Investigating claims that a clothed person's mass loss does not always represent their evaporative heat loss (EVAP), a thermal manikin study was performed measuring heat balance components in more detail than human studies would permit. Using clothing with different levels of vapor permeability and measuring heat losses from skin controlled at 34°C in ambient temperatures of 10, 20, and 34°C with constant vapor pressure (1 kPa), additional heat losses from wet skin compared with dry skin were analyzed. EVAP based on mass loss ( Emass) measurement and direct measurement of the extra heat loss by the manikin due to wet skin ( Eapp) were compared. A clear discrepancy was observed. Emass overestimated Eapp in warm environments, and both under and overestimations were observed in cool environments, depending on the clothing vapor permeability. At 34°C, apparent latent heat (λapp) of pure evaporative cooling was lower than the physical value (λ; 2,430 J/g) and reduced with increasing vapor resistance up to 45%. At lower temperatures, λapp increases due to additional skin heat loss via evaporation of moisture that condenses inside the clothing, analogous to a heat pipe. For impermeable clothing, λapp even exceeds λ by four times that value at 10°C. These findings demonstrate that the traditional way of calculating evaporative heat loss of a clothed person can lead to substantial errors, especially for clothing with low permeability, which can be positive or negative, depending on the climate and clothing type. The model presented explains human subject data on EVAP that previously seemed contradictive.
MEASUREMENT OF LOCAL EVAPORATIVE RESISTANCE OF TYPICAL CLOTHING ENSEMBLE USING A SWEATING THERMAL MANIKIN