最牛的反应

Hydrothermal Reactions from Sodium Hydrogen Carbonate to Phenol Ge Tian, Hongming Yuan, Ying Mu, Chao He, and Shouhua Feng* State Key Laboratory of Inorganic Synthesis and PreparatiVe Chemistry, College of Chemistry, Jilin UniVersity, Changchun, PRC shfeng@mail.jlu.edu.cn Received March 12, 2007 ABSTRACT We report here experimental evidence for the hydrothermal formation of a pure organic molecule, phenol, from the reaction of carbonate with water in the presence of iron powders. Exploration of the origin of life is one of the most fascinating and inspiring challenges in our age.1-3 The basic understand- ing of the origin of life initiated from the hydrothermal formation of organic molecules from the primitive atmo- spheric compositions of CH4, NH3, H2, CO2, and H2O.4 However, the information on how these organic molecules formed from the simplest inorganic molecules is still at a very beginning stage and defies clarity. Abiotic synthesis of organic compounds from CO2 under hydrothermal conditions has been proposed as a source of the precursor compounds from which life originated.5 It is well-known that modern volcanic gases contain mainly H2O and CO2. Recent research showed that the ingredients derived from volcanic outgassing were similar to those found in modern volcanic effluent, so it might be suggested that the primitive atmosphere around the time life originated was dominated by carbon dioxide.6 It has been proposed that CO2 is vented to the surface or atmosphere to be a carbon source and into the magma ocean or mantle to be sinks; the relevant sinks turned out to be carbonates such as CaCO3 or MgCO3 by the alteration of shallow rocks near the ambient ocean temperature.7,8 Sub- sequent reactions of CaCO3, MgCO3, and CO2 in the primeval water environments, producing amino acids or their fragments, must have a clear implication for the abiotic synthesis of complex organic molecules in the origin of life. On the other hand, the study on the fixation of CO2 converting into organic compounds is regarded as one of the most expected solutions for the “Greenhouse Effect” problem. To shed some light on the understanding of this pivotal initiative step, we studied the reactions of sodium hydrogen carbonate with water in the presence of iron powder based on the well-established mild hydrothermal method.9 Because sodium hydrogen carbonate can be translated into CO2, this simulates the ocean environments of the primordial earth in a certain geological time interval. The gas chromatography-mass spectroscopy (GC-MS) spectrum indicated that there were no detectable organic compounds in the starting purified sodium hydrogen carbon- ate, and the iron powder used in this experiment was also free of the contamination of the organic. Purified iron powder and sodium hydrogen carbonate were mixed with water and then added into a steel alloy autoclave (Fe-Cr-Ni alloy, GB1220-92) with a filling capacity of 90%. The mixture was then subjected to a hydrothermal treatment at 200 °C under autogenous pressure (approximate 1.8 MPa) for 5-120 h and then cooled to room temperature rapidly. The final pH (1) Miller, S. L. Science 1953, 117, 528. (2) Plankensteiner, K.; Reiner, H.; Schranz, B.; Rode, B. M. Angew. Chem., Int. Ed. 2004, 43, 1886. (3) Wa¨chterha¨user, G. Proc. Natl. Acad. Sci. U.S.A. 1990, 87, 200. (4) Huber, C.; Wa¨chterha¨user, G. Science 1997, 276, 245. (5) Huber, C.; Eisenreich, W.; Hecht, S.; Wa¨chterha¨user, G. Science 2003, 301, 938. (6) Mojzsis, S. J.; Arrhenius, G.; McKeegan, K. D.; Harrison, T. M.; Nutman, A. P.; Friend, C. R. L. Nature 1996, 384, 55. (7) Severin, K. Angew. Chem., Int. Ed. 2000, 39, 3589. (8) McCollom, T. M.; Seewald, J. S. Geochim. Cosmochim. Acta 2001, 65, 3769. (9) Feng, S.; Xu, R. Acc. Chem. Res. 2001, 34, 239. ORGANIC LETTERS 2007 Vol. 9, No. 10 2019-2021 10.1021/ol070597o CCC: $37.00 © 2007 American Chemical Society Published on Web 04/20/2007 value of the reaction solution was 9. GC-MS was employed to identify the products. It is quite evident that phenol was formed after the hydrothermal reactions, when the mass spectrum of the product was compared to that of standard phenol (Supporting Information, Figure S1). The peak at m/z 94 is assigned to the molecular ion, C6H6O+. Moreover, after the reaction, we found white deposition which was proved to be sodium carbonate by ICP on the bottom of the autoclave. It was noticed that the yield of phenol suddenly increases with the increase of reaction time, reaching a maximum value after 10 h, and then remains nearly constant. The yield of phenol in the hydrothermal reaction (1) is 0.8% mol according to NaHCO3. The effect of other metals and zeolites instead of iron powder under the same reaction conditions was taken into account, including Co and Ni powders, Fe3O4, Fe2+, Fe3+, Co2+, Ni2+-modified ZSM-5, MCM-41, MCM-48, H-â, and Na-Y zeolites, respectively, but none of them gave con- siderable reactions of phenol formation, although trace amounts of phenol could be harvested with the addition of Co and Ni powders. The hydrothermal reaction in the autoclave was checked by carrying out the hydrothermal reaction in N2 rather than in air, and we did not see an observable change either in the types of product or in the yield. Figure 1 shows the kinetic curve for the hydrothermal production of phenol. It is a typical self-catalysis reaction with a short induced period and fast formation reaction after the induced period. In the initial 5 h of reaction time, no organic molecules could be detected. Increasing the reaction time from 5 to 10 h, several organic molecules