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钾通道中的非典型传导机制。

Atypical mechanism of conduction in potassium channels.

作者信息

Furini Simone, Domene Carmen

机构信息

Physical and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford, Oxford OX13QZ, United Kingdom.

出版信息

Proc Natl Acad Sci U S A. 2009 Sep 22;106(38):16074-7. doi: 10.1073/pnas.0903226106. Epub 2009 Sep 4.

DOI:10.1073/pnas.0903226106
PMID:19805261
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC2752519/
Abstract

Potassium channels can conduct passively K+ ions with rates of up to approximately 10(8) ions per second at physiological conditions, and they are selective to these species by a factor of 10(4) over Na+ ions. Ion conduction has been proposed to involve transitions between 2 main states, with 2 or 3 K+ ions occupying the selectivity filter separated by an intervening water molecule. The largest free energy barrier of such a process was reported to be of the order of 2-3 kcal mol(-1). Here, we present an alternative mechanism for conduction of K+ in potassium channels where site vacancies are involved, and we propose that coexistence of several ion permeation mechanisms is energetically possible. Conduction can be described as a more anarchic phenomenon than previously characterized by the concerted translocations of K+-water-K+.

摘要

钾离子通道在生理条件下能够以高达每秒约10⁸个离子的速率被动传导钾离子,并且它们对这些离子的选择性比对钠离子高10⁴倍。离子传导被认为涉及两个主要状态之间的转变,其中2个或3个钾离子占据选择性过滤器,中间隔着一个水分子。据报道,这样一个过程的最大自由能垒约为2 - 3千卡/摩尔。在这里,我们提出了一种钾离子通道中钾离子传导的替代机制,其中涉及位点空位,并且我们提出几种离子渗透机制共存在能量上是可能的。传导可以被描述为一种比以前由K⁺-水-K⁺的协同转运所描述的更为无序的现象。

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