Bell E F, Gray J C, Weinstein M R, Oh W
J Pediatr. 1980 Mar;96(3 Pt 1):452-9. doi: 10.1016/s0022-3476(80)80697-4.
To define the neutral environmental temperature and assess the effects of deviation from that temperature on insensible water loss and heat balance, 12 premature infants were studied in a conventional incubator at four different predetermined ambient temperatures. Our method combines insensible water loss measured by a continuous read-out electronic scale with heat production as determined by open circuit measurement of oxygen consumption. An increase of 1 to 2 degrees C, to an ambient temperature above or near the top of the neutral zone, produced a significant rise in insensible water loss, from 1.90 +/- 0.76 to 3.08 +/- 1.19 ml/kg/hour (mean +/- SD), a corresponding rise in evaporative heat loss, and a fall in nonevaporative heat loss. A decrease of 1 to 2 degrees C, to a slightly subneutral ambient temperature, resulted in an increase in oxygen consumption from 5.82 +/- 0.92 to 7.45 +/- 1.50 ml/kg/minute, and an increase in total heat loss, but no change in insensible water loss and evaporative heat loss. The increased total heat loss was judged to be due entirely to a greater nonevaporative heat loss, both by convection and by radiation. The data confirm that ambient temperature is an important determinant of the magnitude and the partition of heat loss in low-birth-weight infants.
为了确定中性环境温度,并评估偏离该温度对不显性失水量和热平衡的影响,我们在传统培养箱中,于四个不同的预定环境温度下对12名早产儿进行了研究。我们的方法将通过连续读数电子秤测量的不显性失水量与通过开路测量氧气消耗量确定的产热相结合。环境温度升高1至2摄氏度,达到中性区顶部或接近顶部时,不显性失水量显著增加,从1.90±0.76毫升/千克/小时增至3.08±1.19毫升/千克/小时(平均值±标准差),蒸发散热相应增加,非蒸发散热减少。环境温度降低1至2摄氏度,降至略低于中性的温度时,氧气消耗量从5.82±0.92毫升/千克/分钟增至7.45±1.50毫升/千克/分钟,总散热量增加,但不显性失水量和蒸发散热量无变化。总散热量增加被判定完全是由于对流和辐射导致的非蒸发散热量增加。这些数据证实,环境温度是低体重儿热量散失量和散失方式的重要决定因素。