were identified by GC-MS, including the main product phenol and detectable amounts of formic acid and formaldehyde. The reactions completed after 10 h, and the final product was phenol only. It has been reported that methane was discovered at an East Pacific Rise hydrothermal vent and in other crustal fluids, which supports the occurrence of an abiogenic source of hydrocarbons.10 Usually, formation of abiogenic hydro- carbons by the reduction of carbon dioxide was thought to occur under hydrothermal conditions involving Fischer- Tropsch reactions and the serpentinization of ultramafic rocks.11,12 Generally, the products of this process were methanol, methane, and/or formate, which do not seem valuable for the origin of life. Organic synthesis based on CO2 was also studied.13 The production of phenol from solid CO2 reduced by Fe3O4 in the supercritical state was reported,14 but such reaction conditions are rigorous. More- over, in the case of supercritical CO2, the excessive water was considered to be unfavorable for the formation of phenol, which is fatal for the genesis of life under hydrothermal conditions. As a possible clue to searching for the origin of life, it would be important to prove that the reactions of sodium hydrogen carbonate with water happened hydro- thermally. It is noteworthy that the reactions could take place much more efficiently under the influence of iron powder rather than cobalt and nickel under the same reaction conditions. This clearly reflects the relatively large redox potential of iron (-0.44). The result of inductively coupled plasma (ICP) of the achieved solution shows 1% of Fe ions in weight, which confirms the existence of Fe2+ in the reaction solution, implying the occurrence of a redox reaction. The redox reaction involved the oxidization from Fe to Fe2+. On the basis of the observation of the final product phenol and intermittent formic acid and formaldehyde in the hydrothermal reactions, we propose a possible reaction mechanism for phenol formation. Scheme 1 illustrates the main process of the hydrothermal reactions (see details in Supporting Information, Scheme S1). At the first stage of the reactions, sodium hydrogen carbonate was converted to CO2 via its decomposition in hydrothermal solution. Sub- sequently, CO2 and/or CO32- were adsorbed and bound at the surface of metal iron. Meanwhile, metal iron reacted with water, giving H2 and Fe2+. At the surface of iron powder, CO2 could be activated to form formaldehyde (CH2O) finally with the attack of H2. The processes seem complicated but basically involve two simple types of reactions: the oxidative coupling reactions (denoted as 1) and rearrangement reac- tions (denoted as 2). We realized that the process of hydrogen production is the rate-determining step in the acceleration of the reactions because the reaction proceeds rapidly as soon as hydrogen is formed from the reaction of the metal iron with water. The fact that we caught trace formic acid and formaldehyde in the initial stage of the reaction confirms the suggested mechanisms. Water as the source of hydrogen is necessary in this reaction, whereas the ratio of NaHCO3 to water seems to have little effect on the reduction of carbon dioxide. From our accumulated (10) Lollar, B. S.; Westgate, T. D.; Ward, J. A.; Slater, G. F.; Lacrampe- Couloume, G. Nature 2002, 416, 522. (11) Sleep, N. H.; Zahnle, K.; Neuhoff, P. S. Proc. Natl. Acad. Sci. U.S.A. 2001, 98, 3666. (12) Horita, J.; Berndt, M. E. Science 1999, 285, 1055. (13) Amatore, C.; Jutand, A.; Khalil, F.; Nielsen, M. F. J. Am. Chem. Soc. 1992, 114, 7076. (14) Chen, Q.; Qian, Y. Chem. Commun. 2001, 1402. NaHCO3 + H2O f C6H5OH (1) Figure 1. Kinetic curve for the hydrothermal production of phenol. 2020 Org. Lett., Vol. 9, No. 10, 2007 experimental data, we may answer a key question: the abiotic synthesis of organic compounds from CO2 under hydrother- mal conditions can serve as a source of the precursor compounds from which life originated. It was apparently predicted that the final basic solution (pH ) 9) restricted the further reaction to form phenol because of the smaller conversion of CO2 and production of H2 in basic solution, in principle. According to our proposed mechanisms, we conducted the experiment in acidic solution where enough CO2 and H2 were allowed. Results showed that the yield of phenol dramatically increases. This experi- ment confirms our mechanisms and may also provide industrial possibilities. Our study on the hydrothermal reactions from sodium hydrogen carbonate to phenol makes it possible to form prebiotic organic molecules based on carbonate under mild hydrothermal conditions. Because of the hydrothermal formation of phenol which is a fragment of tyrosine, we understand that the existence of important small molecules such as formic acid and formaldehyde in the process of the reactions is basically the source for the hydrothermal formation of amino acids and peptides. One may believe that some of the possible subsequent reactions toward more complicated biomolecules would be expected. Acknowledgment. This work was supported by the Research Fund for the Creative Team of the National Nature Science Foundation of China (20121103). Supporting Information Available: Experimental pro- cedure, GC-MS characterization, and the formation mech- anisms of phenol. This material is available free of charge via the Internet at http://pubs.acs.org. OL070597O Scheme 1. Proposed Mechanism of Phenol Formation 1 Refers to the oxidative coupling reactions. 2 Refers to the rearrangement reactions. Org. Lett., Vol. 9, No. 10, 2007 2021