Rate controls on silicate dissolution in cementitious environments
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چکیده
منابع مشابه
Evidence for silicate dissolution on Mars from the Nakhla meteorite
Veins containing carbonates, hydrous silicates and sulphates that occur within and between grains of augite and olivine in the Nakhla meteorite are good evidence for the former presence of liquid water in the Martian crust. Aqueous solutions gained access to grain interiors via narrow fractures, and those fractures within olivine whose walls were oriented close to (001) were preferentially wide...
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ژورنال
عنوان ژورنال: RILEM Technical Letters
سال: 2017
ISSN: 2518-0231
DOI: 10.21809/rilemtechlett.2017.35