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Formamide Dehydration and Condensation on Acidic Montmorillonite: Mechanistic Insights from Ab-Initio Periodic Simulations

机译:酸性蒙脱土的甲酰胺脱水和缩合:AB-Initio周期性模拟的机械洞察

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Formamide (NH_2CHO) is a molecule of extraordinary relevance as prebiotic precursor of many biological building blocks. Its dehydration reaction, which could take place during the Archean Era, leads to the production of HCN, the fundamental brick of DNA/RNA nitrogenous bases. Mineral surfaces could have played a crucial role in activating biological processes which in gas phase would have too high activation barriers to occur, thus allowing the event cascade, which finally led to the formation of biological macromolecules. In the present work we studied the dehydration process of formamide (NH_2CHO → HCN + H_2O) as catalyzed by a surface of acid montmorillonite. In this surface, a silicon atom has been substituted by an aluminium one, thus generating a negative charge that is compensated by an acidic proton on the top of the surface. This proton should, in principle, help the formamide dehydration. However, our results indicate that this particular acidic surface does not exert an efficient catalytic behavior in the decomposition of formamide.
机译:甲酰胺(NH_2CHO)是作为许多生物构建块的益生元前体的非凡相关的分子。它可以在Archean时代发生的脱水反应导致HCN的生产,DNA / RNA含氮基础的基本砖。矿物表面可能在激活的生物过程中发挥了至关重要的作用,该生物过程在气相中具有太高的活化屏障,从而允许事件级联,这最终导致形成生物大分子。在本工作中,我们研究了由酸蒙脱石表面催化的甲酰胺(NH_2CHO→HCN + H_2O)的脱水过程。在该表面上,硅原子已被铝代替,因此产生由表面顶部的酸性质子补偿的负电荷。原则上,该质子应该帮助甲酰胺脱水。然而,我们的结果表明,该特定的酸性表面在甲酰胺的分解中不发挥有效的催化行为。

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