Concrete alteration due to 55 years of exposure to river water: Chemical and mineralogical characterisation

Autor: Martin Rosenqvist, Manouchehr Hassanzadeh, Katja Fridh, Alexandra Bertron
Přispěvatelé: Laboratoire Matériaux et Durabilité des constructions (LMDC), Institut National des Sciences Appliquées - Toulouse (INSA Toulouse), Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées, Institut National des Sciences Appliquées (INSA)-Université de Toulouse (UT)-Institut National des Sciences Appliquées (INSA)-Université de Toulouse (UT)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)
Jazyk: angličtina
Rok vydání: 2017
Předmět:
Zdroj: Cement and Concrete Research
Cement and Concrete Research, Elsevier, 2017, 92, pp.110--120. ⟨10.1016/j.cemconres.2016.11.012⟩
Cement and Concrete Research, 2017, 92, pp.110--120. ⟨10.1016/j.cemconres.2016.11.012⟩
ISSN: 0008-8846
DOI: 10.1016/j.cemconres.2016.11.012⟩
Popis: This article presents a study on concrete alteration mechanisms due to 55 years of exposure to river water. Many hydro power structures in cold regions suffer from concrete deterioration at the waterline. Progressive disintegration of the concrete surface leads to exposure of the coarse aggregate and eventually the reinforcing steel. Concrete cylinders drilled out at four vertically different locations on the upstream face of a concrete dam were analysed by electron microprobe analysis, X-ray diffraction, thermogravimetry and scanning electron microscopy. Long-term exposure to the river water, which is regarded as soft water, has led to chemical and mineralogical zonation of the cement paste. Up to five zones with different chemical and mineralogical composition, parallel to the upstream face, were observed in the outermost 8–9 mm of the concrete. Decalcification, precipitation of secondary ettringite and the formation of a magnesium-rich silica gel constitute the major changes that define the zones.
Databáze: OpenAIRE