most important observation is that sizing the auxiliary compressor for high environment temperatures will cover the operation in transcritical and subcritical without problems.

3.2. Operating Conditions of the Cascade Cycle

For the cascade cycle, the parameter that must be optimized is the intermediate temperature level (TI), the condensing temperature of CO2 (TK,L) being considered in this case for its representation. As mentioned, exit of CO2 cascade condenser is in saturation, no subcooling is considered, because it provides lower efficiency results. Figure 9 presents the evolution of the overall COP of the cascade solution for an evaporation level of 0 °C for all the considered environment temperatures. Limits of variation of TK,L are any temperature over the evaporating pressure up to a condensing temperature 5 K below the environment temperature (if Tenv < 25.978 °C) or the critical temperature. In Figure 9 it becomes clear that an optimum TK,L temperature exists. No more emphasis is done because different authors studied it in detail [29,30]. COP values at the optimum TK,L are presented in Figure 10. In contrast to the COP evolutions of the MS cycle, it needs to be highlighted that the reduction of COP of cascade systems due to variations of the environment temperature is smoother, being these systems less sensitive to variations of environmental conditions, as previously mentioned by Llopis et al. [14]. Also, to compare the design of the cascade system, the ratio of the high-temperature and low-temperature power consumption are presented in Figure 11. In this case, the power consumption of the high-temperature compressor inside the evaluated range is of the same order of magnitude as that of the CO2 cycle. With a design of the plant as cascade, it could operate with the MS cycle but not the other way round.

4. Discussion of Results

The optimum operating conditions of both cycles were analyzed in Section 3. As mentioned, both refrigeration cycles respond to the same scheme of operation (Figure 1) and may be able to operate with one scheme or the other if some components of the plant are over-sized. However, in practice, only one design of the plant is implemented due to economic reasons, for example: if the plant is designed to be operated in both modes the cascade/subcooler heat exchanger must be sized as cascade heat exchanger, while if it were designed to be operated as MS cycle the subcooler would be size reduced. The same happens for the gas-cooler, a gas-cooler of a cascade system is smaller than that of the MS cycle. Furthermore, if optimum COP results of both solutions are compared (Figure 6 and Figure 10) it can be seen that the MS cycle offers the best results at low environment temperatures and the cascade at high temperatures. Thus, this section is devoted to compare the COP values offered by both solutions. First, the recommended operating range of each cycle is analyzed in terms of COP, and then the results are translated to the different climatic regions of Spain through the computation of the average annual COP. The objective is to obtain conclusions about which system would be more recommended for a given evaporating level in a given climatic region.

4.1. Recommended Operating Conditions

COP values offered by both cycle configurations are merged in Figure 12, where the COP value at each evaporating and environment level corresponds to the best performing system. As it can be observed, the cascade system gets over the MS solution at high environment temperatures and low evaporating levels. In fact, the environment temperature for a given evaporating level that defines the border of both systems is expressed by Equation (11), which was fitted from the results of the models. At environment temperatures above the value given by Equation (11), the cascade solution operates with highest COP. Also, the optimum modes of operation of the MS cycle are depicted in Figure 12. The operating conditions between an environment temperature of 25.3 °C and that defined by Equation (11) will be in transcritical conditions, whereas all lower environment levels the best performing cycle will be in subcritical. As it is observed in Figure 12, the environmental conditions at which the plant would be operated in transcritical are very narrow, which means that the correct design of the first CO2 heat exchanger would be as condenser. In an attempt to summarize all the results of Figure 12, the COP dependence of both cycles versus the temperature difference between the cold and hot sources, Equation (12), is presented in Figure 13. Data used in Figure 13 correspond to all the calculated points to represent Figure 12. It can be observed that the MS cycle offers highest COP values at reduced temperature lifts and the cascade the other way round. The limit is at a temperature lift of 28.5 K approximately. However, it is important to note that the difference between the COP values of the MS cycle regards the cascade are higher at low temperature lifts that the difference between them at high temperature lifts. Those COP differences will condition the operation of the system along different environment temperatures, therefore a climatic evaluation would be needed to compare both cycles. That is discussed in Section 4.2.
T env = 25.95 + 0.4 T o
T = T env T o
Although in Figure 12 it seems that a smooth transition between the MS and the cascade cycle would be possible, it will only happen when the cycle is sized to operate in both configurations. To illustrate this reasoning, the compressor’s displacements for the low and high temperature cycles for both configurations are presented in Figure 14. Those data correspond to the displacements for a refrigeration plant with 50 kW of cooling capacity designed for an environment temperature of 30 °C. It can be observed that the differences of the CO2 compressor are not much significant between both cycles’ solutions, but the compressor of the cascade cycle would be up to 300% higher than that needed for the MS cycle. If the plant is sized to be operated as MS cycle, its operation as cascade would not be possible because of the compressors, and, although not evaluated, because of the size of the subcooler and the gas-cooler.

