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未适应环境的受试者在急性低压缺氧2小时期间前臂和下肢的容积变化。

Volume changes in the forearm and lower limbs during 2 h of acute hypobaric hypoxia in nonacclimatized subjects.

作者信息

Schirlo C, Bub A, Reize C, Bührer A, Kohl J, Koller E A

机构信息

Department of Physiology, University of Zurich, Switzerland.

出版信息

Eur J Appl Physiol Occup Physiol. 1997;75(2):124-31. doi: 10.1007/s004210050136.

Abstract

To investigate the role of fluid shifts during the short-term adjustment to acute hypobaric hypoxia (AHH), the changes in lower limb (LV) and forearm volumes (FV) were measured using a strain-gauge plethysmograph technique in ten healthy volunteers exposed to different altitudes (450 m, 2500 m, 3500 m, 4500 m) in a hypobaric chamber. Arterial blood pressure, heart rate, arterial oxygen saturation (SaO2), endtidal gases, minute ventilation and urine flow were also determined. A control experiment was performed with an analogous protocol under normobaric normoxic conditions. The results showed mean decreases both in LV and FV of 0.52 (SD 0.39) ml x 100 ml(-1) and -0.65 (SD 0.32) ml x 100 ml(-1), respectively, in the hypoxia experiments [controls: LV 0.28 (SD 0.37), FV 0.41 (SD 0.47) ml x 100 ml(-1)]. Descent to normoxia resulted in further small but not significant decreases in mean LV [-0.02 (SD 0.11) ml x 100 ml(-1)], whereas mean FV tended to increase slightly [ + 0.02 (SD 0.14) ml x 100 ml(-1)]; in the control experiments mean LV and FV decreased continuously during the corresponding times [-0.19 (SD 0.31), -0.18 (SD 0.10) ml x 100 ml(-1) , respectively]. During the whole AHH, mean urine flow increased significantly from 0.84 (SD 0.41) ml x min(-1) to 3.29 (SD 1.43) ml x min(-1) in contrast to the control conditions. We concluded that peripheral fluid volume shifts form a part of the hypoxia-induced acute cardiovascular changes at high altitude. In contrast to the often reported formation of peripheral oedema after prolonged exposure to hypobaric hypoxia, the results provided no evidence for the development of peripheral oedema during acute induction to high altitude. However, the marked increase in interindividual variance in SaO2 and urine flow points to the appearance of the first differences in the short-term adjustment even after 2 h of acute hypobaric hypoxia.

摘要

为研究短期适应急性低压缺氧(AHH)过程中体液转移的作用,在低压舱中,对10名健康志愿者分别暴露于不同海拔高度(450米、2500米、3500米、4500米)时下肢(LV)和前臂容积(FV)的变化进行了测量,测量采用应变片体积描记技术。同时还测定了动脉血压、心率、动脉血氧饱和度(SaO2)、呼出气体终末成分、分钟通气量和尿流量。在常压常氧条件下按照类似方案进行了对照实验。结果显示,在缺氧实验中,LV和FV的均值分别下降了0.52(标准差0.39)毫升×100毫升⁻¹和-0.65(标准差0.32)毫升×100毫升⁻¹[对照组:LV为0.28(标准差0.37),FV为0.41(标准差0.47)毫升×100毫升⁻¹]。恢复到常氧状态后,LV均值进一步出现微小但不显著的下降[-0.02(标准差0.11)毫升×100毫升⁻¹],而FV均值则有轻微上升趋势[+0.02(标准差0.14)毫升×100毫升⁻¹];在对照实验中,相应时间段内LV和FV均值持续下降[-0.19(标准差0.31)、-0.18(标准差0.10)毫升×100毫升⁻¹]。在整个AHH期间,与对照条件相比,平均尿流量从0.84(标准差0.41)毫升×分钟⁻¹显著增加至3.29(标准差1.43)毫升×分钟⁻¹。我们得出结论,外周体液量转移是高原缺氧诱导的急性心血管变化的一部分。与长期暴露于低压缺氧后常报道的外周水肿形成情况不同,本研究结果未提供急性高原暴露期间外周水肿发展的证据。然而,SaO2和尿流量个体间差异的显著增加表明,即使在急性低压缺氧2小时后,短期适应过程中也出现了最初的差异。

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