Department of Kinesiology, The Pennsylvania State University, University Park, Pennsylvania, United States.
Center for Healthy Aging, College of Health and Human Development, The Pennsylvania State University, University Park, Pennsylvania, United States.
J Appl Physiol (1985). 2023 Aug 1;135(2):292-299. doi: 10.1152/japplphysiol.00222.2023. Epub 2023 Jun 22.
With climate change, humans are at a greater risk for heat-related morbidity and mortality, often secondary to increased cardiovascular strain associated with an elevated core temperature (T). Critical environmental limits (i.e., the upper limits of compensable heat stress) have been established based on T responses for healthy, young individuals. However, specific environmental limits for the maintenance of cardiovascular homeostasis have not been investigated in the context of thermal strain during light activity. Therefore, the purposes of this study were to ) identify the specific environmental conditions (combinations of ambient temperature and water vapor pressure) at which cardiovascular drift [i.e., a continuous rise in heart rate (HR)] began to occur and ) compare those environments to the environmental limits for the maintenance of heat balance. Fifty-one subjects (27 F; 23 ± 4 yr) were exposed to progressive heat stress across a wide range of environmental conditions in an environmental chamber at two low metabolic rates reflecting minimal activity (MinAct; 159 ± 34 W) or light ambulation (LightAmb; 260 ± 55 W). Whether systematically increasing ambient temperature or humidity, the onset of cardiovascular drift occurred at lower environmental conditions compared with T inflection points at both intensities ( < 0.05). Furthermore, the time at which cardiovascular drift began preceded the time of T inflection (MinAct = 0.01; LightAmb = 0.0002), and the difference in time between HR and T inflection points did not differ (MinAct = 0.08; LightAmb = 0.06) across environmental conditions for either exercise intensity. These data suggest that even in young adults, increases in cardiovascular strain precede the point at which heat stress becomes uncompensable during light activity. To our knowledge, this study is the first to ) identify the specific combinations of temperature and humidity at which an increase in cardiovascular strain (cardiovascular drift) occurs and ) compare those environments to the critical environmental limits for the maintenance of heat balance. We additionally examined the difference in time between the onset of increased cardiovascular strain and uncompensable heat stress. We show that an increase in cardiovascular strain systematically precedes sustained heat storage in young adults.
随着气候变化,人类面临更大的与热相关的发病率和死亡率风险,这通常是由于核心温度(T)升高导致心血管压力增加所致。已经根据健康年轻人的 T 反应确定了临界环境极限(即可补偿热应激的上限)。然而,在轻度活动期间的热应激下,尚未研究维持心血管稳态的特定环境极限。因此,本研究的目的是:)确定心血管漂移(即心率持续升高)开始发生的特定环境条件(环境温度和水蒸气压力的组合);)将这些环境与维持热平衡的环境极限进行比较。51 名受试者(27 岁,F;23 ± 4 岁)在环境室中以两种低代谢率(反映最小活动的 MinAct;159 ± 34 W 和轻度步行的 LightAmb;260 ± 55 W)在广泛的环境条件下进行逐步热应激暴露。无论环境温度或湿度是否系统升高,与两种强度下的 T 拐点相比,心血管漂移的发生都发生在较低的环境条件下(<0.05)。此外,心血管漂移开始的时间早于 T 拐点的时间(MinAct = 0.01;LightAmb = 0.0002),并且在两种运动强度下,HR 和 T 拐点之间的时间差异在环境条件下没有差异(MinAct = 0.08;LightAmb = 0.06)。这些数据表明,即使在年轻人中,心血管压力的增加也先于轻度活动中热应激变得不可补偿的时间点。据我们所知,这项研究首次:)确定心血管压力(心血管漂移)增加时发生的特定温度和湿度组合;)将这些环境与维持热平衡的临界环境极限进行比较。我们还检查了心血管压力增加和不可补偿的热应激之间的时间差异。我们表明,心血管压力的增加系统地先于年轻人持续的热量储存。