Estudio microestructural de productos de reacción álcali-árido en hormigones curados a alta temperatura
DOI:
https://doi.org/10.3989/mc.1993.v43.i232.664Abstract
La degradación del hormigón, debida a la reacción expansiva llamada "reacción álcali-árido", ha sido ampliamente estudiada (1) y (2). Este fenómeno es especialmente relevante en países como Estados Unidos, Canadá, Brasil, etc., donde hay una gran cantidad de áridos con sílice reactiva.
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