Institute of Mountain Emergency Medicine, EURAC Research, Bolzano, Italy.
Department of Anesthesia and Intensive Care Medicine, 'F. Tappeiner' Hospital, Merano, Italy.
J Physiol. 2021 Feb;599(4):1083-1096. doi: 10.1113/JP280601. Epub 2020 Nov 16.
Acclimatization to hypoxia leads to a reduction in plasma volume (PV) that restores arterial O content. Findings from studies investigating the mechanisms underlying this PV contraction have been controversial, possibly as experimental conditions were inadequately controlled. We examined the mechanisms underlying the PV contraction evoked by 4 days of exposure to hypobaric hypoxia (HH) in 11 healthy lowlanders, while strictly controlling water intake, diet, temperature and physical activity. Exposure to HH-induced an ∼10% PV contraction that was accompanied by a reduction in total circulating protein mass, whereas diuretic fluid loss and total body water remained unchanged. Our data support an oncotically driven fluid redistribution from the intra- to the extravascular space, rather than fluid loss, as the mechanism underlying HH-induced PV contraction.
Extended hypoxic exposure reduces plasma volume (PV). The mechanisms underlying this effect are controversial, possibly as previous studies have been confounded by inconsistent experimental conditions. Here, we investigated the effect of hypobaric hypoxia (HH) on PV in a cross-over study that strictly controlled for diet, water intake, physical activity and temperature. Eleven males completed two 4-day sojourns in a hypobaric chamber, one in normoxia (NX) and one in HH equivalent to 3500 m altitude. PV, urine output, volume-regulating hormones and plasma protein concentration were determined daily. Total body water (TBW) was determined at the end of both sojourns by deuterium dilution. Although PV was 8.1 ± 5.8% lower in HH than in NX after 24 h and remained ∼10% lower thereafter (all P < 0.002), no differences were detected in TBW (P = 0.17) or in 24 h urine volumes (all P > 0.23). Plasma renin activity and circulating aldosterone were suppressed in HH during the first half of the sojourn (all P < 0.05) but thereafter similar to NX, whereas no differences were detected for copeptin between sojourns (all P > 0.05). Markers for atrial natriuretic peptide were higher in HH than NX after 30 min (P = 0.001) but lower during the last 2 days (P < 0.001). While plasma protein concentration was similar between sojourns, total circulating protein mass (TCP) was reduced in HH at the same time points as PV (all P < 0.03). Despite transient hormonal changes favouring increased diuresis, HH did not enhance urine output. Instead, the maintained TBW and reduced TCP support an oncotically driven fluid redistribution into the extravascular compartment as the mechanism underlying PV contraction.
低氧适应会导致血浆体积(PV)减少,从而恢复动脉 O 含量。研究低氧适应导致 PV 收缩的机制的发现一直存在争议,这可能是因为实验条件没有得到充分控制。我们研究了 11 名健康低地人在低压缺氧(HH)环境中暴露 4 天后 PV 收缩的机制,同时严格控制水摄入、饮食、温度和体力活动。HH 诱导的 PV 收缩约为 10%,同时伴随着总循环蛋白质量的减少,而利尿剂液体丢失和总体水保持不变。我们的数据支持渗透压驱动的液体从血管内向血管外空间的重新分布,而不是液体丢失,这是 HH 诱导的 PV 收缩的机制。
长期低氧暴露会降低血浆体积(PV)。这一效应的机制尚存在争议,可能是因为以前的研究因实验条件不一致而受到干扰。在这里,我们通过一项交叉研究调查了 HH 对 PV 的影响,该研究严格控制了饮食、水摄入、体力活动和温度。11 名男性在低压舱中完成了两次为期 4 天的逗留,一次在常氧(NX)中,一次在相当于 3500 米海拔的 HH 中。每天测定 PV、尿排量、调节激素和血浆蛋白浓度。在两次逗留结束时通过氘稀释法测定总体水(TBW)。尽管 HH 后 24 小时 PV 比 NX 低 8.1±5.8%,此后仍保持约 10%的低水平(均 P<0.002),但 TBW(P=0.17)或 24 小时尿量(均 P>0.23)无差异。HH 期间,血浆肾素活性和循环醛固酮在前半段时间被抑制(均 P<0.05),但此后与 NX 相似,而两个逗留期间的 copeptin 无差异(均 P>0.05)。HH 后 30 分钟时心房利钠肽标志物高于 NX(P=0.001),但最后 2 天降低(均 P<0.001)。虽然两个逗留期间的血浆蛋白浓度相似,但总循环蛋白质量(TCP)在与 PV 相同的时间点在 HH 中降低(均 P<0.03)。尽管短暂的激素变化有利于增加尿量,但 HH 并未增加尿量。相反,维持的 TBW 和减少的 TCP 支持渗透压驱动的液体向血管外空间的重新分布,这是 PV 收缩的机制。