4.2. Operation in Different Climate Conditions

As mentioned by Minetto et al. [31], the superiority of one refrigeration system regards another in terms of energy efficiency must be discussed with reference to the climatic conditions of the installation site and the characteristics of cooling profile. In agreement with them, and in order to obtain conclusions about the performance of the MS cycle configuration regards the cascade design, in this subsection an evaluation of the systems at different climate conditions is reported. In this case, a climatic evaluation was made using the BIN temperature methodology [32] with the Energy Plus meteorological data (https://energyplus.net/weather) for different locations in Spain. This methodology groups the number of annual hours in which a certain temperature was recorded, allowing an accurate representation of the annual climate.
In fact, the energy performance of the systems was evaluated for the twelve climatic regions of Spain [33], Table 1, covering cold, mild and warm climates, using 20 temperature BINs from −3 to 33 °C of dry bulb temperature. For the evaluation, two simplified cooling load profiles were considered. Representing air-conditioning (AC) applications, no cooling load was considered below 21 °C, a linear dependence on the cooling load from temperatures above 21 up to 29 °C and 100% from 29 °C on. For commercial applications a constant value of 50% of cooling load up to 23 °C, linear dependence from 23 to 31 °C and 100% from 31 ºC on. Cooling load profiles are detailed in Table 1.
Using the meteorological data of dry-bulb temperature, an averaged COP value for both cycle configurations was evaluated using Equation (13). Where COP (Tenv,i) is the COP of each system evaluated at the average temperature of the ‘i’ temperature BIN, NHi is the number of hours of operation inside the ‘i’ temperature BIN and FQi the cooling load fraction inside the ‘i’ temperature BIN.
COP ¯ = i = 1 nbin [ COP ( T env , i ) × NH i × FQ i ] i = 1 nbin ( NH i × FQ i )
Averaged COP values for both refrigeration systems, for the different climatic regions using the cooling load profiles detailed in Table 1, are summarized in Table 2. Regarding AC application (To = 5 °C), it can be seen that the MS cycle over performs the cascade configuration for all the climatic regions except for the D3, C3, C4 and B4, that are regions with high environment temperatures during summer, where both configuration perform similar. Regarding the general application, for evaporating temperatures from 0 to −20 °C, the MS cycle also presents highest performance for all the climatic regions up to an evaporating level of −10 °C. At −15 °C both solutions perform similar and for −20 °C the cascade solution is the best performing. The differences between both refrigeration systems for the different climate conditions and the different evaporating levels and cooling load profiles are represented in Figure 15 as percentage variation from the MS cycle COP values, according to Equation (14). Values of Equation (14) represent the average annual COP advantage of the MS cycle regard the cascade cycle. It can be observed that the MS cycle is recommended from an energy point of view for any evaporating level higher or equal to −10 °C, both systems similar perform at −15 °C and the cascade should be recommended for the temperature level of −20 °C.
COP   ( % ) = COP MS COP casc COP casc × 100
As previously mentioned, both refrigeration cycle designs could be implemented in a system if some of the components are oversized, mainly the high temperature compressor, subcooler and gas-cooler/condenser, although it is not commonly done. Nonetheless, if only one cycle of operation is selected, it is important to quantify what would be its overall performance regards a plant with possibility to operate as cascade or as MS cycle, that would be the plant that will offer the best average annual COP values. To quantify the differences of the individual systems, their average annual COP values according to Equation (13) were compared to the ones obtained by an ideal refrigeration system with COP values equal to the maximum COP values of the MS or the cascade system. Percentage annual COP deviations regards the ideal system are specified in Table 3 for the different Spanish climate regions, and represented for two representative cases in Figure 16, which correspond to the operation at −5 °C and −20 °C of evaporating temperature. As it can be observed, any individual system has reductions of annual COP values regards the optimum or best system, since in some hours of the year the other solution would be more performing. That occurs for all the climatic regions and evaporating levels except for the climatic region C1 with evaporating levels from 5 to −5 °C. In general, for all the climatic regions, the system that better performs is the MS cycle configuration, with annual deviations from the best system up to 5% at evaporating levels higher or equal than −15 °C. On the other side, if the considered evaporating level is −20 °C, the solution with less deviation from the ideal system is the cascade, however, it is important to note that the MS cycle will have deviations lower than 5% regards the ideal system for all the climatic regions except for the C4, B4, A3 and A4. That indicates that although the MS cycle does not reach the performance of the cascade solution at −20 °C, its average annual performance would be good enough for all the climatic conditions without large reductions of efficiency. This solution will avoid the over sizing of the plant, and thus, allow to operate with a lower cost plant.

