Department of Chemistry, Temple University, Philadelphia, PA 19122, USA.
Orig Life Evol Biosph. 2012 Aug;42(4):275-94. doi: 10.1007/s11084-012-9271-8. Epub 2012 May 6.
An important constraint on the formation of the building blocks of life in the Hadean is the availability of small, activated compounds such as ammonia (NH(3)) relative to its inert dinitrogen source. Iron-sulfur particles and/or mineral surfaces have been implicated to provide the catalytic active sites for the reduction of dinitrogen. Here we provide a combined kinetic, spectroscopic, and computational modeling study for an alternative source of ammonia from water soluble nitrogen oxide ions. The adsorption of aqueous nitrite (NO(2)(-)) and nitrate (NO(3)(-)) on pyrite (FeS(2)) and subsequent reduction chemistry to ammonia was investigated at 22°C, 70°C, and 120°C. Batch geochemical and in situ Attenuated Total Reflection - Fourier Transform Infrared (ATR-FTIR) spectroscopy experiments were used to determine the reduction kinetics to NH(3) and to elucidate the identity of the surface complexes, respectively, during the reaction chemistry of NO(2)(-) and NO(3)(-). Density functional theory (DFT) calculations aided the interpretation of the vibrational data for a representative set of surface species. Under the experimental conditions used in this study, we detected the adsorption of nitric oxide (NO) intermediate on the pyrite surface. NH(3) production from NO(2)(-) occurred at 70 and 120°C and from NO(3)(-) occurred only at 120°C.
在冥古宙时期,生命构建模块的形成受到重要限制,因为相对其惰性氮源而言,可供使用的小型活性化合物(如氨(NH3))数量较少。铁硫颗粒和/或矿物表面被认为是为氮气还原提供催化活性位点的物质。在这里,我们提供了一项关于水可溶性氮氧化物离子替代氨源的联合动力学、光谱和计算建模研究。在 22°C、70°C 和 120°C 下,研究了水合亚硝酸盐(NO2-)和硝酸盐(NO3-)在黄铁矿(FeS2)上的吸附以及随后的还原化学过程至氨。批处理地球化学和原位衰减全反射 - 傅里叶变换红外(ATR-FTIR)光谱实验分别用于确定 NH3 的还原动力学和阐明 NO2-和 NO3-反应化学过程中表面络合物的身份。密度泛函理论(DFT)计算有助于解释代表一系列表面物种的振动数据。在本研究中使用的实验条件下,我们检测到在黄铁矿表面吸附一氧化氮(NO)中间体。NO2-在 70 和 120°C 时产生 NH3,而 NO3-仅在 120°C 时产生 NH3。