January 20, 2014 report
Researchers find reactions occur faster in micro-droplets
The research by the team is part of an effort to try to learn how it was that life here on Earth came to be—likely as part of some unknown chemical reaction. To that end, they wondered if perhaps such reactions might have been more likely if they occurred in a more constricted space. Others have suggested that life may have gotten its start in micro-droplets of water after they evaporated from the ocean or other sources. To find out if such an idea might be plausible, the researchers tried to mimic conditions that existed on our prebiotic planet.
They chose two molecules—an aldehyde and an amine —taken alone they are not florescent—when they meet, though, a reaction occurs causing the formation of a molecule that is: a fluorescent imine. They conducted several experiments whereby the two molecules were allowed to meet and react in different sized liquid environments—from standing pools of water to micro-droplets. To measure how fast the reaction took place, the team measured how quickly the mix turned fluorescent. They report that the reactions occurring in the micro-droplets ran as fast as forty five times as fast as the reactions occurring in standing water.
To explain what they had observed, the team created a mathematical model that allows for manipulating volume size versus surface area of the environment. The model suggests that reactants in a small liquid volume where there is a relatively large surface area, provide an opportunity for the creation of larger molecules. That, the researchers suggest, might help explain how larger molecules (such as those that eventually led to something that was alive) could form from smaller ones during the time when life was beginning to emerge. Notable is that their experiments show that evaporation may not have been part of that process.
The team plans to next study multi-step reaction times in confined spaces.
A bimolecular synthetic reaction (imine synthesis) was performed compartmentalized in micrometer-diameter emulsion droplets. The apparent equilibrium constant (Keq) and apparent forward rate constant (k1) were both inversely proportional to the droplet radius. The results are explained by a noncatalytic reaction-adsorption model in which reactants adsorb to the droplet interface with relatively low binding energies of a few kBT, react and diffuse back to the bulk. Reaction thermodynamics is therefore modified by compartmentalization at the mesoscale—without confinement on the molecular scale—leading to a universal mechanism for improving unfavorable reactions.
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