Document ExNkDaxaeQ7pQOJeEE7wnOa3N

122 CHAPTER 6 1952 Guide EFFECTIVE TEMPERATURE INDEX AND COMFORT ZONES There is no precise physiologic observation by which comfort can be evaluated.; Mean skin temperature offers some promise. The zone of' thermal neutrality differs with clothing, season, activity, and all the other faictors controlling heat production (Table 4). The comfort zone is very similar to the zone of thermal neutrality. Sensations of warmth , or cold depend not only on the temperature of the surrounding air as registered by a dry-bulb thermometer, but also upon the temperature indicated by a wet-bulb thermometer, upon air movement, and upon radiation effects. Dry air at a relatively high tem perature may feel cooler than air of lower temperature with a high moisture content. Air motion makes any moderate condition feel cooler. Radia tion to cold or from warm surfaces is another important factor under certain conditions affecting the comfort reaction of the individual. Fig. 7. Evaporative Heat and Moistube Loss fbom the Human Bodt in Rela tion to Dby-Bulb Tempebatube fob Still Aib Conditions* 14 * Loo. Cit. See footnote a. Fig. 5. Combinations of temperature, humidity, and air movement which in duce the same feeling of warmth are called thermo-equivalent condi tions. A series of studies22 at the A.S.H.V.E. Research Laboratory, estab lished the equivalent conditions for practical use. This scale of thermoequivalent conditions not only indicates the sensation of. warmth, but also to a considerable degree determines the physiological effects on the body induced by heat or cold. For this reason, it is called the effective temperature scale or index, and it denotes sensory heat level. Effective temperature is an empirically determined index of the degree of warmth perceived on exposure to different combinations of temperature, humidity, and air movement. It was determined by trained subjects who compared the relative warmth of various air conditions in two adjoining conditioned rooms by passing back and forth from one room to the other. The numerical value of the index for any given air conditions is fixed by the temperature of slowly moving (15 to 25 fpm air movement) saturated ' Physiological Principles T23 .air which induces a like sensation of warmth or cold. Thus, any air con dition has an effective temperature of 60 deg when it induces a: sensa tion of warmth like that experienced in slowly moving air at 60 F saturated with moisture. The effective temperature index cannot be measureddirectly, but is determined from dry- and wet-bulb temperatures and air motion observations by reference to an Effective Temperature Chart (see Figs. 8, 9, and 10) or tables. Fig. 8 gives the effective temperature for any combination of dry- .and wet-bulb temperatures for still air (15 to 25 fpm) conditions. Charts similar to Fig. 8 for air velocities of 3b0 and 500 fpm have been presented in some of the earlier editions, of the Guide. Fig. 9 is another form of effective temperature chart embodying all three variables: dry-bulb and wet-bulb temperatures, and air velocity. Table 4. Comparison of Comfobt Ranges With Zone of Thermal Neutrality Investigators Effective Temperature Operative Temp Optimum Line Range Range Remarks Comfort Zone Houghten and Yaglou. 66 63-71 Yaglou and Drinker... 71 Yaglou.......................... 72.5 Keeton et al................. 75 66-75 66-82 74-76 Winter non-basal; at rest, nor mally clothed. Men and women. Summer non-basal: at rest and normally clothed. Men. Entire year; non-basal; at rest. and stripped to waist. Men. Entire year;basal,nude.Steady state. (9 hr exposure). Men and women. Zone of Thermal Neutrality DuBois and Hardy___ Winslow, Herrington and Gagge......... 75 71.8 73.2-76.9 64.8-76.0 Basal; nude; men. . Basal; clothed; mien. 84.0-87.8 Non-basal; at rest; nude: men.' 74 -84 Non-basal ;at rest ;clothed;men. - As stated previously, effective temperature is an index of the degree of warmth experienced by the body. An effective temperature line is, there fore, a fine defining the various combinations of conditions which will induce like sensations of warmth. It does not necessarily follow that like sensations of comfort will also be experienced along the entire length of an effective temperature line. Some degree of discomfort is likely to be experienced at very high or very low relative humidities, regardless of the effective temperature. It has also been found that the optimum effective temperature varies with the season, and is lower in winter than in summer. Tests14 made at the A.S.H.V.E. Research Laboratory in very hot conditions, with subjects doing light work, were in very close agreement with the effective temperature chart. Other work20 under similar environmental conditions, but with subjects walking 3 mph and carrying 20 lb packs, indicated that the effective temperature lines should be more