• Title/Summary/Keyword: zeolites

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PROTROPIC AND PHOTOPHYSICAL PROPERTIES OF 7-HYDROXYQUINOLINE IN X AND Y ZEOLITES

  • Park, Ji-Ho;Jang, Du-Jeon
    • Journal of Photoscience
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    • v.1 no.1
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    • pp.25-29
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    • 1994
  • Diffuse reflectance and emission spectra of 7-hydroxyquinoline intercalated in the supercage of X and Y zeolites are compared with the absorption and emission spectra of aqueous 7-hydroxyquinoline solutions at various pH to understand protropic and photophysical properties of 7-hydroxyquinoline in zeolite microenvironments. Predominance of zwitterionic spedes with significant existences of the other three protropic equilibrium species, normal, protonated and deprotonated species in zeolite samples indicates that the major fraction of the molecules interact with strong acid and base sites of zeolite at an adsorbed position. Observed zeolite pHs of near neutrality are established by a near balance in numbers of many strong acid and base sites rather than by'small numbers or weakness of acid and base sites. Excitations of nonzwitterionic species such as deprotonated species also give prevailing zwitterionic fluorescence, indicating that excited and ground proton transfer cycles of protropic species can be triggered by photons in organized zeolite media as well as in water.

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Composite Crystal Phases of Authigenic Heulandite-clinoptilolite from Sandstones and Its Crystal-chemical Significance (사암에서 산출되는 속성 기원 휼란다이트-클리놉틸로라이트의 복합 결정상의 그 결정화학적 의의)

  • 노진환
    • Journal of the Mineralogical Society of Korea
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    • v.9 no.2
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    • pp.82-92
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    • 1996
  • The coarse-grained (0.05∼0.2mm) zeolites occur as the single-crystal cement in the sandstones of the Chunbuk Formation in the Pohang area. The zeolite cements unusually consist of the composite phases of heulandite and clinoptilolite and in a crystal. The zeolite crystals show chemical zoning ranging from 3.56 to 4.10 in Si/(Al+Fe), and tend to become continuously more silicic and alkalic from the margin toward inside of the crystal. The DTA and high-temperature XRD analyses also show complex patterns of both zeolites. Such a composite crystal showing chemical zoning and complex thermo-chemical behaviors indicates that heulandite and clinoptilolite are constituting a solid solution resulted from the coupled substitution of K+Si4+=Ca2+Al3+.

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Stabilization of Zeolites Y For Separation by Gas Chromatography (GC분리에 의한 Zeolite Y 안정화)

  • Yim, Going;Heenan, Willian A.
    • The Journal of Natural Sciences
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    • v.8 no.1
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    • pp.41-45
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    • 1995
  • A. partially decationized Y zeolite was pretreated under specific conditions. It was found this calcinated zeolite retains its separation properties for mixtures of the gases hydrogen, nitrogen, oxygen, carbon monoxide, and methane but has much lower affinity for water molecules than untreated, e.g., zeolites A type or X type. The observed effect is discussed on the basis of the results of adsorption measurements on the adsorption capacities, isotherms, and heats of adsorption.

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Synthetic study of Zeolites from Some Glassy Rocks (I) L Low-Temperature Hydrothermal Synthesis of Zeolites Na-P, Na-X, and Na-A (유리질 암석으로부터 제올라이트 합성에 광한 연구 (I) : Na-P, Na-X 및 Na-A 제올라이트의 저온 수열 합성)

