Laboratories of The Rockefeller Institute for Medical Research.
J Gen Physiol. 1932 Sep 20;16(1):157-63. doi: 10.1085/jgp.16.1.157.
In a model consisting of a non-aqueous layer (representing the protoplasm) placed between an inner, more acid, aqueous layer (representing the sap) and an outer, more alkaline, aqueous solution (representing the external solution bathing a living cell) the penetration of potassium creates an outwardly directed potential against which potassium continues to diffuse inward, thereby increasing the outward potential. This continues until the steady state is reached. The potassium sets up less potential in entering than in escaping and the net result is an outwardly directed potential. A similar process appears to take place in certain living cells.
在一个模型中,非水层(代表细胞质)置于内、更酸的水层(代表汁液)和外、更碱性的水溶液(代表浸泡活细胞的外部溶液)之间,钾的渗透会产生向外的电位,钾继续向内扩散,从而增加向外的电位。这一过程持续到达到稳定状态。钾进入时产生的电位小于逃脱时产生的电位,净结果是向外的电位。在某些活细胞中似乎也发生了类似的过程。