5. Conclusions

This communication analyzes two modes of operation of a CO2-based two-stage refrigeration cycle with equivalent design that can be operated as cascade refrigeration system or as a CO2 refrigeration plant with dedicated mechanical subcooling system. Both schemes are being considered now to spread the use of CO2 in medium and warm regions of the planet for medium temperature applications.
Using relations of the overall efficiency of compressors, adjusted from experimental data of a semi-hermetic CO2 and a semi-hermetic R1234yf compressors, a simplified model of both cycles was developed. With the thermodynamic models, the optimum operating conditions of each refrigeration cycle, covering evaporating temperatures from −20 to 5 °C and environment temperatures from 15 to 40 °C, were determined. Then, by merging the COP values of each refrigeration solution, the external conditions at which each refrigeration solution is the best performing were established. Furthermore, the analysis was translated for the different climatic regions of Spain to compare the systems.
Regarding the CO2 refrigeration cycle with mechanical subcooling, it was concluded that the environment temperature that will limit the operation in subcritical or transcritical is 25.3 °C, thus the design of the gas-cooler would be always as condenser, since the region at which this system will operate in transcritical is very narrow. Furthermore, the optimum subcooling degree results higher at lowest evaporating levels and high environment levels. Nonetheless, the maximum ratio of power consumption of the mechanical subcooling compressor will not exceed from 21% of the power consumption of the CO2 compressor.
It was concluded that the cascade configuration using CO2 as low temperature refrigerant will have highest performance than the MS cycle when the temperature lift between the cold and heat sources is higher than 28.5 K. However, in this case the power consumption of the high-temperature cycle will be even higher than the power consumption of the CO2 rack.
The analysis was extended to the different climatic regions of Spain using a based temperature-BIN methodology. It was calculated that the MS cycle would offer highest energy efficiencies in overall-year operation than the cascade solution for evaporating levels below −15 °C, including the air-conditioning application. However, at the evaporating level of −20 °C the cascade solution will over perform the MS cycle. Also, the individual systems were compared to an ideal refrigeration cycle that could be operated as CO2 with mechanical subcooling or as cascade at any climatic condition, which is called the best system. The average annual COP of each individual system was compared with the best system. It was observed that the MS cycle will have annual reductions of efficiency up to 5% at evaporating levels higher or equal than −15 °C, and also reductions below 5% at the evaporating level of −20 °C except for 4 climatic regions of Spain.
As general conclusion of this work, it can be affirmed that if this cycle configuration is sized as cascade or as a single-stage cycle with mechanical subcooling, the configuration that will offer the best performing levels at the analyzed conditions would be the CO2 refrigeration cycle with mechanical subcooling.

