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Mercury Intrusion Porosimetry Studies with Geopolymers
Abstract The present study examines the role of micro-structure on the compressive strengths of geopolymers using mercury intrusion porosimetry technique. Geopolymers were synthesized from pozzolanas such as, class-F fly ash, kaolinite, metakaolinite, ground granulated blast furnace slag and red soil. Geopolymer reactions were accomplished by alkali activation of the pozzolanas using 10 M NaOH solution at 100 °C for 7-days. The geopolymers exhibited tri-modal nature of pores i.e., macro-pore mode (entrance pore radius: 25–5000 nm), meso-pore mode (entrance pore radius: 1.25–25 nm) and air void mode (entrance pore radius >5000 nm). The micro pores (entrance pore radius <1.25 nm) do not contribute to porosity of the geopolymers. The fly ash geopolymer exhibited largest total intruded volume (0.3908 cm3/g), while the red soil geopolymer exhibited the least intruded volume (0.0416 cm3/g). Interestingly, geopolymers with higher intruded volumes were characterized by larger compressive strengths. The experimental results also indicated that geopolymers with larger air voids + macro pores volume exhibited superior compressive strength; the results imply that geopolymers which develop an open microstructure during polymerization are characterized by larger compressive strength, possibly from stronger bond formation in the silico aluminate structure.
Mercury Intrusion Porosimetry Studies with Geopolymers
Abstract The present study examines the role of micro-structure on the compressive strengths of geopolymers using mercury intrusion porosimetry technique. Geopolymers were synthesized from pozzolanas such as, class-F fly ash, kaolinite, metakaolinite, ground granulated blast furnace slag and red soil. Geopolymer reactions were accomplished by alkali activation of the pozzolanas using 10 M NaOH solution at 100 °C for 7-days. The geopolymers exhibited tri-modal nature of pores i.e., macro-pore mode (entrance pore radius: 25–5000 nm), meso-pore mode (entrance pore radius: 1.25–25 nm) and air void mode (entrance pore radius >5000 nm). The micro pores (entrance pore radius <1.25 nm) do not contribute to porosity of the geopolymers. The fly ash geopolymer exhibited largest total intruded volume (0.3908 cm3/g), while the red soil geopolymer exhibited the least intruded volume (0.0416 cm3/g). Interestingly, geopolymers with higher intruded volumes were characterized by larger compressive strengths. The experimental results also indicated that geopolymers with larger air voids + macro pores volume exhibited superior compressive strength; the results imply that geopolymers which develop an open microstructure during polymerization are characterized by larger compressive strength, possibly from stronger bond formation in the silico aluminate structure.
Mercury Intrusion Porosimetry Studies with Geopolymers
Rao, Sudhakar M. (author) / Acharya, Indra Prasad (author)
Indian Geotechnical Journal ; 47 ; 495-502
2017-06-17
8 pages
Article (Journal)
Electronic Resource
English
Mercury Intrusion Porosimetry Studies with Geopolymers
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