4.7 Article

Phase transformation and morphology evolution of sepiolite fibers during thermal treatment

Journal

APPLIED CLAY SCIENCE
Volume 143, Issue -, Pages 205-211

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.clay.2017.03.042

Keywords

Sepiolite; Phase transformation; Morphology evolution; Thermal treatment; Mineral fibers

Funding

  1. Hebei University Innovation Team Leader Talent Cultivation Project [LJRC020]
  2. National Natural Science Foundation of China [51404085]
  3. Key Technology R & D Program of Tianjin city [15ZCZDSF00030]
  4. National Key Technology R & D Program of China [2008BAE60B07]

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In this study, the phase transformation and micromorphology evolution of sepiolite fibers were studied along with the increase of temperature from 300 to 1300 degrees C, using raw sepiolite samples as raw materials. Through characterization by scanning electron microscope (SEM), high resolution transmission electron microscope (HRTEM), X-ray diffraction (XRD), thermo-gravimetric analysis (TGA/DTG) and differential scanning calorimeter (DSC), it was found that the determined transition temperature values for the dehydrations of the hygroscopic water and the zeolitic water were 120 degrees C and 340 degrees C, and the values for the dehydration of the bound water and the dehydroxylation of the hydroxyls were about 500 degrees C and 810 degrees C. Moreover, orthoenstatite (MgSiO3) was recrystallized from dehydroxylated phase at 852 degrees C and then transformed into protoenstatite, at 970 degrees C, and enstatite crystals grew along with c-axis of the fiber with the increase of temperature. Amorphous phase as the other phase of sepiolite dehydroxylation recrystallized into cristobalite in the temperature range of 1130-1200 degrees C and the samples began to melt at the above temperature range. In terms of morphology, both sepiolite bundles and laths remained constant after heating up to 1000 degrees C and sintering phenomenon appeared when the temperature was up to 1100 degrees C. The bundles partly melted and adhered each other, which further formed a porous structure after calcination at 1200 degrees C. When the temperature was up to 1300 degrees C, the sample substantially melted except for a small amount of enstatite and cristobalite crystals. The present study reflects the thermal reaction of sepiolite, which could be applied in exploring the reinforcement mechanism of sepiolite reinforced ceramic body composites.

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