Pedersen K E, Koldkjaer O, Berndtz N H, Hvidt S, Kjaer K, Midtskov C, Sanchez G
Acta Med Scand. 1982;211(5):335-9. doi: 10.1111/j.0954-6820.1982.tb01958.x.
To assess the cellular effects of digoxin, intraerythrocytic sodium and potassium concentrations were measured in 17 patients during the early phase of digitalization, in 45 patients on long-term therapy and in 64 non-digitalized control patients. Acute digitalization raised intraerythrocytic sodium from 11.6 +/- 0.4 to 16.7 +/- 1.0 mmol/l (mean +/- SEM) (p less than 0.01) and reduced intraerythrocytic potassium from 100.1 +/- 1.3 to 95.9 +/- 1.8 mmol/l (p less than 0.01). These changes were strongly correlated with the steady-state plasma digoxin concentration. During a few weeks of digoxin therapy, the intraerythrocytic cation composition normalized gradually. In patients on chronic treatment, neither intraerythrocytic sodium (11.3 +/- 0.3 mmol/l) nor potassium concentrations (100.0 +/- 0.6 mmol/l) differed significantly from the values of the control group (11.4 +/- 0.2 and 99.9 +/- 0.5 mmol/l, respectively). The changes in intraerythrocytic cation concentrations, induced by acute digitalization, seem to disappear during chronic administration of the drug.
为评估地高辛的细胞效应,我们测定了17例处于洋地黄化早期的患者、45例接受长期治疗的患者以及64例未接受洋地黄治疗的对照患者红细胞内的钠和钾浓度。急性洋地黄化使红细胞内钠浓度从11.6±0.4 mmol/L升至16.7±1.0 mmol/L(均值±标准误)(p<0.01),并使红细胞内钾浓度从100.1±1.3 mmol/L降至95.9±1.8 mmol/L(p<0.01)。这些变化与稳态血浆地高辛浓度密切相关。在数周的地高辛治疗期间,红细胞内阳离子组成逐渐恢复正常。在接受长期治疗的患者中,红细胞内钠浓度(11.3±0.3 mmol/L)和钾浓度(100.0±0.6 mmol/L)与对照组的值(分别为11.4±0.2和99.9±0.5 mmol/L)相比,均无显著差异。急性洋地黄化引起的红细胞内阳离子浓度变化在药物长期给药期间似乎消失了。