  • 노진환
    • Journal of the Mineralogical Society of Korea
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    • v.3 no.1
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    • pp.7-17
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    • 1990
  • 화산 유리질 암석을 출발 물질로 사용하여 저온 ($80^{\circ}C$)에서 수열 처리하여 Na-P Na-X 및 Na-A 제올라이트를 합성하였다. 합성과정은 (1) 유리질 분말 시료와 알칼리 용액과의 용해.변질 반응에 의한 1차적인 Na-P의 합성 방식과 (2) 여기서 잔류된 규산질 모액에 Al(OH)3나 NaAlO2의 수용액을 공급하여 보다 고순도의 Na-P, Na-X 및 Na-A를 효과적으로 합성할 수 있었다. 원암의 암상과 조성은 제올라이트들의 화학 조성과 순도 및 백색도같은 물리적 특성에는 영향을 주지만, 합성된 제올라이트의 광물종을 규제하는 주된 요인은 아닌 것으로 해석된다. 합성된 제올라이트의 광물상은 반응 용액의 pH, Al(OH)4 및 Na+에 대한 농도 조건에 주로 의존되는 경향을 나타낸다. 또한 화산 유리질 암석을 제올라이트 합성원료로 활용하는 데에 있어서 (2)와 같음 합성 방안이 보완적으로 시행되면 그 생산성과 효율성을 제고시킬 수 있을 것으로 여겨진다.

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Normal Mode Calculations of Faujasite-Type Zeolite Frameworks

  • Kong, Young-Shik;Jhon, Mu-Shik;No, Kyoung-Tai
    • Bulletin of the Korean Chemical Society
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    • v.6 no.2
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    • pp.57-60
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    • 1985
  • Normal mode calculations about the extended double six ring (D6R) subunit cluster model of Faujasite-type zeolites have been done by using the valence force field with reasonably adjusted force constants. We have studied for four X, Y zeolites species varying in M$_{f}$(Al/Si + Al) values. The calculated characteristic frequencies of D6R mode (${\nu}_{D_{6}R}$) and the rate of change of ${\nu}_{D_{6}R}$ with the mole fractions of aluminum, M$_{f}$ (Al/Si + Al) values agree well with Flanigen's experimental data; the experimental slope is -79 cm$^{-1}$, while the calculated slope is -82 cm$^{-1}$. Those are the improved results as compared to Blackwell's theoretical study; his predicted slope is -94 cm$^{-1}$.

The pH Effect on the Preparation of MFI Type Ferrisilicate Zeolites

  • 염영훈;남상성;김성보;이규완
    • Bulletin of the Korean Chemical Society
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    • v.20 no.7
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    • pp.781-785
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    • 1999
  • Ferrisilicates with MFI type structure were hydrothermally synthesized. The structural environments of iron in the ferrisilicates were characterized by XRD, SEM, IR, EPR, and ammonia-TPD. It has been shown that pH of the final gel mixture during the synthesis affects the crystal size, morphology, chemical composition and catalyticactivity. The results of the lattice parameters, IR, and EPR indicate the existence of a framework iron and the content of framework iron depends on pH of the synthesis gel. Finally, the catalytic activity of these zeolites was examined for the cyclohexane oxidation to cyclohexanol and cyclohexanone in the liquid phase. The conversion of this reaction was increased with increasing iron content of the framework lattice positions.

Determination of Net Atomic Charges Using a Modified Partial Equalization of Orbital Electronegativity Method V. Application to Silicon-Containing Organic Molecules and Zeolites

  • 석재은;노경태
    • Bulletin of the Korean Chemical Society
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    • v.16 no.10
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    • pp.915-923
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    • 1995
  • The parameters for an empirical net atomic charge calculation method, Modified Partial Equalization of Orbital Electronegativity (MPEOE), were determined for the atoms in organosilicon compounds and zeolites. For the organosilicon family, the empirical parameters were determined by introducing both experimental and ab initio observables as constraints, these are the experimental and ab initio dipole moments, and the ab initio electrostatic potential of the organosilicon molecules. The Mulliken population was also introduced though it is not a quantum mechanical observable. For the parameter optimization of the atoms in the aluminosilicates, the dipole moments and the electrostatic potentials which calculated from the 6-31G** ab initio wave function were used as constraints. The empirically calculated atomic charges of the organosilicons could reproduce both the experimental and the ab inito dipole moments well. The empirical atomic charges of the aluminosilicates could reproduce the ab initio electrostatic potentials well also.