ASHRAE NA-04-2-5-2004 Thermal Comfort in the Climatic Conditions of Southern Italy《在意大利南部的气候条件下的热舒适性》.pdf
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1、NA-04-2-5 Thermal Comfort in the Climatic Conditions of Southern Italy Ida Fato Francesco Martellotta, Ph.D. Cecilia Chiancarella ABSTRACT This paper presents the results of four thermal comfort surveys conducted in naturally ventilated and air-conditioned buildings located in Bari, in southern Ital
2、y, during winter and summer seasons. The buildings were of dierent types, includ- ing ofices, lecture rooms, and library reading rooms. The sample of subjects consisted mostly of students. A total of 20 rooms were analyzed by measuring indoor climatic parame- ters. During the measurements, the subje
3、cts located near the probes were asked top11 in a questionnaire to rate the thermal environment ut that moment. A total of 1840 valid question- naires were collected during the four suwqs. Clothing insu- lation levels were 0.45 CIO in summer and 0.90 clo in wintev. Metabolic rate was assumed equal t
4、o 1.2 met. Thermal neutral- ity, according to the ASHRAE seven-point scale, occurred at 24.4“C and 26.3“C in summer and at 20.7“C and 20.6“C in winter, respectively in naturally ventilated (Nv) and air-condi- tioned (AC) buildings. Preferred temperature, based on the Mclntyre preference scale, was c
5、ooler in summer (24.2“C and 25.6“C in NV and AC buildings, respectively) and warmer in winter (23.1“C and 21.2“C in NV and AC buildings, respec- tively). Thermal acceptability was investigated by means of all the available scales, showing that the indirect estimation of acceptability (based on the t
6、hree central categories of the ASHRAE scale) onlyprovidespartial information about occu- pants conditions. Finally, the whole set of data was analyzed in order to propose an adaptive algorithm for this climaticzone. The resulting equation fl, = 17.82 + 0.315 Td, where T, is the comfort temperature a
7、nd T, is the running mean outdoor air temperature, proved to be in good agreement with other studies. INTRODUCTION Many thermal comfort surveys have been carried out in different parts ofthe world, and a database including a selected sample of these is currently available on-line (De Dear 1998). The
8、 spread of field studies is mostly due to the development of laboratory-grade field instruments and to an enhanced set of protocols, which make comfort data obtained in the field as rigorous as their climate chamber counterparts. in addition, chamber research tended to simplifi comfort models, negle
9、ct- ing many factors (such as expectations and adaptation) that are now fully recognized as a part of the problem. Most of the research is aimed at investigating how subjects living in different climatic zones react to their thermal environment. Some research has been explicitly commis- sioned by AS
10、HRAE in order to have a set of state-of-the-art, fully comparable field experiments across different climatic zones, including: temperate (Schiller et al. 1988), hot-humid (de Dear and Fountain 1994), cold (Donnini et al. 1996), and hot-arid (Cena and de Dear 1999). However, most of the research is
11、represented by independent studies carried out in thermally critical climatic zones, such as tropical and subtrop- ical (Busch 1990; Chan et al. 1998; Kwok 1998; Nicol et al. 1999; Wong and Khoo 2002; Kwok and Chungyoon 2003). Another important subject of investigation is how well Fangers comfort eq
12、uation, on which both IS0 7730 (1994) and current revisions to ASHRAE Standard 55 (1992) are based, works in real environments. In fact, several papers have pointed out significant discrepancies between rational indices and actual comfort ratings in both naturally ventilated build- ings and air-cond
13、itioned ones (de Dear and Aulicems 1985; Humphreys and Nicol 2002). The origin of the discrepancies may be found in biases in all the contributing variables I. Fato is an associate professor, E Martellotta is an assistant professor, and C. Chiancarella is a Ph.D. student in the Dipartimento di Fisic
14、a Tecnica, Politecnico di Bari, Italy. 578 Q2004 ASHRAE. (Humphreys and Nicol 2002) or, as suggested by Fanger and Toftum (2002), in different “expectations” of the people. A further argument ofresearch is the observation that, due to its inaccuracy, the PMV model is no better at predicting the comf
15、ort vote than simpler equations based on regression anal- yses using temperature alone as the independent variable. According to Nicol and Humphreys, this effect could be the result of a feedback between the comfort of the subjects and their behavior so that they “adapted” to the climatic conditions
16、 in which the field study was conducted (Nicol and Humphreys 2002). Important evidence that supports this adaptive approach is the good performance of the outdoor temperature as a predictor of the comfort temperature. In fact, variables such as clothing, posture, use of building controls, and meta-
17、bolic rate all depend on outdoor temperature. The feedback between climate, and these actions explain why only the latter need be considered in real situations in real buildings. The present paper provides a comprehensive analysis of the results of four transverse field studies carried out in Bari (
18、in southern Italy) and partly presented elsewhere (Conte and Fato 2000; Fato and Chiancarella 2003). The collected data have been used to investigate the effects of indoor climate on thermal perception, the relation between different scales, and the possibility of developing an adaptive algorithm to
19、 predict comfort temperature. THE THERMAL COMFORT SURVEYS Climatic Environment The thermal comfort surveys were carried out in Bari, in Apulia, in southern Italy. The city is located on the Adnatic Sea at a latitude of 41 O 8 N, in a large and homogeneous rain- fall region including the entire easte
20、rn Mediterranean (Tuni- sia, Sicily, Greece, Asia Minor, and the Black Sea region, the Levantine and Egyptian coasts as far as Cyrenaica) character- ized by rainfall from September to March (Littmann 2000; Petrarca et al. 1999). The rainfall is much lower than that observed in the northern part of I
21、taly (more influenced by the continental climate) and is mostly due to air mass movements caused by southern winds. During the spring, there are frequent day-to-day thermal variations due to the different origins of the air mass (from the Balkan peninsula and north- ern Europe or from the African re
22、gion). During the summer, the rainfall is negligible and the temperatures are quite stable with peaks due to southern winds. During the winter, the weather is quite unstable, with frequent alternation of cloudy and rainy days with sunny, but equally cold, days. According to the meteorological data b
23、ased on ten-year statistics (Petrarca et al. 1999), the range of daily mean temperatures in the winter season varies from 8.7”C to 10.9”C, with the lowest temperature observed in January. In summer, the mean temperatures vary from 21.4”C to 24.3OC, with the highest temperature observed in August (wi
24、th maximum temperatures up to 36C). The relative humidity varies from 60% to 75% in winter and from 50% to 70% in summer. The thermal comfort surveys were carried out in summer 1995 (S95), winter 1996 (W96), summer 1999 (S99), and winter 2000 (WOO). Sample of Buildings Five different university buil
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