Document QgQyK0bQXEo4okeZeeZ5akdj7

126 CHAPTER 6 -1955 Guides measurable degree the optimum conditions for comfort previously in dicated. Since the mean radiant temperature of a space is affected by cold walls and windows, as well as by the warm surfaces of heating units placed within the room or imbedded in the walls, these factors must be 90 AIR MOVEMENT OR TURBULENCE 15 TO 25 FT PER MIN physiological Principles 127 Many field studies23 have been made to determine the optimum indoor effective temperature for both winter and summer in several metropolitan districts of the United States and Canada, in cooperation with the manage ments of offices employing large numbers of workers (Fig. 11). On the whole, women of all age groups studied prefer an effective temperature for comfort, 1.0 deg higher than men. All men and women over 40 years of age prefer a temperature 1 deg ET higher than that desired by persons below this age. The persons serving in all of these studies were repre sentative of office workers dressed for air conditioned spaces in the summer season, and engaged in the customary office activity. 80 lil N 40 50 70 80 DRY BULB TEMPERATURE F 90 100 Fig. 10. A.S.H.V.E. Comfort Chart for Still Air* * Note.--Both summer and winter comfort lines apply to inhabitants of the United States only. Applies-.-:; tion of winter comfort line is further limited to rooms heated by central systems of the convection type. Thein line does not apply to rooms heated by radiant methods. Application of summer oomfort line is limited to** homes, offices and the like, where the occupants become fully adapted to the artificial air conditions. Tbe?^ line does not apply to theaters, department stores, and the like where the exposure is less than 3 hours. The|r summer comfort line shown pertains to Pittsburgh and to other cities in the northern portion of the United]?- States and Southern Canada, and at elevations not in excess of 1000 ft above sea level. An increase of one deg*-; ET should be made approximately per 5 deg reduction in north latitude. -Ig b Dotted portion of winter comfort line was extrapolated beyond test data. ' `f compensated. Likewise, in densely occupied spaces, such as classrooms, j theaters and auditoriums, temperatures somewhat lower than those;indicated by the. comfort line may be desirable because of counter-;; radiation between the bodies of occupants in close proximity to each other s Such radiation will also elevate the mean radiant temperature of the room.'. Pig. 11. Relation Between Effective Temperature and Percentage Observa tions Indicating Comfort On the basis of present knowledge,; for different geographical regions and age groups, the most popular temperature varies from a low of 66 ET in winter to a high of 73 ET in summer. The spread for summer comfort is 69 to 73 ET. A- spread of 3 deg in the optimum effective temperature for summer cooling is ascribed to geographical location. However, variations in sensa tion of comfort among individuals may be greater for any given location than variations due to a difference in geographical location. The available information indicates that changes in. weather conditions over a period of a few days do not alter the optimum indoor temperature. Sudden chilling (shock) of persons entering a cooled and air conditioned Pace during the summer months, may at times be important. It is due 10 the rapid evaporation of perspiration which accumulated on the skin ^d in the clothing during previous subjection to hot and humid outside c?n<fitins. While studies26 have shown that for healthy individuals this TM is not harmful, under some conditions it may be unpleasant or