1985
DOI: 10.1107/s0108270185007892
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Structure of the new zeolite theta-1 determined from X-ray powder data

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Cited by 20 publications
(17 citation statements)
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“…The commercial (c-ZSM-22) and in house prepared (m-ZSM-22) zeolites have Si/Al ratios of 49 and 38, respectively, which are within the optimal Si/Al ratio found for mesopore generation for MFI zeolites [19,24,29]. Both samples consist of a highly crystalline ZSM-22 structure [50][51][52][53], as indicated by the diffractograms shown in Fig. S1.…”
Section: Parent Materials Descriptionsupporting
confidence: 54%
See 1 more Smart Citation
“…The commercial (c-ZSM-22) and in house prepared (m-ZSM-22) zeolites have Si/Al ratios of 49 and 38, respectively, which are within the optimal Si/Al ratio found for mesopore generation for MFI zeolites [19,24,29]. Both samples consist of a highly crystalline ZSM-22 structure [50][51][52][53], as indicated by the diffractograms shown in Fig. S1.…”
Section: Parent Materials Descriptionsupporting
confidence: 54%
“…The TON topology is characterized by a pore structure of non-intersecting 5.7 x 4.6 Å 10-member ring channels and crystallizes preferentially as needles, with the micropore channels running in the direction of the needles [49][50][51][52][53]. Zeolites having the TON topology (ZSM-22, NU-10, Theta-1) are certainly strongly affected by diffusion limitations.…”
Section: Introductionmentioning
confidence: 99%
“…Our results are in agreement, within 0.1-0-15 A, with the structure as illustrated in the c-axis projection by Highcock, Smith & Wood (1985), but indicate substantial revision of some of the z coordinates, Si(3) and Si (4) …”
Section: Results Comparison With Powder Diffraction Studysupporting
confidence: 79%
“…They differ from the profile-fitting method in the manner in which the contribution of instrumental and spectral factors to the integrated peak intensities are taken into account and are known as "trial-anderror" methods. The profile-fitting method and the related "trial-and-error" procedures have been successfully used to determine the crystal structure of some zeolites, e.g., Theta-1 [447] and, as a straight classical example, ZSM-S [448]. However, in most cases these methods were applied for the determination of lattice positions of cations and their occupancy by different cations.…”
Section: Profile-fitting Methodsmentioning
confidence: 99%