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高原肺水肿的早期发病机制:时间进程和机制。

Early hours in the development of high-altitude pulmonary edema: time course and mechanisms.

机构信息

Pulmonary, Critical Care and Sleep Medicine, University of Washington, Veterans Affairs Puget Sound Health Care System, Seattle, Washington.

出版信息

J Appl Physiol (1985). 2020 Jun 1;128(6):1539-1546. doi: 10.1152/japplphysiol.00824.2019. Epub 2020 Mar 26.

Abstract

Clinically evident high-altitude pulmonary edema (HAPE) is characterized by severe cyanosis, dyspnea, cough, and difficulty with physical exertion. This usually occurs within 1-2 days of ascent often with the additional stresses of any exercise and hypoventilation of sleep. The earliest events in evolving HAPE progress through clinically silent and then minimally recognized problems. The most important of these events involves an exaggerated elevation of pulmonary artery (PA) pressure in response to the ambient hypoxia. Hypoxic pulmonary vasoconstriction (HPV) is a rapid response with several phases. The first phase in both resistance arterioles and venules occurs within 5-10 min. This is followed by a second phase that further raises PA pressure by another 100% over the next 2-8 h. Combined with vasoconstriction and likely an unevenness in the regional strength of HPV, pressures in some microvascular regions with lesser arterial constriction rise to a level that initiates greater filtration of fluid into the interstitium. As pressures continue to rise local lymphatic clearance rates are exceeded and interstitial fluid begins to accumulate. Beyond elevation of transmural pressure gradients there is a dynamic noninjurious relaxation of microvascular and epithelial cell-cell contacts and an increase in transcellular vesicular transport which accelerate leakage. At some point with further pressure elevation, damage occurs with breaks of the barrier and bleeding into the alveolar space, a late-stage situation termed capillary stress failure. Earlier before there is fluid accumulation, alveolar hypoxia and hyperventilation-induced hypocapnia reduce the capacity of the alveolar epithelium to reabsorb sodium and water back into the interstitial space. More modest ascent which slows the rate of rise in PA pressure and allows for adaptive remodeling of the microvasculature, drugs which lower PA pressure, and those that can enhance fluid reabsorption will all forestall the deleterious early rise of microvascular pressures and diminished active alveolar fluid reabsorption that precede and underlie the development of HAPE.

摘要

临床上明显的高原肺水肿(HAPE)的特征是严重发绀、呼吸困难、咳嗽和体力活动困难。这通常发生在上升后 1-2 天内,通常伴有任何运动的额外压力和睡眠时的通气不足。HAPE 发展过程中的最早事件经历了从临床无症状到最小程度的认识问题。这些事件中最重要的是肺动脉(PA)压力因周围缺氧而过度升高。缺氧性肺血管收缩(HPV)是一种快速反应,有几个阶段。阻力小动脉和小静脉中的第一个阶段在 5-10 分钟内发生。接下来是第二个阶段,在接下来的 2-8 小时内,PA 压力进一步升高 100%。再加上血管收缩和 HPV 的区域强度不均,一些微血管区域的压力升高到开始将更多的液体滤入间质的水平。随着压力的继续升高,局部淋巴清除率超过,间质液开始积聚。局部跨壁压力梯度升高之外,还有微血管和上皮细胞-细胞接触的动态非损伤性松弛以及细胞内囊泡运输的增加,这加速了渗漏。在某些情况下,随着压力的进一步升高,屏障会破裂并发生出血进入肺泡腔,这是一个晚期的情况,称为毛细血管应激衰竭。在发生积液之前,肺泡缺氧和通气过度引起的低碳酸血症会降低肺泡上皮细胞将钠和水重新吸收回间质空间的能力。更适度的上升,减缓 PA 压力的上升速度,并允许微血管的适应性重塑,降低 PA 压力的药物,以及可以增强液体吸收的药物,都将阻止微血管压力的早期升高和损害,以及在 HAPE 发展之前和基础上的主动肺泡液体吸收的减少。

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