Acknowledgments

The authors gratefully acknowledge the Spanish Ministry of Economy and Competitiveness (project ENE2014-53760-R.7) for financing this research work.

Author Contributions

R.L. suggested the idea and conceived the calculation models. R.L. and L.N.-A. carried out the simulations and analyzed the data; D.S. and R.C. checked the calculations. R.L. and L.N.-A. wrote the paper and J.C.-G. contributed to the correction of the paper.

Conflicts of Interest

The authors declare no conflict of interest.

Nomenclature

Casccascade cycle with CO2 as low temperature refrigerant
COPcoefficient of performance
FQcooling load fraction inside a temperature BIN
GWPGlobal warming potential
HXheat exchanger
hspecific enthalpy, kJ·kg−1
NHnumber of hours inside a temperature BIN
nbinnumber of temperature bins
MSCO2 cycle with mechanical subcooling
m ˙ mass flow rate, kg·s−1
Ppressure, bar
PCcompressor power consumption, kW
Q ˙ O cooling capacity, kW
SUBdegree of subcooling at the subcooler, K
Ttemperature, °C
tcompression ratio
TEWItotal equivalent warming impact
V ˙ G compressor displacement, m3·h−1
GREEK SYMBOLS
ηGoverall compressor efficiency
Δincrement
εheat exchanger efficiency
SUBSCRIPTS
CO2referring to CO2 cycle
critcritical point
envenvironment
gcgas-cooler
Hhot sink
highrefers to pressure at gas-cooler and subcooler or cascade heat exchanger
Iintermediate temperature level
Kcondensing level
Lcold source, low temperature cycle
MSreferring to the dedicated mechanical subcooling cycle
Oevaporating level
R1234yfreferring to the R1234yf cycle
satsaturation

