Fuentes, el reventón energético

Vol. 22 Núm. 1 (2024): Fuentes, el reventón energético
Artículos

EFECTO DE LAS DISPERSIONES ACUOSAS DE ÓXIDO DE GRAFENO SOBRE LA HUMECTABILIDAD DE LAS ROCAS

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  • José Carlos Cárdenas,
  • Angelli Stephanie Pérez,
  • Rodrigo Torres Saez,
  • Emiliano Ariza León
José Carlos Cárdenas
Instituto Colombiano del Petróleo-ICP
Angelli Stephanie Pérez
Instituto Colombiano del Petróleo-ICP
Rodrigo Torres Saez
Instituto Colombiano del Petróleo-ICP
Emiliano Ariza León
Universidad Industrial de Santander
DOI: https://doi.org/10.18273/revfue.v22n1-2024002

Publicado 2024-04-12

Palabras clave

  • Modificador de Permeabilidad,
  • Mojabilidad de Rocas,
  • Óxido de Grafeno

Cómo citar

Cárdenas, J. C. ., Pérez, A. S. ., Torres Saez, R. ., & Ariza León, E. (2024). EFECTO DE LAS DISPERSIONES ACUOSAS DE ÓXIDO DE GRAFENO SOBRE LA HUMECTABILIDAD DE LAS ROCAS. Fuentes, El reventón energético, 22(1), 21–34. https://doi.org/10.18273/revfue.v22n1-2024002
Creative Commons License

Esta obra está bajo una licencia internacional Creative Commons Atribución 4.0.

Resumen

Entre los diversos métodos para mejorar la recuperación de petróleo de los yacimientos (estimulación de pozos), el uso de nanofluidos ha surgido como una alternativa prometedora para modificar la mojabilidad y permeabilidad de las rocas de arenisca. Por esta razón, en este estudio, se sintetizó óxido de grafeno (GO) a partir de grafito y se formuló un nanofluido utilizando GO disperso en agua para evaluar su capacidad para modificar la mojabilidad en núcleos de arenisca de yacimientos colombianos. El montaje experimental incluyó tres pruebas preliminares: mojabilidad visual, mediciones del ángulo de contacto y detergencia. Los resultados demostraron un aumento en la mojabilidad al agua de las rocas, lo que llevó a una disminución del ángulo de contacto del sistema agua-roca de hasta un 42.6%. Además, las pruebas de mojabilidad visual y detergencia arrojaron resultados positivos, indicando que el óxido de grafeno es un modificador efectivo de la mojabilidad, haciendo que la roca sea más mojada por agua.

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