Di Rienzo M, Castiglioni P, Rizzo F, Faini A, Mazzoleni P, Lombardi C, Meriggi P, Parati G
Fondazione Don Carlo Gnocchi, ONLUS, Dept. of Biomedical Technology, Via Capecelatro 66, 20148 Milano, Italy.
Methods Inf Med. 2010;49(5):521-5. doi: 10.3414/ME09-02-0053. Epub 2010 Jun 22.
To investigate the effects of hypoxia during sleep on linear and self-similar components of heart rate variability (HRV) in eight healthy subjects at high altitude on Mount Everest.
ECG was monitored by using an innovative textile-based device, the MagIC system. For each subject three night recordings were performed at sea level (SL), at 3500 m and 5400 m above SL. RR Interval (RRI) was derived on a beat-by-beat basis from the ECG and the VLF, LF and HF spectral components and the LF/HF ratio were estimated. Short- (α₁) and long-term (α₂) scale exponents as well as the recently proposed spectrum of self-similarity coefficients, α(n) were estimated by detrended fluctuation analysis (DFA).
With respect to SL, all HRV parameters but one (α₂) were significantly modified at 3500 m. However, at 5400 m they tended to return to the SL values and this was in contrast with the increase in the hypobaric hypoxia and in the number of central sleep apneas occurring at higher altitude. The only HRV index that displayed changes at 5400 m was the DFA α(n) spectrum, with α(n) values significantly lower than at SL for 20 < n <50 and higher for 200 < n <400, being n the box size.
While the biological interpretation of these results is still in progress, our data indicates that the cardiac response to high altitude hypoxia during sleep can hardly be fully explored by traditional HRV estimators only, and requires the additional support of more sophisticated indexes exploring also nonlinear and fractal features of cardiac variability.
研究睡眠期间缺氧对珠穆朗玛峰高海拔地区8名健康受试者心率变异性(HRV)线性和自相似成分的影响。
使用创新的基于纺织品的设备MagIC系统监测心电图。对每位受试者在海平面(SL)、海拔3500米和海拔5400米处进行三晚记录。逐搏从心电图得出RR间期(RRI),并估计超低频(VLF)、低频(LF)和高频(HF)频谱成分以及LF/HF比值。通过去趋势波动分析(DFA)估计短期(α₁)和长期(α₂)尺度指数以及最近提出的自相似系数谱α(n)。
与海平面相比,除一项(α₂)外,所有HRV参数在海拔3500米处均有显著改变。然而,在海拔5400米处,它们倾向于恢复到海平面值,这与更高海拔处出现的低氧性缺氧增加和中枢性睡眠呼吸暂停数量增加形成对比。在海拔5400米处显示变化的唯一HRV指标是DFA α(n)谱,对于20 < n < 50,α(n)值显著低于海平面,对于200 < n < 400则高于海平面,其中n为区间大小。
虽然这些结果的生物学解释仍在进行中,但我们的数据表明,仅靠传统的HRV估计器很难充分探索睡眠期间高海拔缺氧时的心脏反应,还需要更复杂的指标提供额外支持,这些指标也要探索心脏变异性的非线性和分形特征。