2020
DOI: 10.1016/j.clay.2020.105672
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High-pH/low pH ordinary Portland cement mortars impacts on compacted bentonite surfaces: Application to clay barriers performance

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Cited by 15 publications
(4 citation statements)
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“…Visual observation of the tablets during the dissolution test (Fig. 6) indicated that bentonite forms a gel structure in dissolution media at pH 7.2, whereas the tablets disintegrated at less acidic pH values, which could be related to the dissolution of montmorillonite at low pH and itself was responsible for gel-building in bentonite (Bendou & Amrani, 2014; Mouzon et al , 2016; Alkrad et al , 2017; González-Santamaría et al , 2020).
Fig.
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Section: Discussionmentioning
confidence: 99%
“…Visual observation of the tablets during the dissolution test (Fig. 6) indicated that bentonite forms a gel structure in dissolution media at pH 7.2, whereas the tablets disintegrated at less acidic pH values, which could be related to the dissolution of montmorillonite at low pH and itself was responsible for gel-building in bentonite (Bendou & Amrani, 2014; Mouzon et al , 2016; Alkrad et al , 2017; González-Santamaría et al , 2020).
Fig.
…”
Section: Discussionmentioning
confidence: 99%
“…Secondly, the saturated bentonite can support and suspend the large particle aggregate, which is precipitated and separated downward in the slurry, so that the particle distribution of the slurry is more uniform, and the strength and permeability of the cured backfill will be improved. In addition, we believe that the microbead effect of bentonite and fly ash fine particles can improve the bonding force between slurry particles [44]. When bentonite is moistened and expanded, its particles will attract one another and form a binding water film when they contact the surface of gangue/tailings particles [45].…”
Section: Bleeding Ratementioning
confidence: 99%
“…Although Ordinary Portland cement (OPC) is the most common cementitious material, its pore solution has a pH > 12.5, potentially forming a hyper-alkaline plume due to groundwater percolation. The contact of a hyper-alkaline plume with buffer materials, such as compacted bentonite, that surround cementitious materials may lead to the alkaline alteration of these materials, which may cause the dissolution of minerals [2][3][4][5][6] and/or secondary mineral formation to occur [4][5][6][7][8][9]. These phenomena may change the permeability of barrier materials and affect the long-term performance of the repository.…”
Section: Introductionmentioning
confidence: 99%