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高原缺氧情况下的经胸电阻抗

Transthoracic electrical impedance in cases of high-altitude hypoxia.

作者信息

Roy S B, Balasubramanian V, Khan M R, Kaushik V S, Manchanda S C, Guha S K

出版信息

Br Med J. 1974 Sep 28;3(5934):771-5. doi: 10.1136/bmj.3.5934.771.

Abstract

Changes in transthoracic electrical impedance (T.E.I.) due to high-altitude hypoxia (3,658 m) have been measured in 20 young, healthy Indian soldiers. They were first studied at sea level (198 m) and then rapidly transported by air to 3,658 m, where they were studied daily from day 1 to day 5 and then on days 8 and 10. The mean (+/-S.D.) T.E.I. at sea level (34.6+/-0.6Omega) fell sharply to 29.6+/-0.8Omega, 30.3+/-0.9Omega, and 30.5+/-1.1Omega on days 1, 2, and 3 (P <0.001) and levelled off at 31.5+/-0.7Omega on day 10, which was comparable to the mean value obtained in 13 persons permanently resident at high altitude (32.2+/-0.7Omega). Five sea-level residents who had acute mountain sickness (A.M.S.) or high-altitude pulmonary oedema (H.A.P.O.) had a still lower mean value (22.5+/-1.1Omega). One normal healthy subject who at sea level had a T.E.I. of 34.7Omega developed H.A.P.O. when the T.E.I. fell to 21.1Omega. Ninety minutes after the administration of 80 mg of intravenous frusemide the value increased to 35.5Omega. In another subject with A.M.S. who received 40 mg of frusemide intravenously the T.E.I. rose from 21.9 to 33.2Omega.Since the study was non-invasive the changes in impedance could not be correlated objectively with alterations in either pulmonary blood volume or pulmonary extravascular water space. In the subject, however, with x-ray evidence of H.A.P.O. and a low T.E.I. intravenous frusemide produced a marked rise in T.E.I. together with clearing of the chest x-ray picture within 24 hours, indicating an inverse relationship between impedance and thoracic fluid volume. It is suggested that with further objective verification in man the measurement of T.E.I. may be a potentially promising technique for the early detection of increased pulmonary fluid volume.

摘要

在20名年轻、健康的印度士兵中测量了高海拔低氧(3658米)导致的经胸电阻抗(T.E.I.)变化。他们首先在海平面(198米)进行研究,然后迅速空运至3658米,在那里从第1天到第5天每天进行研究,随后在第8天和第10天进行研究。在海平面时平均(±标准差)T.E.I.为(34.6±0.6Ω),在第1、2和3天急剧降至29.6±0.8Ω、30.3±0.9Ω和30.5±1.1Ω(P<0.001),并在第10天稳定在31.5±0.7Ω,这与13名长期居住在高海拔地区者(32.2±0.7Ω)获得的平均值相当。5名患急性高原病(A.M.S.)或高原肺水肿(H.A.P.O.)的海平面居住者的平均值更低(22.5±1.1Ω)。一名在海平面时T.E.I.为34.7Ω的正常健康受试者,当T.E.I.降至21.1Ω时发生了高原肺水肿。静脉注射80毫克速尿90分钟后,该值升至35.5Ω。在另一名接受40毫克静脉速尿治疗的急性高原病受试者中,T.E.I.从21.9升至33.2Ω。由于该研究为非侵入性,电阻抗变化无法与肺血容量或肺血管外水间隙的改变进行客观关联。然而,在一名有高原肺水肿X线证据且T.E.I.较低的受试者中,静脉注射速尿使T.E.I.显著升高,并在24小时内使胸部X线片清晰,表明电阻抗与胸内液体量呈负相关。有人提出,随着在人体中进一步的客观验证,T.E.I.测量可能是早期检测肺液体量增加的一种潜在有前景的技术。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ebd3/1611914/8d81c962e790/brmedj01998-0031-a.jpg

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Evidence for increased intrathoracic fluid volume in man at high altitude.关于高海拔地区人体胸腔内液体量增加的证据。
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