Ti-substituted organosilica membranes for H 2 sieving: Sol-gel and DFT insights


KAYI H., Kaya P., Kurt T., Mirza E. S., TOPUZ B.

INTERNATIONAL JOURNAL OF HYDROGEN ENERGY, cilt.65, ss.496-504, 2024 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 65
  • Basım Tarihi: 2024
  • Doi Numarası: 10.1016/j.ijhydene.2024.04.091
  • Dergi Adı: INTERNATIONAL JOURNAL OF HYDROGEN ENERGY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Academic Search Premier, PASCAL, Artic & Antarctic Regions, Chemical Abstracts Core, Chimica, Communication Abstracts, Compendex, Environment Index, INSPEC
  • Sayfa Sayıları: ss.496-504
  • Ankara Üniversitesi Adresli: Evet

Özet

The fabrication of gas-sieving amorphous silica membranes exhibiting superior thermal/hydrothermal/chemical stability by the facile, scalable and controllable synthesis strategies is highly desired to bring the silica membranes a step closer to large scale deployment. Sol -gel modification of bis(triethoxylsilyl)ethane (BTESE) membrane pore network with Ti substitution resulted with a shift in the molecular level cut -off to smaller molecules establishing ideal selectivity improvement from 13 +/- 2 to 20 for H 2 /N 2 and 17 +/- 4 to 28 for H 2 /CH 4 at 200 degrees C. BTESE and analogous Ti-substituted BTESE membranes (BTESE-Ti) exhibited H 2 permeances of (0.9-1.2)x10 -6 mol/(m 2 sPa) and 5.8 x 10 - 7 mol/(m 2 sPa), respectively, reflecting a difference in their thickness. Decrease in the sol concentration by 2 -fold led to an increase in the H 2 permeance value to 8.9 x 10 -7 mol/ (m 2 sPa) at 200 degrees C for BTESE-Ti membranes. We further theoretically designed amorphous BTESE and BTESE-Ti structures, and simulated their interactions with the gas molecules along with the pore diffusion of H 2 as a model system to elucidate the membrane performance through the density functional theory (DFT) calculations. Theoretical findings suggest that the only transport mechanism is the direct transport from the gas phase to the pore entrance by excluding the surface diffusion possibility.