Magnetita (Fe3O4): Una estructura inorgánica con múltiples aplicaciones en catálisis heterogénea
Magnetite (Fe3O4): An inorganic structure with many applications for heterogeneous catalysis
Palabras clave:
magnetita, Fe3O4, catálisis, química verde, síntesis orgánica (es)magnetite, Fe3O4, catalysis, green chemistry, organic synthesis (en)
Se describió la intervención del mineral magnetita como catalizador o como soporte catalítico, un material inorgánico con una estructura de espinela inversa (FeFe2O4), en el desarrollo de un número importante de reacciones químicas de interés científico, tecnológico y ambiental. Debido a la necesidad actual de generar procesos químicos eficientes y favorables ambientalmente, la magnetita se ha convertido en un material promisorio en los contextos de la química verde, la química fina y la catálisis heterogénea. Este óxido de hierro se ha estudiado en diversas reacciones: catalizador másico, soporte catalítico de metales y de óxidos metálicos, núcleo de catalizadores tipo core-shell, o modificado mediante el anclaje de organocatalizadores y complejos metálicos. Se discute el desempeño catalítico de estos sistemas basados en magnetita, en reacciones de catálisis asimétrica, ambiental, ácido-base, de óxido-reducción, de síntesis multicomponente y de acoplamiento C-C. Particularmente, dichos catalizadores han mostrado enorme importancia en ciertas reacciones de tipo Sonogashira, Sonogashira–Hagihara, Mannich, Ullman, Knoevenagel, Suzuki-Miyaura y Fenton heterogénea, entre otras. Finalmente, se detallaron algunos usos tecnológicos de la magnetita en el contexto nacional (Colombia) y se intentó localizar geográficamente los depósitos importantes.
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