2020
DOI: 10.3390/molecules25051220
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Natural Mordenite from Spain as Pozzolana

Abstract: This work deals with anomalous concentrations of natural mordenite in the southeast of Spain. The X-ray diffraction (XRD) and scanning electron microscopy (SEM) studies evidenced that the samples contain mainly monomineral zeolitic phase of mordenite (70% to 74%), usually accompanied by smectite (montmorillonite), the principal component of bentonite. A study of the applicability of these zeolites is presented to establish the potential use as pozzolanic cements. For comparative purposes, synthetic commercial … Show more

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Cited by 9 publications
(10 citation statements)
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References 19 publications
(19 reference statements)
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“…The coexistence of both mineral phases seems to reinforce their syngenetic origin from the devitrification of volcanic glass, as can be seen in Figure 2c. Costafreda [34] and later Presa et al [35] have described this allochemical process on several occasions, and this fact significantly reinforces what is stated in this research.…”
Section: Scanning Electron Microscopy (Sem)supporting
confidence: 90%
“…The coexistence of both mineral phases seems to reinforce their syngenetic origin from the devitrification of volcanic glass, as can be seen in Figure 2c. Costafreda [34] and later Presa et al [35] have described this allochemical process on several occasions, and this fact significantly reinforces what is stated in this research.…”
Section: Scanning Electron Microscopy (Sem)supporting
confidence: 90%
“…As can be seen, this figure represents the concentration of saturation in calcium ions as a function of the concentration of hydroxyl ions in a solution at 40 • C. According to this diagram, the zeolites of the study area have a marked pozzolanic behaviour. This fact could be provoked by the high crystallinity of the silica in the zeolites analysed; similar results have been presented by Machiels et al [28], Costafreda et al [29] and Presa et al [30]. The amorphous silica favours even more the pozzolanic reactivity, as has been established by Mirzahosseini and Riding [31].…”
Section: Results Of the Eight-day Pozzolanicity Analysis To Determine The Pozzolanic Reactivity Of The Samplessupporting
confidence: 77%
“…In addition to mordenite, the smectite (montmorillonite), muscovite, plagioclase, halloysite, gypsum, quartz, and devitrified volcanic glass representing the amorphous phase was detected. According to the information offered in Figure 4b,c,g, it follows that zeolitic mineralization occurred from the hydrothermal alteration of the amorphous phase; this reasoning is also reflected in the work of Presa et al [10]. A fact worth mentioning is the abundance of mordenite even at the deepest levels of the Los Frailes Caldera.…”
Section: Scanning Electron Microscopy (Sem)mentioning
confidence: 54%
“…According to Arribas [1] Los Frailes Caldera is a circular volcanic structure which is approximately 5 km in diameter, which was formed 14.4 ± 0.8 ma ago because of eruptive processes of several pyroclastic flows of dacitic and andesitic composition. At the same time, Benito et al [6], Costafreda [7], Costafreda and Martin [8], Costafreda et al [9], Presa et al [10], and Stamatakis et al [11] have recently investigated and described minerals and industrial rocks inside Los Frailes Caldera, consisting of strongly zeolitized and bentonitized cineritic tuffs (ZBT) and glassy volcanic tuffs (GVT), to be used in the production of pozzolanic cements, mortars, concretes, and as light aggregates for concrete. Other researchers [12][13][14] have focused their research on the bentonite deposits of the Los Frailes Caldera and surrounding distal areas.…”
Section: Introductionmentioning
confidence: 99%