2021
DOI: 10.3389/fbuil.2021.640243
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Use Of Olivine For The Production Of MgO-SiO2 Binders

Abstract: The potential for using MgO and SiO2, recovered from olivine, was investigated for use as a cementitious binder system. The MgO to SiO2 proportion for the binder was fixed at 1:1. The nature of the hydration products were characterized using a variety of techniques including isothermal calorimetry, XRD, FTIR, and SEM. The primary binding component of the paste was determined to be magnesium silicate hydrate (M-S-H). The recovered silica exhibited faster reactivity compared to commercially available silica fume… Show more

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Cited by 6 publications
(2 citation statements)
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“…Also, the Si‐rich, Mg‐bearing amorphous phase detected only in weathered diopside samples could possibly be an amorphous magnesium silicate hydrate (M‐S‐H) secondary phase. Note that the broad band observed in the 3,000–4,000 cm −1 region of the IR spectra of the diopside sample after batch experiments (Figure S14 in Supporting Information ) can be associated with the asymmetrical stretching and bending vibrations of O‐H bonds, respectively, indicating presence of Mg‐OH and/or Fe‐OH vibrations (Nye et al., 2021). Formation of M‐S‐H phases has been reported in numerous scenarios (Roosz et al., 2015 and refs therein), including some related to the alteration of silicate materials (e.g., cement and borosilicate glass) (Dauzeres et al., 2016; De Weerdt & Justnes, 2015; de Ruiter and Austrheim, 2017) and during the injection of CO 2 ‐charged water into basalt (CarbFix project), where the predominant secondary mineral formed was a Mg‐Fe‐rich silicate phase (Oelkers et al., 2019).…”
Section: Discussionmentioning
confidence: 99%
“…Also, the Si‐rich, Mg‐bearing amorphous phase detected only in weathered diopside samples could possibly be an amorphous magnesium silicate hydrate (M‐S‐H) secondary phase. Note that the broad band observed in the 3,000–4,000 cm −1 region of the IR spectra of the diopside sample after batch experiments (Figure S14 in Supporting Information ) can be associated with the asymmetrical stretching and bending vibrations of O‐H bonds, respectively, indicating presence of Mg‐OH and/or Fe‐OH vibrations (Nye et al., 2021). Formation of M‐S‐H phases has been reported in numerous scenarios (Roosz et al., 2015 and refs therein), including some related to the alteration of silicate materials (e.g., cement and borosilicate glass) (Dauzeres et al., 2016; De Weerdt & Justnes, 2015; de Ruiter and Austrheim, 2017) and during the injection of CO 2 ‐charged water into basalt (CarbFix project), where the predominant secondary mineral formed was a Mg‐Fe‐rich silicate phase (Oelkers et al., 2019).…”
Section: Discussionmentioning
confidence: 99%
“…In summary, the use of magnesium silicate minerals offers a potentially low carbon method to produce globally significant quantities of MgO. It should be noted that in addition to MgO, the mineral recovery process also generates a highly reactive silica that can be used along with the MgO to form an effective cement [35].…”
Section: Mgo From Mg-silicatesmentioning
confidence: 99%