Sedin G, Hammarlund K, Nilsson G E, Strömberg B, Oberg P A
Clin Perinatol. 1985 Feb;12(1):79-99.
Measurement of transepidermal water loss without disturbing the microclimate in the air layers above the skin has not been possible with previously available methods. The introduction of a new instrument, the Evaporimeter, for measuring the vapor pressure gradient above the skin surface meant that the evaporation of water from the skin could be determined. Each measurement is of short duration, and measurements can be made even in the most preterm infants under the conditions in which they are normally nursed. Studies of the evaporation rate and transepidermal water loss by this technique have increased our knowledge considerably during the last ten years. It is now well established that the loss of water from the skin surface is related to the ambient humidity, gestational age at birth, and postnatal age, and to weight, activity, and body temperature, and that it differs between appropriate- and small-for-gestational-age infants. Conclusions of special clinical importance drawn from these studies are that the most preterm infants may lose as much as 13 per cent of their body weight as TEWL during their first day after birth even at an ambient humidity of 50 per cent, and much more at a lower ambient humidity, and that their losses gradually diminish with age but are of significance even four weeks after birth. Small-for-gestational-age infants have a lower TEWL early after birth than appropriate-for-gestational-age infants. For heat exchange between the infant and its environment, TEWL plays an important role. In preterm infants, losses of heat through evaporation are very high early after birth. On the other hand, their heat losses through other routes are smaller because of the high ambient temperature in which they have be nursed in order to maintain a stable and normal body temperature. Simultaneous measurements of evaporation rate and skin blood flow have shown that the skin blood flow increases at a lower body temperature than the evaporation rate and that not all full-term infants sweat in a warm environment even when their body temperature becomes higher than 37.2 degrees C, which may indicate a delay in the postnatal adaptation of heat regulation. In addition, this regulation can easily be disturbed by a central cold-stimulation in infants who react with sweating in a warm environment.
使用先前可用的方法无法在不干扰皮肤上方空气层微气候的情况下测量经表皮水分流失。一种用于测量皮肤表面蒸汽压梯度的新仪器——蒸发仪的引入,意味着可以确定皮肤水分的蒸发情况。每次测量持续时间短,甚至可以在最早产的婴儿正常护理的条件下进行测量。在过去十年中,通过这种技术对蒸发速率和经表皮水分流失的研究极大地增加了我们的知识。现在已经明确,皮肤表面的水分流失与环境湿度、出生时的胎龄、出生后年龄、体重、活动和体温有关,并且在适于胎龄儿和小于胎龄儿之间存在差异。从这些研究中得出的具有特殊临床重要性的结论是,即使在环境湿度为50% 的情况下,最早产的婴儿在出生后的第一天经表皮水分流失可能高达其体重的13%,在较低的环境湿度下流失更多;并且他们的流失量会随着年龄增长逐渐减少,但即使在出生四周后仍很显著。小于胎龄儿出生后早期的经表皮水分流失低于适于胎龄儿。对于婴儿与其环境之间的热交换,经表皮水分流失起着重要作用。在早产儿中,出生后早期通过蒸发的热量损失非常高。另一方面,由于为了维持稳定和正常体温而将他们置于较高的环境温度中,他们通过其他途径的热量损失较小。同时测量蒸发速率和皮肤血流量表明,皮肤血流量在体温低于蒸发速率时增加,并且并非所有足月儿在温暖环境中都会出汗,即使他们的体温高于37.2摄氏度,这可能表明出生后热调节适应延迟。此外,在温暖环境中会出汗的婴儿,其这种调节很容易受到中枢冷刺激的干扰。