2017
DOI: 10.1016/j.conbuildmat.2017.01.079
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Collapsibility potential of gypseous soil stabilized with fly ash geopolymer; characterization and assessment

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Cited by 68 publications
(20 citation statements)
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“…At between higher wave numbers of 1600 cm -1 ,1751 cm -1 and 2762 cm -1 , 4000 cm -1 for both of S1F and S1FR two main broad peaks of 1651 cm -1 and 3622 cm -1 with low intensities of 2% were observed indicating stretching and deformation vibrations of OH and H-O-H groups from the weakly bound water molecules, which were adsorbed on the surface or trapped in the cavities between the framework bonds of the activated specimen. These observations were similar to those reported by plenty of researchers [7][8][9][10][11][12][13][14][15][16][17].…”
Section: Microstructural Analysessupporting
confidence: 92%
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“…At between higher wave numbers of 1600 cm -1 ,1751 cm -1 and 2762 cm -1 , 4000 cm -1 for both of S1F and S1FR two main broad peaks of 1651 cm -1 and 3622 cm -1 with low intensities of 2% were observed indicating stretching and deformation vibrations of OH and H-O-H groups from the weakly bound water molecules, which were adsorbed on the surface or trapped in the cavities between the framework bonds of the activated specimen. These observations were similar to those reported by plenty of researchers [7][8][9][10][11][12][13][14][15][16][17].…”
Section: Microstructural Analysessupporting
confidence: 92%
“…A strength increment rate of 1900% for specimen cured for 28 days was observed attaining a strength value of 3680 kPa for KSF40 followed by KSF30 with a UCS value at 2830 kPa, while the KSF10, KSF20 were exhibiting less UCS values at 1705 kPa, 1929 kPa respectively. This finding is in a line with results drawn by compressive testes carried out by many researches [15][16][17][18] who reached a conclusion that a proportional coloration between fly ash content and compressive strength values was recorded, which was attributed to the vitreous silica and alumina present in the precursor.…”
Section: Microstructuralsupporting
confidence: 91%
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“…This is attributed to the fact that the slow dissolution of Class F FA ultimately allows more time for the formation of a well-defined 3D structural bonding, responsible for the higher long-term strength gain reported (Cristelo et al [12]). Alsafi et al [18] and Liu et al [19] showed that soils stabilized with potassium hydroxide (KOH) activated Class F FA produced a higher degree of polymerization and compressive strength as compared to Class F FA samples activated using sodium hydroxide (NaOH) solution. Alsafi et al [18] stated that the advantage of KOH over NaOH was due to the K+ cation being larger in size as compared to Na+ cation which led to a significant increase in the degree of polymerization.…”
Section: Geopolymer Stabilizationmentioning
confidence: 99%
“…Given its pozzolanic properties, FA has been successfully used as an effective agent for chemical and mechanical stabilization of loess through modifying the particle size distribution, enhancement in bonding strength between particles, and destruction of its open structure [48,49]. Therefore, FA can improve soil density and plasticity and reduce water content and strength performance of loess; thus, FA has been used in treating loess soils by many researchers in recent years [50][51][52][53][54]. For example, Prabakar et al (2003) studied the influence of FA on strength behavior of three different types of soil by using different percentages of FA from 9% to 46% by weight of the soil [55].…”
Section: Introductionmentioning
confidence: 99%