ASHRAE OR-16-C016-2016 Comprehensive Assessment of Centrifugal Chillers Using Next Generation Refrigerant R1233zd(E).pdf
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1、Steve Kujak is the director-next generation refrigerant research for Ingersoll Rand, La Crosse, WI. Kenneth Schultz, PhD, is a engineer- next generation refrigerant research for Ingersoll Rand, La Crosse, WI. Julie Majurin is chemist- next generation refrigerant for Ingersoll Rand, La Crosse, WI. Co
2、mprehensive Assessment of Centrifugal Chillers Using Next Generation Refrigerant R1233zd(E) Steve Kujak Kenneth Schultz, PHD Julie Majurin Member ASHRAE Member ASHRAE Member ASHRAE ABSTRACT A new olefin refrigerant, R1233zd(E), has been identified for use in HVAC chillers. R1233zd(E) is being consid
3、ered for a number of applications including use as, but not limited to, a solvent, a foam blowing agent, a refrigerant in large centrifugal chillers, and a refrigerant in heat recovery equipment. R1233zd(E) provides specific environmental and safety features of interest including very short atmosphe
4、ric life (26 days), no impact to stratospheric ozone, ultra-low Global Warming Potential (GWP of 1), no measured secondary adverse environmental impacts (such as increases in ground level ozone or trifluoroacetic acid (TFA), low toxicity, and non-flammability. This paper will provide an overall asse
5、ssment of applying this new olefin refrigerant in centrifugal water cooled chillers. System performance characteristics will be compared to a number of refrigerants including R134a, R1234ze(E), R245fa, and R123. LCCP emission profiles will be compared. Reliability indicators, such as material compat
6、ibility and chemical stability, will be provided INTRODUCTION New regulatory policies and regulations to restrict and lower the direct GWP impact of F-gases have recently been proposed and adopted by some countries. These regulations have spurred both the technology development of alternative lower
7、GWP F-gas chemistries and renewed consideration of so-called “natural” refrigerants, such as water (R718), ammonia (R717), carbon dioxide (R744), and hydrocarbons. A new olefin refrigerant, R1233zd(E) or trans-1-chloro-3,3,3-trifluoro-1-propene, is under consideration as a refrigerant which meets th
8、ese new regulatory requirements. R1233zd(E) is a single component refrigerant that ASHRAE Standard 34 has listed as Class A1 (lower toxicity/non-flammable). This makes R1233zd(E) compatible with existing application standards and building codes and therefore allows its immediate use. As shown in Fig
9、ure 1 and Figure 2, R1233zd(E) does not possess the thermodynamic and physical properties to directly replace existing HCFC or HFC refrigerants currently used in HVACR equipment, like R123 or R245fa. The operating pressures of R1233zd(E) are 30% to 45% higher than R123 for a given temperature. R1233
10、zd(E) produces 39% more capacity than R123 for a given compressor volumetric displacement when operating at 44F (6.7C) evaporator saturation temperature and 100F (37.8C) condenser saturation temperature. The thermodynamic efficiency of R1233zd(E) falls short of R123 by less than 1% at these conditio
11、ns. Use of R1233zd(E) represents a new design centerline and therefore requires new equipment designs for optimal performance. R1233zd(E)s higher operating pressures require equipment designs to meet ASME or other pressure vessel codes. A newly designed centrifugal chiller, using R1233zd(E) has been
12、 developed and is being offered in the market place as a future low GWP replacement option for R123, R245fa and R134a centrifugal chiller applications. Figure 1 Pressure-enthalpy comparison for R1233zd(E), R245fa, and R123 Figure 2 Temperature-entropy comparison for R1233zd(E), R245fa, and R123 ASSE
13、SSMENT OF R1233ZD(E) IN CENTRIFUGAL CHILLER PRODUCTS Environmental and Safety Environmental: An assessment of the environmental impact is needed prior to widespread use of any new chemical or a specific class of chemicals. A number of environmental factors need to be considered, such as climate chan
14、ge, tropospheric ozone formation, formation of noxious environmental degradation products, and stratospheric ozone loss. The unifying chemical feature in olefin (unsaturated) HFCs or olefin HCFCs is the presence of a carbon-carbon double bond that limits atmospheric lifetime as compared to saturated
15、 compounds. As a result, the ability of these molecules to contribute to photochemical ozone creation potential (POCP), direct GWP, and ozone depletion potential (ODP) is severely limited in nature. These olefins have short atmospheric lifetimes, measured in days to weeks, which results in negligibl
16、e POCPs, GWPs, and ODPs. A recently published article (Wallington et al., 2014) summarizes the atmospheric chemistry and features of a range of short-chain haloolefins, including R1233zd(E), compared to a wide range of currently used refrigerants. R1233zd(E) is documented to have an atmospheric life
17、time of 26 days, a GWP of 1, a POCP of 3.9, no significant reports of environmental breakdown products of concern, and an ODP near zero. In comparison, saturated HFCs have GWPs of 858 for R245fa, 1300 for R134a, and 79 for R123. Photochemical ozone creation potential is defined as the additional ozo
18、ne formed in a multi-day modelling relative to adding the same mass of ethene to simulate the impact on local ozone air quality. The POCP scale is relative to a reference substance, ethene, with a POCP defined as 100. Haloolefins have POCPs which are larger than halocarbons but much smaller than tho
19、se of alkenes. Haloolefins have POCPs which lie between methane (0.6) and ethane (12.3) which both oxidize sufficiently slowly so as not to contribute to local air quality issues and are exempt from air quality regulations. R1233zd(E)s POCP of 3.9 indicates that it should not contribute to local air
20、 quality issues and as such the US EPA has ruled that R1233zd(E) is not a local area quality target pollutant. Another potential source of environmental concern for haloolefins is the potential for TFA formation. TFA formation has been studied extensively and the World Meteorological Organization co
21、ncluded in 2011 that TFA from degradation of HCFCs and HFCs will not result in environmental concentrations capable of significant ecosystem damage. The same is applicable and documented for haloolefins. In the case of R1233zd(E), chlorine-substituted oxidization products are expected, HCOCl, and no
22、 TFA formation is expected to be produced in the environment. HCOCl is expected to be incorporated in rain, cloud, and fog water, followed by hydrolysis and removal by wet deposition within days, followed by hydrolysis to produce formic acid. Formic acid is a pervasive component of the environment a
23、nd is of no concern. Sulbaek Andersen et al. (2012) proposed an alternate atmospheric fate mechanism, but the proposed route did not show a high likelihood of TFA as a possible degradation product. Chlorine- and bromine-containing haloolefins could potentially contribute to stratospheric ozone, alth
24、ough it is negligible in most cases because of the haloolefins short atmospheric lifetimes which are measured in days, rather than years as in the case of saturated halocarbons. Patten and Wuebbles (2010) concluded that at the concentrations likely to be emitted by R1233zd(E), which has an ODP of 0.
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