Schoonen M A, Xu Y
Department of Geosciences, State University of New York-Stony Brook, Stony Brook, NY 11794-2100, USA.
Astrobiology. 2001 Summer;1(2):133-42. doi: 10.1089/153110701753198909.
Dinitrogen is reduced in dilute hydrogen sulfide (H2S) solutions to ammonium at 120 degrees C. Experiments with dissolved dinitrogen (partial pressure 50 bar) in a 12 x 10(-3) mol/L H2S(aq) solution yield approximately 10(-5) mol/L NH4+ within 2-7 days. These yields are consistent with the equilibrium NH4+ concentration for the N-S-H system under these conditions. The formation of ammonium is catalyzed by the presence of freshly precipitated iron monosulfide. These results indicate that dinitrogen can be reduced at moderate temperatures in hydrothermal vent systems. Abiotic nitrogen reduction could have taken place within primordial hydrothermal vents, supplying some ammonia for the synthesis of C-H-O-N compounds via abiotic processes. The yield of ammonia via dinitrogen reduction by hydrogen sulfide, however, is so low that it is doubtful this process could have produced enough ammonia to sustain prebiotic hydrothermal synthesis of C-H-O-N compounds in or around vent systems.
在120摄氏度下,二氮在稀硫化氢(H₂S)溶液中被还原为铵。在12×10⁻³mol/L的H₂S(水溶液)溶液中,对溶解的二氮(分压50巴)进行实验,在2至7天内产生约10⁻⁵mol/L的NH₄⁺。这些产量与这些条件下N-S-H系统的平衡NH₄⁺浓度一致。新鲜沉淀的硫化亚铁的存在催化了铵的形成。这些结果表明,在热液喷口系统中,二氮可以在中等温度下被还原。在原始热液喷口内可能发生了非生物固氮,通过非生物过程为C-H-O-N化合物的合成提供了一些氨。然而,通过硫化氢还原二氮产生氨的产量非常低,以至于怀疑这个过程是否能产生足够的氨来维持喷口系统内或周围C-H-O-N化合物的益生元热液合成。