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在离体龟心脏中铯对钾的可逆性替代作用。

The reversible replacement of internal potassium by caesium in isolated turtle heart.

作者信息

Guerin M, Wallon G

出版信息

J Physiol. 1979 Aug;293:525-37. doi: 10.1113/jphysiol.1979.sp012905.

DOI:10.1113/jphysiol.1979.sp012905
PMID:501630
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC1280729/
Abstract
  1. By perfusing the isolated turtle heart with Cs solution, most of the intracellular K can be replaced by Cs. After 3--4 hr, Cs approaches a steady-state distribution with a concentration slightly below initial K concentration. 2. During the initial stages of perfusion, the heart accumulated Cs and lost K, the exchange ratio of K for Cs was estimated to be about 0.6. Subsequently perfusion yielded an equi-ionic substitution of K by Cs. 3. In presence of DNP (2 x 10(-4) M), K efflux and Cs accumulation increased but the low initial K--Cs exchange was abolished. Then, the replacement of K by Cs took place at a ratio of K:Cs of about 0.8. Ouabain (10(-5) M) suppressed uptake of Cs whereas K loss was the same as with DNP. 4. These results confirm that permeability of the cardiac sarcolemma to Cs is low, and suggest that the movement of Cs must be mainly attributed to its active transport into cells by the ionic exchange which normally transports K+ and is coupled to the extrusion of Na. The initial low net K efflux could be explained by an accumulation process which facilitates retention of K by the heart. A mechanism of this kind would be described as active reabsorption of some K present in extracellular space and would consequently reduce the uptake of Cs. 5. After loading the heart with Cs, perfusion with K solution showed the exchange of Cs for K at a ratio of Cs:K of about 0.5. K reaccumulation is reduced by ouabain (10(-5) M) and comes back to a normal steady-state distribution after 5 hr. At this time, K concentration was slightly below normal K value, but only half Cs content was eliminated. After 15 hr of perfusion, intracellular K remained constant whereas 15% of the original Cs remained.
摘要
  1. 用铯溶液灌注离体龟心,大部分细胞内钾可被铯取代。3 - 4小时后,铯达到稳态分布,其浓度略低于初始钾浓度。2. 在灌注初期,心脏积累铯并丢失钾,钾与铯的交换率估计约为0.6。随后灌注导致铯对钾的等离子体取代。3. 在存在二硝基苯酚(2×10⁻⁴ M)的情况下,钾外流和铯积累增加,但初始低钾 - 铯交换被消除。然后,铯对钾的取代以约0.8的钾:铯比例发生。哇巴因(10⁻⁵ M)抑制铯的摄取,而钾丢失与二硝基苯酚处理时相同。4. 这些结果证实心肌肌膜对铯的通透性较低,并表明铯的移动主要归因于其通过通常转运钾离子并与钠离子外流偶联的离子交换主动转运进入细胞。初始低钾净外流可由促进心脏保留钾的积累过程来解释。这种机制可被描述为对细胞外空间中一些钾的主动重吸收,因此会减少铯的摄取。5. 用铯使心脏负荷后,用钾溶液灌注显示铯与钾以约0.5的铯:钾比例交换。哇巴因(10⁻⁵ M)减少钾的重新积累,5小时后恢复到正常稳态分布。此时,钾浓度略低于正常钾值,但仅消除了一半的铯含量。灌注15小时后,细胞内钾保持恒定,而仍有15%的原始铯残留。

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