2016
DOI: 10.3390/ma9070580
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Optimizing and Characterizing Geopolymers from Ternary Blend of Philippine Coal Fly Ash, Coal Bottom Ash and Rice Hull Ash

Abstract: Geopolymers are inorganic polymers formed from the alkaline activation of amorphous alumino-silicate materials resulting in a three-dimensional polymeric network. As a class of materials, it is seen to have the potential of replacing ordinary Portland cement (OPC), which for more than a hundred years has been the binder of choice for structural and building applications. Geopolymers have emerged as a sustainable option vis-à-vis OPC for three reasons: (1) their technical properties are comparable if not better… Show more

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Cited by 47 publications
(28 citation statements)
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“…For every 1 kg of fly ash–fiber mixture, 400 g of alkaline activator (well-mixed 80% water glass solution, 20% 12 M NaOH by weight) was added gradually while mixing using a laboratory motorized mixer. The mass ratio was chosen to achieve a geopolymer mix with considerable compressive strength and good workability [39]. Mixing was continued for about 15 min until the mixture appeared homogenous.…”
Section: Methodsmentioning
confidence: 99%
“…For every 1 kg of fly ash–fiber mixture, 400 g of alkaline activator (well-mixed 80% water glass solution, 20% 12 M NaOH by weight) was added gradually while mixing using a laboratory motorized mixer. The mass ratio was chosen to achieve a geopolymer mix with considerable compressive strength and good workability [39]. Mixing was continued for about 15 min until the mixture appeared homogenous.…”
Section: Methodsmentioning
confidence: 99%
“…X-ray diffractograms of the rice hull ash discovered the presence of a low quantity of crystalline phase of cristobalite-SiO 2 in mainly amorphous materials. Geopolymers were formed from the rice hull ash and other amorphous alumino-silicate materials by alkaline activation [19]. The rice hull ash composition was found as SiO 2 70.1%; K 2 O 1.10% and CaO 0.19% by mass.…”
Section: Discussionmentioning
confidence: 99%
“…Figure 7c,d shows morphologies after FA carbonization, which has the "cubic-like" structures of calcite ( Figure 7c) and "needle-like" structures of aragonite ( Figure 7d). In addition, FA particles are reported to be globular and irregular with high porosity [58], glassy cenospheres [59,60], spherical-shaped and flake-like particles [61,62], spherical particles of varying sizes and particles of unburned coal [59,63,64], and predominantly spherical in shape and consisting of solid spheres, cenospheres, irregular-shaped debris and porous unburnt carbon [15]. In Figure 8, the FA particles are mainly spherical, consisting of solid spheres, cenospheres, irregular fragments and porous unburned carbon.…”
Section: Physical and Chemical Properties Of Fly Ashmentioning
confidence: 99%