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Title: Water splitting by titanium exchanged zeolite A

Journal Article · · J. Am. Chem. Soc.; (United States)
DOI:https://doi.org/10.1021/ja00489a059· OSTI ID:6618450

Analysis of the product resulting from the equilibration 25 g of zeolite A with 50 cc of unstirred 20% titanium chloride solution for 1 h at ambient temperature indicated that 75% of the potassium cations are replaced by titanium cations on the surface of the /sup 1///sub 16/ in.-diameter Linde 3A particles; the cages probably remained intact since little aluminum leaching occurred. Approximately 0.4 cc of gas (40% hydrogen, 60% air) per g of zeolite was collected after direct exposure to strong illumination (> or = 8000 ft-c) for >5 m followed by a 45 m period without illumination. Ti exchanged zeolites X and Y did not evolve detectable H/sub 2/ under similar conditions. The authors concluded that a photoformed radical composed of a Ti(IV)-oxygen complex in which four oxygen atoms surround the Ti atom in a perfect tetrahedron with the unpaired electrons shared by the oxygen atoms is the precursor of H/sub 2/ formation in water submerged titanium-zeolite A. Partial regeneration was accomplished by heating the inactive material to 275/sup 0/C at 3 x 10/sup -2/ Torr for 4 h.

Research Organization:
Univ. of Utah, Salt Lake City
OSTI ID:
6618450
Journal Information:
J. Am. Chem. Soc.; (United States), Vol. 100:21
Country of Publication:
United States
Language:
English