
handle: 10261/161060
Estudios mineralógicos y microtexturales revelan el carácter nocivo de las rocas opalinas utilizadas como áridos para el hormigón, observándose la neoformación de silicatos complejos que generan importantes presiones disruptivas en el seno del hormigón. Calicinita, zeolitas y geles silico-calcicos-alcalinos son las fases silíceas que pueden llevar a la destrucción del hormigón.
Centro de Estudios y Experimentación de Obras Públicas (MOPU)
Peer reviewed
Opalos, Hormigón, Reacción álcali-árido, Áridos
Opalos, Hormigón, Reacción álcali-árido, Áridos
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