January 2008
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184 Reads
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21 Citations
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... Magnesium-silicate gel This gel occurs as a narrow rim in the place of brucite on the inner periphery of dolomite crystals, as a result of the reaction between brucite (or its gel) in dedolomitisation and cryptocrystalline quartz (or ASG) present nearby (Figure 2(c)). Magnesium-silicate gel has been reported from dolomitic aggregates in field concretes in Ontario (Katayama, 2004(Katayama, , 2006(Katayama, , 2010a(Katayama, , 2011, Quebec (Katayama, 2006), Japan (Katayama et al., 2008), Saudi Arabia (Katayama and Grattan-Bellew, 2012) and in Austrian aggregates in concrete microbar (Katayama, 2004). Unlike the ASR gel, magnesiumsilicate gel does not seem to expand. ...
- Citing Article
January 2008