2012
DOI: 10.4067/s0718-915x2012000100005
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Activación térmica de bentonitas para su utilización como puzolanas

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Cited by 8 publications
(10 citation statements)
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“…Figure 1 shows the X-ray diffraction pattern obtained for the natural pozzolan (NP), where several common minerals can be identified, such as quartz (SiO 2 ), anorthite (Ca(Al 2 Si 2 O 8 )), cordierite (Mg 2 (Al 4 Si 5 O 18 )) and montmorillonite (Na,Ca) 0,3 (Al,Mg) 2 (Si 4 O 10 (OH) 2X H 2 O) plagioclases. The latter, part of the smectite family of the phyllosilicate mineral group, exhibited the highest water adsorption among the clay minerals due to its laminar structure and the charge distribution patterns inside its structure (20). To reduce the demand of water in the geopolymer material, it was necessary to calcine the material at 700 °C, which was performed at a heating rate of 14 °C/min and maintained for 15 minutes.…”
Section: Methodsmentioning
confidence: 99%
“…Figure 1 shows the X-ray diffraction pattern obtained for the natural pozzolan (NP), where several common minerals can be identified, such as quartz (SiO 2 ), anorthite (Ca(Al 2 Si 2 O 8 )), cordierite (Mg 2 (Al 4 Si 5 O 18 )) and montmorillonite (Na,Ca) 0,3 (Al,Mg) 2 (Si 4 O 10 (OH) 2X H 2 O) plagioclases. The latter, part of the smectite family of the phyllosilicate mineral group, exhibited the highest water adsorption among the clay minerals due to its laminar structure and the charge distribution patterns inside its structure (20). To reduce the demand of water in the geopolymer material, it was necessary to calcine the material at 700 °C, which was performed at a heating rate of 14 °C/min and maintained for 15 minutes.…”
Section: Methodsmentioning
confidence: 99%
“…The results in Table 6 indicate that the treated clay has a higher surface area, therefore it is expected to be more re- active and, in addition, to have a higher average pore size. As some authors have shown, the reactivity of calcined samples is related to their specific surface: the larger the surface, the greater the reactivity (22). Figure 4 shows the radius of the pores against their accumulated volume for clays.…”
Section: Porosimetry and Surface Areamentioning
confidence: 96%
“…The increase in porosity (average size and volume) and in the specific surface area occurs due to the fact that the thermal treatment produces a deterioration of the montmorillonite sheets and that when the interlaminar water is released in the form of vapor, the structure widens and this in turn causes disorder in the structure (22).…”
Section: Porosimetry and Surface Areamentioning
confidence: 99%
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