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and Photostimulated Heterogeneous synthesize organic species in Interstellar Space on the Reactions in the and in the surface of particles (as they were on primitive ). Primitive Earth’s Atmosphere. Some peculiar features of heterogeneous photocatalytic Relevance to the Genesis of systems, namely (i) the considerable red shift of the spectral range of a given photoreaction compared with N. Serpone,1, 2 A. Emeline,1 V. Otroshchenko,3 one in homogeneous and (ii) the effect of spectral and V. Ryabchuk 4 selectivity of photocatalysts (5), favor the synthesis of 1 Department of & , Concordia organic substrates under the above-mentioned natural University, Montreal (QC), Canada H3G 1M8. conditions. The first feature utilizes a considerably larger 2 Dipartimento di Chimica Organica, Universita di Pavia, fraction of Solar than is otherwise possible in Pavia, Italia. homogeneous photochemical reactions. The second 3 Bach Institute of Biochemistry, Russian Academy of feature influences the dependence of the relative chemical Sciences, Moscow, Russia. yields of different products of a given reaction on the 4 Department of , University of St.-Petersburg, of the actinic radiation. In particular, the St. Petersburg 198504, Russia. products of complete and partial oxidation of and other result principally from the Studies of micrometeoritic particles captured by Earth of - photocatalysts in the (i.e. ) absorption bands (strong at different geological times and discovered in Antarctica fundamental intrinsic have deduced that many organic substances necessary for absorption of UV and of blue ). More complex the Origin of Life on Earth are synthesized in Interstellar organic compounds are formed under irradiation of the catalysts in the absorption bands (weak to Space and are subsequently transported to Earth by extrinsic , , and (1). Over 120 types moderate absorption of red light). The latter peculiarity of of have been identified in interstellar dust / dust cloud-like heterogeneous systems makes clouds in the last three decades. Most organic molecules them similar to what takes place in the (modern) Earth’s contain more than 10 . Phosphorous- atmosphere in which the layer protects the containing molecules {e.g. PN}, CN, HCHO, cyano- Biosphere from destruction by UVC radiation (i.e. and others are the molecular precursors of radiation below 290 nm). biologically important substances (2). Evidently, a cosmic Solid particles of the photocatalyst can store energy of dust particle provides a logical reactor surface on which irradiation through formation of trapped photoelectrons to synthesize organic species in open Interstellar Space. and photoholes at the surface and in the bulk of the solid, The same holds for the dust particles in the primitive as well as through promotion of surface chemical Earth’s atmosphere. Solar and cosmic electromagnetic reactions under additional thermal or long wavelength UV/visible radiations are excellent sources of free energy photoexcitation (6). Such particles also serve to adsorb needed to drive the abiogenic synthetic process to produce molecules and radicals (at sufficiently low temperatures). organic molecules (3). Such processes find equivalence in Indeed, both atmospheric and cosmic dust particles are heterogeneous photochemical reactions that belong to a suitable vehicles that permit different stages of class of processes in heterogeneous (4). heterogeneous photoreactions (pre- of , In its most simplistic format, heterogeneous photo- photoexcitation of catalyst, chemical transformation on can be described briefly and simply as the particle surface, and desorption of reaction products) to be separated in time and space at different locations of A + Cat + light à B + Cat [1] the interstellar medium (7). This likely occurred also in the primitive Earth’s atmosphere. where A and B are chemical reagents and products, respectively, in the gaseous or phase, and Cat Acknowledgments denotes the solid photocatalyst. Thus, heterogeneous We thank the Natural Sciences and Engineering photocatalysis represents the generalization of thermal Research Council of Canada for support of our work in (acceleration of a process with Montreal. conservation of the catalyst Cat) and References (involvement of free energy in the catalytic process). 1. K.L. Brinton, C. Engrand, D.P. Glavin, J.L. Bada, and When the in [1] is not complete (i.e. when M.A. Maurette, Origins Life Evol. Biosphere, 28, 413 Cat is not restored), the process is best referred to as a (1998). heterogeneous photochemical stoichiometric reaction. 2. P. Ehrenfreund and S.B. Charnley, Ann. Rev. Astron. It is now well established that of different Astrophys., 38, 1 (2000). (e.g., metal , halides, sulfides, and complex natural 3. V.A. Otroshchenko, M.S. Kritsky, N.V. Vasilyeva, ) can serve as effective photocatalysts. Different V.A. Alekseev, V. Ryabchuk, and R.R. Bagautdinov, types of reactions, including reactions that lead to 12ème Rencontres de Blois, Château de Blois, June 25- formation of multi-carbon compounds (e.g. formation of July 1, 2000, Frontiers of Life (in press 2002). , and ethylene from methane), take place at 4. N. Serpone, A. Salinaro, A. Emeline, V. Ryabchuk, J. the surface of solid photocatalyst particles under Photochem. Photobiol. A:Chem., 130, 83 (2000). illumination. Quantum yields are typically around 0.1 and 5. A. Emeline, V. Ryabchuk, and N. Serpone, J. Phys. reach unity in some systems. The heterogeneous Chem. B, 103, 1316 (1999). photoreactions take place in a wide range of temperatures 6. A. Emeline, G.V. Kataeva, V. Ryabchuk, and N. (from ~77 K to ca. 500 K) and in a wide range of gas Serpone, J. Phys. Chem. B, 103, 9190 (1999). that includes the zero limit. In the latter 7. A. Emeline, V. Otroshchenko, V. Ryabchuk, and N. case, reactions occur between reagents pre-adsorbed on Serpone, J. Photochem. Photobiol. C:Revs., in press. solid surfaces at sufficiently low temperatures. Accordingly, we infer that appropriate conditions exist to