Abstract
Formation de H 2 a >395 nm dans une argile naturelle (bentonite) en suspension en presence de Ru(bpy) 2+ , MV 2+ et d'agregat [n-Bu 4 N] [Fe 4 S 4 (SPh) 4 ] dans l'ethanolamine. L'agregat est preadsorbe par l'argile
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