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手性分子的分离:走向手性同质性的途径。

Separation of chiral molecules: a way to homochirality.

机构信息

Institute of Spectroscopy, Russian Academy of Science, 142190, Troitsk, Moscow Region, Russia.

出版信息

Orig Life Evol Biosph. 2012 Feb;42(1):55-73. doi: 10.1007/s11084-012-9265-6. Epub 2012 Feb 29.

Abstract

A mechanism for separating chiral molecules is proposed. The separation of two enantiomers in an aquifer is considered. The molecules are dragged in the aquifer porous medium by a flow of water or of another liquid. The molecule velocity is u=v/R, where v is the liquid velocity, and R is the retardation factor. The aquifer consists of two one-dimensional layers disposed in series. The layers differ by the retardation factor or by the liquid velocity. The enantiomer velocity is a function of the enantiomer concentrations. This function is different in the two layers. For certain values of the model parameters and when the molecules entering the aquifer are enantiomerically enriched or when the medium is chiral, the concentration of one enantiomer increases around the interface between the two layers and in one layer, whereas the concentration of the other enantiomer decreases. Enantiomer synthesis and decay are not taken into account. The needed values of the parameters can be obtained when the enantiomers are moved by an alternating liquid flow, and the retardation factor oscillates in synchronism with the alternating liquid flow. The parameters of the model are then understood as quantities averaged over one oscillation period. The equations that give the values of the stationary concentrations of the enantiomers are found. The evolution of the enantiomer concentrations is determined by numerically solving a system of two nonlinear advection-dispersion equations. The proposed mechanism may have played a role in the emergence of biomolecular homochirality.

摘要

提出了一种分离手性分子的机制。考虑了在含水层中两种对映异构体的分离。分子通过水流或另一种液体在含水层多孔介质中被拖曳。分子速度 u=v/R,其中 v 是液体速度,R 是滞后因子。含水层由两个串联的一维层组成。两层之间的滞后因子或液体速度不同。对映体速度是对映体浓度的函数。该函数在两层中不同。对于模型参数的某些值,当进入含水层的分子对映体富集或介质手性时,两种层之间的界面处和一层中一种对映体的浓度增加,而另一种对映体的浓度降低。没有考虑对映体的合成和衰减。当对映体通过交替的液体流移动并且滞后因子与交替的液体流同步振荡时,可以获得所需的参数值。然后将模型的参数理解为一个振荡周期内的平均值。找到给出对映体静态浓度值的方程。通过数值求解两个非线性对流-扩散方程系统来确定对映体浓度的演化。所提出的机制可能在手生物质同手性的出现中发挥了作用。

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