ASHRAE 4710-2004 Climatic Impacts on Heating Seasonal Performance Factor (HSPF) and Seasonal Energy Efficiency Ratio (SEER) for Air-Source Heat Pumps《气候对空气源热泵的供暖季节性能系数(HSPF)和季节能效比(.pdf
《ASHRAE 4710-2004 Climatic Impacts on Heating Seasonal Performance Factor (HSPF) and Seasonal Energy Efficiency Ratio (SEER) for Air-Source Heat Pumps《气候对空气源热泵的供暖季节性能系数(HSPF)和季节能效比(.pdf》由会员分享,可在线阅读,更多相关《ASHRAE 4710-2004 Climatic Impacts on Heating Seasonal Performance Factor (HSPF) and Seasonal Energy Efficiency Ratio (SEER) for Air-Source Heat Pumps《气候对空气源热泵的供暖季节性能系数(HSPF)和季节能效比(.pdf(11页珍藏版)》请在麦多课文档分享上搜索。
1、471 O - Climatic Impacts on Heating Seasonal Performance Factor (HSPF) and Seasonal Energy Efficiency Ratio (SEER) for Air-Source Heat Pumps Danny S. Parker Associate Member ASHRAE Matthew Lombardi Philip Fairey Member ASHRAE Bruce Wilcox Member ASHRAE ABSTRACT Within ratingprocedures established by
2、 the US. Depart- ment of EnerD, benchmarks have been established for the comparative performance of heat pumps and air conditioners. The heating seasonal performance factor (HSPF) and seasonal energy eficiency ratio (SEER) index heating and cooling season performance, respectively. Although theproce
3、- dures result in a highly desirable standard metric, the climate- related limitations of the published values must be under- stood-particularly when attempting to extend performance prediction across regions. This paper describes evaluation of climate-related variation of heat pump and air-conditio
4、ner performance. Operating seasonal eficiencies are statistically related to location-specijic winter andsummer design temper- atures and manilfacturers equipment ratings. Implications are discussed. HEAT PUMPS Residential air-source heat pumps are an increasingly popular heating system in the South
5、ern United States. Over 10 million heat pumps (HPs) are currently in use (EIA 200 I). The practical efficiency that air-source heat pumps achieve is a coefficient of performance (COP) of 2.0-3.0. To rate heat pumps in a standard fashion, a heating seasonal performance factor (HSPF) is determined tha
6、t takes into account operation under varying outdoor temperatures as well as part-load impacts (effects of running short cycles under mild condi- tions). HSPF is rendered as BtdWh so that typical HSPFs are nominally on the order of 6.8-10 BtdWh (the dimensionless value of the minimum HSPF of 6.8 is
7、COP = 1.99). HSPF is defined according to test procedures as promulgated by AM in its Standard 210/240, as well as ASHRAE Standard 116 and the DOE Test Procedure in 10 CFR, Part 430, Appendix M (AM 2003). The rateanameplate HSPF from AR1 2 1 O240 is based on the temperature in climate region IV (200
8、0-2500 heating load hours) and the minimum design heating requirement (DHR) that is a function of machine heating capacity. This selection is favorable to limit the contribution of resistance heating because it typically results in a balance point in the 17F to 25F range. Although published HSPFs ar
9、e linked to this climate, and specifically to 2080 heating load hours, it was never envisioned that this single value could be used to gener- ically predict performance for all climate locations. Given the severity of winter in much of the continental United States and the sensitivity of heat pumps
10、to the outdoor temperature, site- specific performance must vary significantly with climate. Although temperature bin data and procedures within AR1 2101240 are available to compute performance in other climatic regions (Sections A.6.2.4 and A.6.2.5 of that stan- dard), the published data available
11、for all heat pump and air- conditioning units is that of climate zone IV. Thus, although a method is available to compute HSPF and SEER in other regions, this is not done, and the information is unavailable to consumers and others without access to data on machine performance at the specific test po
12、ints. The AR1 directory of certified unitary air-source heat pumps does provide rudimentary information on heating performance for all six heating regions. The directory includes a table entitled “Heating Cost Factor,” which provides infor- mation that can be used to adjust the annual energy cost ba
13、sed on the FTC-labeled amount for Region IV for each unit that is listed to annual energy costs for the other five regions. Unfor- tunately, as will be shown within this paper, the climate clas- sifications within the ARI directorys map leave much to be Philip Fairey is director, Danny S. Parker is
14、principal research scientist, and Matthew Lombardi is a research assistant at the Florida Solar Energy Center, Cocoa, Fla. Bruce Wilcox is principal at Berkeley Solar Group, Bcrkeley, Calif. 1 78 02004 ASHRAE. desired relative to accuracy in capturing winter severity. Also, the methods used to estim
15、ate the heating system performance within the procedure itself tends to be optimistic relative to typical operating conditions, setpoints, etc. Moreover, the six climatic zones available within the ARI 21 O240 method are necessarily coarse with respect to climate. For instance, ARI Climate Zone 2 in
16、cludes the widely varying climates of Phoenix (1 125 heating degree-days HDD/4189 cooling degree-days CDD, 99% Design Temp = 37“F, 1% Design Temp = 108F) and Ft. Worth, Texas (2370 HDD/ 2568 CDD, 99% Design Temp =24“F, I% Design Temp = 98“F). Although it was never intended that the Region IV HSPF an
17、d SEER would be used to estimate energy use across climates, these values have indeed been used for these purposes within software and calculation procedures (for instance, see ACCA 19861). Particularly for heat pumps, this can lead to erroneous conclusions on their relative merit as compared with n
18、on-heat pump alternatives across climates. Given these limitations, it is highly desirable to have some means to interpret the seasonal performance of heat pumps and air conditioners across locations. Beyond the climatic variation, there are other reasons that typical performance may not reach that
19、suggested by the AM standard. Within the 2 10/240 procedures, a correction factor, C, with a value of 0.77, is used to reduce the heating loads on the heat pump. The justification for the C-factor is that it more closely matches measured building loads when used with degree-day or bin weather data b
20、ased on a 65F setpoint (Harris et al. 1965). The reason the building loads are lower is due to heat gains, such as solar gains and internal gains, which cause a balance point lower than 65F. A better method to account for this is to use a lower balance point rather than a multiplier since the effect
21、 at varying outdoor temperatures can be very different from the C= 0.77 default. For instance, tests performed by the Electric Power Research Institute in the late 1970s found that C could vary from 1.2 to 0.4 in actual resi- dences (EPRI 1980). As a result, the method of estimation has fallen out o
22、f favor, as evidenced by its disappearance from the ASHRAE Handbook-Fundamentals after 1985. Another problem associated with the AR1 procedure is that it implicitly assumes a 65F interior heating setpoint by using bin data at 65F along with C to reduce those loads. In our analysis, we desired to use
23、 the more commonly preferred 68F interior heating setpoint. This will have the effect of increasing the building load, which, in turn, will tend to reduce the simulated HSPF as compared with the assumption of 65“F, as in ARI 210/240. Backup resistance use will also increase. At an outdoor temperatur
24、e of 45“F, this difference could impose a 30% increase in loads after internal and solar gains are taken into account. I. Similarly, the mild climate of Los Angeles falls into the same clas- sification as Atlanta, Georgia, and St. louis, Missouri, whereas each of these has widely varying weather. Co
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