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Abiotic ammonium formation in the presence of Ni-Fe metals and alloys and its implications for the Hadean nitrogen cycle

机译:Ni-Fe金属和合金存在下非生物铵的形成及其对哈代氮循环的影响

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摘要

Experiments with dinitrogen-, nitrite-, nitrate-containing solutions were conducted without headspace in Ti reactors (200°C), borosilicate septum bottles (70°C) and HDPE tubes (22°C) in the presence of Fe and Ni metal, awaruite (Ni_(80)Fe_(20)) and tetrataenite (Ni_(50)Fe_(50)). In general, metals used in this investigation were more reactive than alloys toward all investigated nitrogen species. Nitrite and nitrate were converted to ammonium more rapidly than dinitrogen, and the reduction process had a strong temperature dependence. We concluded from our experimental observations that Hadean submarine hydrothermal systems could have supplied significant quantities of ammonium for reactions that are generally associated with prebiotic synthesis, especially in localized environments. Several natural meteorites (octahedrites) were found to contain up to 22 ppm N_(tot). While the oxidation state of N in the octahedrites was not determined, XPS analysis of metals and alloys used in the study shows that N is likely present as nitride (N~(3-)). This observation may have implications toward the Hadean environment, since, terrestrial (e.g., oceanic) ammonium production may have been supplemented by reduced nitrogen delivered by metal-rich meteorites. This notion is based on the fact that nitrogen dissolves into metallic melts.
机译:在含Fe和Ni金属,钙矾石(Ni_(80)Fe_(20))和四方晶石(Ni_(50)Fe_(50))。通常,在本次调查中使用的金属对所有被调查的氮物种的反应性均比合金高。亚硝酸盐和硝酸盐比二氮更快地转化为铵盐,还原过程对温度的依赖性强。我们从实验观察得出的结论是,哈代海底热液系统可能已经为通常与益生元合成相关的反应提供了大量的铵,特别是在局部环境中。发现几种天然陨石(八面体)的N_(tot)含量高达22 ppm。虽然不确定八面体中N的氧化态,但研究中使用的金属和合金的XPS分析表明,N可能以氮化物(N〜(3-))的形式存在。该观察结果可能对哈代环境有影响,因为陆地(例如海洋)铵的生产可能已被富含金属的陨石所输送的氮减少所补充。该概念基于氮溶解到金属熔体中的事实。

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