Compositions and Microstructures of Carbonated Geopolymers with Different Precursors

  • 0Graduate School of Science and Technology for Innovation, Yamaguchi University, 2-16-1 Tokiwadai, Ube 755-8611, Japan.

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Summary

This summary is machine-generated.

Geopolymers made from fly ash and slag readily carbonate. Carbonation forms nahcolite or calcite, with blend-based geopolymers showing unique pore-plugging structures, revealing gel composition and changes.

Area Of Science

  • Materials Science
  • Geochemistry
  • Construction Materials

Background

  • Geopolymers (GPs) are susceptible to carbonation, particularly when cured at ambient temperatures.
  • Understanding the impact of carbonation on geopolymer matrix gel composition and microstructure is crucial.

Purpose Of The Study

  • To investigate the composition and microstructure of geopolymer matrix gels.
  • To identify the carbonation products formed in geopolymers derived from fly ash (FA) and ground granulated blast-furnace slag (GGBS).
  • To analyze compositional changes in geopolymers after carbonation using advanced analytical techniques.

Main Methods

  • Preparation of geopolymers using low-lime FA and GGBS precursors, alone or blended.
  • Specimen curing at 20 °C with alkali activator solution, followed by sealed or accelerated carbonation.
  • Analysis using X-ray Diffraction (XRD), Scanning Electron Microscopy with Energy Dispersive X-ray Spectroscopy (SEM-EDS), and ternary diagram analysis.

Main Results

  • Carbonation products identified as nahcolite (FA-based GPs) and calcite (GGBS-based GPs).
  • SEM-EDS revealed cube-shaped and small calcite particles in GGBS-based GPs, and unique hail-like particles in FA/GGBS blend-based GPs.
  • Ternary diagram analysis confirmed hail-like particles as calcite and C-A-S-H gel complexes that plug pores in spongy C-A-S-H gels.

Conclusions

  • Combined ternary diagram analysis of S-(C+M+N)-A and A-(C+M)-N effectively determines geopolymer gel type and carbonation products.
  • C-A-S-H gels exhibit linear distribution along the (C+M+N)-albite join, while N-A-S-H gels show scattered distribution in S-(C+M+N)-A diagrams.
  • Distinct zoning for N-A-S-H and C-A-S-H gels is observed in A-(C+M)-N diagrams, aiding in understanding compositional changes post-carbonation.

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