References and Notes

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Figure 1. Schematic representation of cascade and CO2 with mechanical subcooling.
Figure 1. Schematic representation of cascade and CO2 with mechanical subcooling.
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Figure 2. Pressure-enthalpy diagram of mechanical subcooling (MS) cycle in subcritical conditions.
Figure 2. Pressure-enthalpy diagram of mechanical subcooling (MS) cycle in subcritical conditions.
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Figure 3. Pressure-enthalpy diagram of MS cycle in transcritical conditions.
Figure 3. Pressure-enthalpy diagram of MS cycle in transcritical conditions.
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Figure 4. Pressure-enthalpy diagram of the low temperature cycle (CO2) of the cascade.
Figure 4. Pressure-enthalpy diagram of the low temperature cycle (CO2) of the cascade.
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Figure 5. COP dependence on the subcooling degree of MS cycle. (To = 0 °C).
Figure 5. COP dependence on the subcooling degree of MS cycle. (To = 0 °C).
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Figure 6. COP of the MS cycle at optimum conditions.
Figure 6. COP of the MS cycle at optimum conditions.
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Figure 7. Optimum subcooling degrees of the MS cycle.
Figure 7. Optimum subcooling degrees of the MS cycle.
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Figure 8. Ratio of compressor’s power consumptions of the MS cycle.
Figure 8. Ratio of compressor’s power consumptions of the MS cycle.
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Figure 9. COP dependence on the low-temperature condensing temperature of cascade system. (To = 0 °C).
Figure 9. COP dependence on the low-temperature condensing temperature of cascade system. (To = 0 °C).
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Figure 10. COP of the cascade cycle at optimum conditions.
Figure 10. COP of the cascade cycle at optimum conditions.
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Figure 11. Ratio of compressor’s power consumptions of the cascade cycle.
Figure 11. Ratio of compressor’s power consumptions of the cascade cycle.
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Figure 12. Best performing cycle for the different operating conditions.
Figure 12. Best performing cycle for the different operating conditions.
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Figure 13. COP dependence on cold and hot sink temperature lift. MS and cascade cycles.
Figure 13. COP dependence on cold and hot sink temperature lift. MS and cascade cycles.
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Figure 14. Compressor’s displacements of a plant with 50 kW capacity at an environment at 30 °C.
Figure 14. Compressor’s displacements of a plant with 50 kW capacity at an environment at 30 °C.
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Figure 15. COP percentage variation of MS cycle vs. the cascade system at different climatic condition.
Figure 15. COP percentage variation of MS cycle vs. the cascade system at different climatic condition.
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Figure 16. Percentage average annual COP deviations of MS and cascade cycles regards the best system.
Figure 16. Percentage average annual COP deviations of MS and cascade cycles regards the best system.
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Table 1. Reference Spanish cities for the evaluation of the systems. Climatic regions, temperature BINs, hours of operation and cooling load profiles.
Table 1. Reference Spanish cities for the evaluation of the systems. Climatic regions, temperature BINs, hours of operation and cooling load profiles.
CityLeónPamplonaTeruelAlbaceteLa CoruñaBarcelonaGranadaToledoCastellón de la PlanaSevillaMálagaAlmería
Spanish climatic regionE1D1D2D3C1C2C3C4B3B4A3A4
Average annual temperature (°C)10.7912.2211.5513.5114.1415.3714.8815.5716.7418.2517.9918.54
Temperature BINAC cooling load (%)Commercial cooling load (%)Annual hours inside the temperature BIN
<−300.5000000000000
−3 to −100.5000000000000
−1 to 100.52480391000000000
1 to 300.5990341878633002481550000
3 to 500.5936962875847006926020000
5 to 700.5847111463381705408436631246200
7 to 900.5915819887571537909571876903754620
