Thompson R L, Hayward J S
Department of Biology, University of Victoria, British Columbia, Canada.
J Appl Physiol (1985). 1996 Sep;81(3):1128-37. doi: 10.1152/jappl.1996.81.3.1128.
Simulated conditions of hiking in rain, wind, and cold, without protective rainwear, were used to investigate wet-cold hypothermia in 18 male subjects. Thermal, metabolic, and motor responses were monitored during an attempted 5-h walk (5.1 km/h) at 5 degrees C, with continuous exposure to rain (7.4 cm/h) and wind (8.0 km/h) over the final 4 h. The majority of subjects (11) could not complete the protocol because of intolerance of wet-cold conditions during the last 2 h. Therefore, data from 5 subjects who completed the protocol in rain and control conditions were used to describe the general pattern of response. During the 1st h of walking, core temperature rose 1 degree C to 38.1 degrees C. The subsequent 2 h of rain caused substantial cold stress, indicated by a 40% increase in heat production due to shivering and significant loss of strength and manual dexterity. However, core temperature only decreased to 37.1 degrees C, merely eliminating the initial exercise hyperthermia. Over the last 2 h of rain, core temperature remained relatively stable at 36.8 degrees C, decreasing slightly to 36.4 degrees C by 5 h. Two other subjects developed significant hypothermia (35 degrees C). One demonstrated fatigue of shivering after 2.5 h of rain, confirming the exhaustion hypothesis of wet-cold hypothermia. The older cooled rapidly when he failed to maintain the walking pace. We conclude that if a person can tolerate the intense discomfort of prolonged wet-cold exposure, he or she has the potential to resist significant core hypothermia for at least 4 h of walking under the conditions of this experiment. Exceptions to this generalization occur, making exposure of < 4 h a hypothermia risk for some individuals. Exposures > 4 h would involve increasing probability of rapid decline into hypothermia, associated with exhaustion of shivering and exercise heat production.
在无防护雨具的情况下,模拟在雨、风和寒冷环境中徒步的条件,对18名男性受试者进行了湿冷性体温过低的研究。在5摄氏度下尝试进行5小时的步行(速度为5.1公里/小时)过程中,监测热、代谢和运动反应,在最后4小时持续暴露于雨(7.4厘米/小时)和风(8.0公里/小时)中。大多数受试者(11名)因在最后2小时无法耐受湿冷条件而未能完成实验方案。因此,使用5名在雨中及对照条件下完成实验方案的受试者的数据来描述一般反应模式。在步行的第1小时,核心体温上升1摄氏度至38.1摄氏度。随后2小时的降雨造成了严重的冷应激,表现为颤抖导致的产热增加40%,以及力量和手部灵活性的显著丧失。然而,核心体温仅降至37.1摄氏度,仅消除了最初的运动性体温过高。在降雨的最后2小时,核心体温相对稳定在36.8摄氏度,到5小时时略有下降至36.4摄氏度。另外两名受试者出现了显著的体温过低(35摄氏度)。一名受试者在降雨2.5小时后出现颤抖疲劳,证实了湿冷性体温过低的耗竭假说。年龄较大的受试者在未能保持步行速度时体温迅速下降。我们得出结论,如果一个人能够耐受长时间湿冷暴露带来的强烈不适,那么在本实验条件下,他或她有潜力在至少4小时的步行过程中抵抗显著的核心体温过低。但这一普遍规律存在例外,对于一些个体而言,暴露时间小于4小时也存在体温过低的风险。暴露时间超过4小时会增加迅速陷入体温过低的可能性,这与颤抖和运动产热的耗竭有关。