Análisis por resonancia magnética nuclear del deterioro en hormigón con piedra pómez tras ciclos hielo-deshielo
DOI:
https://doi.org/10.3989/mc.2016.09014Palabras clave:
Hormigón de piedra pómez natural, Propagación de daños, Resonancia magnética nuclear (RMN), Porosidad, Tiempo de relajaciónResumen
En este trabajo se analiza la propagación de los daños que se producen en la estructura porosa de hormigón aligerado a base de piedra pómez natural sometido a la acción cíclica de hielo-deshielo. Después de realizarse los ensayos de hielo-deshielo, el hormigón se analizó mediante resonancia magnética nuclear (RMN), determinándose la porosidad y la distribución del tiempo de relajación transversal, T2, y registrándose las imágenes captadas por resonancia magnética. De acuerdo con los resultados obtenidos, antes de los ciclos de hielo-deshielo la distribución de T2 del hormigón aligerado presentaba cuatro picos, indicativos de un predominio de poros pequeños. Después de que se sometiera a 50, 100, 150, y 200 ciclos, se observó un aumento importante tanto de la porosidad como de la superficie total del espectro de T2. Las imágenes captadas por resonancia magnética evidenciaron la modificación de la distribución espacial de los poros del hormigón aligerado durante el ensayo. Por otra parte, mediante la comprobación por técnicas de prospección ultrasónica se confirmó que la nueva tecnología RMN es de alta precisión y gran practicidad en la investigación de los daños producidos en el hormigón por los ciclos de hielo-deshielo.
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