9 to 1100.581888473498116971057827663968846996810
11 to 1300.594384675160413648196689498137851055943
13 to 1500.582694485575615531063851572854789941933
15 to 1700.55527657336691556824814638943858884975
17 to 1900.549261552270595081779557890984110611094
19 to 2100.5244430430583673104661276497610081002851
21 to 230.20.53042742133394306133076158005819191068
23 to 250.40.63043042443060518461431552581738800
25 to 270.60.71552762732730337214275394523397488
27 to 290.80.81861862173040217243183338275426458
29 to 3110.90012412400273393186243279340
31 to 331100021700124155030400
>33110003100217248031000
Table 2. Averaged annual COP of cascade and MS cycles for Spanish Climate Regions.
Table 2. Averaged annual COP of cascade and MS cycles for Spanish Climate Regions.
Climatic RegionE1D1D2D3C1C2C3C4B3B4A3A4
Cascade cycle annual averaged COP
To = 5 °C (AC)3.743.723.573.414.303.793.333.333.663.343.633.63
To = 0 °C4.514.454.424.234.534.264.134.044.113.874.003.94
To = −5 °C3.753.703.683.543.773.563.463.393.453.263.373.32
To = −10 °C3.183.143.123.013.193.032.952.902.952.802.882.84
To = −15 °C2.732.702.692.602.742.612.552.512.542.422.492.46
To = −20 °C2.372.352.332.262.382.272.222.182.222.122.172.15
MS cycle annual averaged COP
To = 5 °C (AC)3.923.883.653.434.824.003.323.333.803.343.763.76
To = 0 °C5.655.525.485.145.675.164.974.814.894.494.684.56
To = −5 °C4.384.294.264.024.404.043.893.783.853.553.703.62
To = −10 °C3.503.443.413.233.523.253.143.063.112.893.002.94
To = −15 °C2.862.812.792.652.872.672.582.512.562.382.482.43
To = −20 °C2.362.322.302.192.372.212.132.082.121.982.062.02
Climatic regionE1D1D2D3C1C2C3C4B3B4A3A4
Cascade cycle annual averaged COP
To = 5 °C (AC)3.743.723.573.414.303.793.333.333.663.343.633.63
To = 0 °C4.514.454.424.234.534.264.134.044.113.874.003.94
To = −5 °C3.753.703.683.543.773.563.463.393.453.263.373.32
To = −10 °C3.183.143.123.013.193.032.952.902.952.802.882.84
To = −15 °C2.732.702.692.602.742.612.552.512.542.422.492.46
To = −20 °C2.372.352.332.262.382.272.222.182.222.122.172.15
MS cycle annual averaged COP
To = 5 °C (AC)3.923.883.653.434.824.003.323.333.803.343.763.76
To = 0 °C5.655.525.485.145.675.164.974.814.894.494.684.56
To = −5 °C4.384.294.264.024.404.043.893.783.853.553.703.62
To = −10 °C3.503.443.413.233.523.253.143.063.112.893.002.94
To = −15 °C2.862.812.792.652.872.672.582.512.562.382.482.43
To = −20 °C2.362.322.302.192.372.212.132.082.121.982.062.02
Table 3. Percentage deviation of annual COP values of MS and cascade cycles regards the best system.
Table 3. Percentage deviation of annual COP values of MS and cascade cycles regards the best system.
Climatic RegionE1D1D2D3C1C2C3C4B3B4A3A4
Cascade cycle
To = 5 °C (AC)−4.7−4.3−3.1−2.6−10.9−5.2−2.5−2.8−4.3−2.7−4.2−4.1
To = 0 °C−20.2−19.6−19.6−18.2−20.0−17.5−17.4−16.6−16.2−14.6−14.9−14.2
To = −5 °C−14.6−14.1−14.1−12.9−14.3−12.3−12.3−11.6−11.2−10.0−10.1−9.5
To = −10 °C−9.7−9.3−9.3−8.4−9.3−7.8−7.9−7.4−6.9−6.1−6.2−5.7
To = −15 °C−5.5−5.2−5.2−4.6−5.0−4.1−4.2−4.0−3.6−3.1−3.1−2.8
To = −20 °C−1.4−1.3−1.3−1.1−1.1−1.0−1.0−1.0−0.8−0.7−0.7−0.6
MS cycle
To = 5 °C (AC)−0.2−0.2−0.8−2.00.0−0.1−2.7−2.8−0.7−2.7−0.8−0.8
To = 0 °C−0.1−0.1−0.2−0.50.0−0.1−0.7−0.9−0.4−1.1−0.5−0.6
To = −5 °C−0.3−0.3−0.5−1.00.0−0.5−1.3−1.5−0.8−1.9−1.1−1.3
To = −10 °C−0.6−0.7−0.9−1.6−0.1−1.0−2.0−2.4−1.6−3.1−2.1−2.4
To = −15 °C−1.1−1.3−1.5−2.5−0.4−2.0−3.1−3.7−2.9−4.7−3.6−4.1
To = −20 °C−1.9−2.4−2.6−4.0−1.5−3.8−4.8−5.6−5.0−7.1−6.1−6.7

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MDPI and ACS Style

Nebot-Andrés, L.; Llopis, R.; Sánchez, D.; Catalán-Gil, J.; Cabello, R. CO2 with Mechanical Subcooling vs. CO2 Cascade Cycles for Medium Temperature Commercial Refrigeration Applications Thermodynamic Analysis. Appl. Sci. 2017, 7, 955. https://doi.org/10.3390/app7090955

AMA Style

Nebot-Andrés L, Llopis R, Sánchez D, Catalán-Gil J, Cabello R. CO2 with Mechanical Subcooling vs. CO2 Cascade Cycles for Medium Temperature Commercial Refrigeration Applications Thermodynamic Analysis. Applied Sciences. 2017; 7(9):955. https://doi.org/10.3390/app7090955

Chicago/Turabian Style

Nebot-Andrés, Laura, Rodrigo Llopis, Daniel Sánchez, Jesús Catalán-Gil, and Ramón Cabello. 2017. "CO2 with Mechanical Subcooling vs. CO2 Cascade Cycles for Medium Temperature Commercial Refrigeration Applications Thermodynamic Analysis" Applied Sciences 7, no. 9: 955. https://doi.org/10.3390/app7090955

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