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尿渗透压间隙的一种改良方法:一种估算尿铵的改进方法。

A modification of the urine osmolal gap: an improved method for estimating urine ammonium.

作者信息

Dyck R F, Asthana S, Kalra J, West M L, Massey K L

机构信息

Department of Medicine, University of Saskatchewan, Saskatoon, Canada.

出版信息

Am J Nephrol. 1990;10(5):359-62. doi: 10.1159/000168150.

Abstract

A modification of the urine osmolal gap was evaluated as an estimate of urine [NH4+]. We proposed that: Urine [NH4+] = Urine osmolality - [2(Na+ + K+) + urea + glucose]/2 Spot urine samples were collected from normal volunteers and from individuals with ketonuria; the modified urine osmolal gap as well as two other previously described estimates of urine [NH4+] were compared with measured urine [NH4+]. There was a significant positive linear correlation between the urine [NH4+] and the modified urine osmolal gap in normal volunteers (r = 0.81; p less than 0.01) and in individuals with ketonuria (r = 0.93; p less than 0.001). The originally described urine osmolal gap greatly overestimated the urine [NH4+] but also showed a significant correlation. The urine anion gap was not a valid estimate of urine [NH4+] within the range of values measured in our subjects. The modified urine osmolal gap is an improvement over previously described estimates of urine [NH4+] and can be used as a single calculation in place of the other two.

摘要

对尿渗透压间隙的一种改良方法进行了评估,以估算尿[NH4+]。我们提出:尿[NH4+] = 尿渗透压 - [2(Na+ + K+) + 尿素 + 葡萄糖]/2 从正常志愿者和酮尿症患者中收集即时尿样;将改良后的尿渗透压间隙以及另外两种先前描述的尿[NH4+]估算方法与实测尿[NH4+]进行比较。在正常志愿者中,尿[NH4+]与改良后的尿渗透压间隙之间存在显著的正线性相关性(r = 0.81;p < 0.01),在酮尿症患者中也是如此(r = 0.93;p < 0.001)。最初描述的尿渗透压间隙极大地高估了尿[NH4+],但也显示出显著相关性。在我们研究对象所测的值范围内,尿阴离子间隙并非尿[NH4+]的有效估算指标。改良后的尿渗透压间隙优于先前描述的尿[NH4+]估算方法,可作为一种单一计算方法替代另外两种方法使用。

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