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皮肤氧张力作为施加于皮肤压力的函数:对压疮形成的影响。

Skin oxygen tension as a function of imposed skin pressure: implication for decubitus ulcer formation.

作者信息

Seiler W O, Stähelin H B

出版信息

J Am Geriatr Soc. 1979 Jul;27(7):298-301. doi: 10.1111/j.1532-5415.1979.tb06043.x.

Abstract

Pressure is a crucial factor in the formation of decubitus ulcers. To elucidate the effect of imposed skin pressure, a new cutaneous oxygen sensor was used to measure the skin oxygen tension under increasing pressure upon skin tissue at "hard sites" (bony prominences) and at "soft sites" (muscle-padded areas). At hard sites the skin oxygen tension fell rapidly under increasing pressure (y = 90.9--0.39. X; r = 0.98) from an initial value of 86.4 +/- 10.6 to 20.2 +/- 12.1 mm Hg under an imposed skin pressure load of 175 gm/cm 2. At soft sites a pressure load of 175 gm/cm 2 decreased the skin oxygen tension only from 82.9 +/- 5.8 to 71.4 +/- 10.0 mm Hg. These results may explain why hard sites (bony prominences) are preferential areas for decubitus ulcer formation.

摘要

压力是压疮形成的关键因素。为了阐明施加的皮肤压力的影响,一种新型皮肤氧传感器被用于测量在“硬部位”(骨隆突)和“软部位”(肌肉垫部位)对皮肤组织施加递增压力时的皮肤氧张力。在硬部位,随着压力增加,皮肤氧张力迅速下降(y = 90.9 - 0.39X;r = 0.98),在175克/平方厘米的皮肤压力负荷下,从初始值86.4±10.6毫米汞柱降至20.2±12.1毫米汞柱。在软部位,175克/平方厘米的压力负荷仅使皮肤氧张力从82.9±5.8毫米汞柱降至71.4±10.0毫米汞柱。这些结果或许可以解释为什么硬部位(骨隆突)是压疮形成的优先区域。

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