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A new equation for calculation of colloid osmotic pressure based on serum total protein concentration and UV-light absorption

机译:基于血清总蛋白浓度和紫外吸收的胶体渗透压计算新方程

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Colloid osmotic pressure (COP) plays a major role in transcapillary fluid exchange. COP is generally calculated using the serum total protein (TP) concentration. The difference between calculated and measured COP may be considerable depending on albumin to globulin (A/G) ratio. There is a linear relationship between the absorbance and protein concentration. The aim of this study was to find an equation for calculation of COP based on serum TP and UV-light absorption. Serum samples with different A/G ratio were prepared in vitro, and COP, serum TP concentration and serum UV-light absorption (at 280 nm) were measured. The relationship between COP, serum TP concentration and UV-light absorption were determined. The validity of the obtained equations was confirmed by comparison between measured and calculated COP in 122 hospitalized patients and healthy individuals. By a linear curve fitting, the following equation was obtained for calculation of COP with a highly significant correlation (r2=0.92, p0.05): COP=1.8×TP×Abs+5.5; where Abs is the serum UV-light absorption at 280 nm. This equation is accurate and simple formula for calculation of COP based on serum TP concentration and UV-light absorption and can be useful in clinic where colloid osmometers are not available.
机译:胶体渗透压(COP)在跨毛细血管液交换中起主要作用。 COP通常使用血清总蛋白(TP)浓度计算。根据白蛋白与球蛋白(A / G)的比例,计算出的COP和测量到的COP之间的差异可能会很大。吸光度和蛋白质浓度之间存在线性关系。这项研究的目的是找到一个基于血清TP和紫外线吸收来计算COP的方程。体外制备具有不同A / G比的血清样品,并测量COP,血清TP浓度和血清UV光吸收(在280nm)。确定了COP,血清TP浓度和紫外线吸收之间的关系。通过比较122位住院患者和健康个体的实测COP和计算COP,可以确认所获得方程的有效性。通过线性曲线拟合,获得以下等式,具有非常显着的相关性(r2 = 0.92,p <0.05),用于计算COP:COP = 1.8×TP×Abs + 5.5;其中,Abs是在280 nm下的血清紫外线吸收率。该公式是基于血清TP浓度和紫外线吸收量计算COP的准确而简单的公式,可用于无法使用胶体渗透计的临床中。

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