Vitale G C, Neill G D, Fenwick M K, Stewart W W, Cuschieri A
Am Surg. 1985 Dec;51(12):675-81.
The precise mechanism of initiation and maintenance of the disturbed fluid and electrolyte balance in cirrhotic patients remains unclear. Measurement of total exchangeable potassium in 11 cirrhotic patients with ascites revealed marked depletion compared to 9 healthy volunteers. Total exchangeable potassium was 50.8 +/- 5.1 m moles/L TBW in the patient group compared to 75.2 +/- 3.4 m moles/L TBW in the control group (P less than 0.01, Mann-Whitney U Test). Total body exchangeable sodium measured 80.1 +/- 3.7 m mole/L TBW in the cirrhotic group, which is not significantly elevated compared to the value in healthy volunteers of 74.1 +/- 1.9 m mole/L TBW. Serum sodium was low in four of the cirrhotic patients (129-133 mEq/L); exchangeable sodium was low in only one of these four (53.4 m mole/L TBW). Serum potassium was low in two of the cirrhotics (2.6-2.9 mEq/L); total body potassium was depressed in both of these patients (43.5-50.1 m mole/L TBW). An additional three patients had a low total body potassium (29.6-48.9 m mole/L TBW) with normal serum levels (4.0-4.2 mEq/L). There was no correlation between serum and total exchangeable electrolyte levels (Pearson's regression, r = 0.16 and 0.23). This work confirms that serum levels are not reliable indicators of true body sodium and potassium stores. The decreased total exchangeable potassium appears to be related to loss of body cell mass rather than intracellular potassium depletion.(ABSTRACT TRUNCATED AT 250 WORDS)
肝硬化患者体内液体和电解质平衡紊乱的起始及维持的确切机制仍不清楚。对11例肝硬化腹水患者的可交换钾总量进行测量,结果显示与9名健康志愿者相比,钾明显缺乏。患者组可交换钾总量为50.8±5.1毫摩尔/升(每升总体液量),而对照组为75.2±3.4毫摩尔/升(每升总体液量)(曼-惠特尼U检验,P<0.01)。肝硬化组总体可交换钠为80.1±3.7毫摩尔/升(每升总体液量),与健康志愿者的74.1±1.9毫摩尔/升(每升总体液量)相比,无显著升高。4例肝硬化患者血清钠较低(129 - 133毫当量/升);这4例中仅1例可交换钠较低(53.4毫摩尔/升,每升总体液量)。2例肝硬化患者血清钾较低(2.6 - 2.9毫当量/升);这2例患者的总体钾均降低(43.5 - 50.1毫摩尔/升,每升总体液量)。另外3例患者总体钾较低(29.6 - 48.9毫摩尔/升,每升总体液量),血清钾水平正常(4.0 - 4.2毫当量/升)。血清与可交换电解质总量水平之间无相关性(皮尔逊回归,r = 0.16和0.23)。这项研究证实血清水平并非体内真实钠和钾储备的可靠指标。可交换钾总量的降低似乎与体细胞量的减少有关,而非细胞内钾缺乏。(摘要截选至250词)