• Applied Chemistry for Engineering
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• v.21 no.4
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• pp.417-423
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• 2010

In this study, an effective method to prepare granular binderless ZSM-5 which is as efficient p-xylene separatory adsorbent was explored. Colloidal silica sol 30 wt% solution as an inorganic binder and microcrystalline cellulose as an organic additive were added to ZSM-5 powder ($SiO_2/Al_2O_3$ = 50). Adsorbent with enough strength (0.721 kgf), high crystallinity (94.6%) and high BET specific surface area ($379.2m^2$/g) was obtained by calcination, binderless treatment, ${NH_4}^+$ ion exchange, and activation after spherical granulation process. A batch type adsorption experiment was proceeded with solutions comprising 3 xylene isomers by 1 : 1 : 1 weight ratio to evaluate adsorption characteristics of prepared absorbent. As a result, the obtained binderless ZSM-5 granule showed a higher selective adsorption performance for para-xylene than that of commercial adsorbent.

• Journal of the Korean Ceramic Society
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• v.39 no.1
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• pp.51-56
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• 2002

The effect of kind of starting materials used for a sintering additive. magnesium acetate and magnesium nitrate, on the mechanical properties of alumina sintered body made by adding 1000 ppm of the additives, respectively, was investigated. As for the alumina sintered bodies prepared from magnesium acetate and magnesium nitrate, we observed that their relative densities decreased rapidly with increasing sintering temperature 1$600^{\circ}C$. Outer layer of alumina bodies had a duplex microstructure consisting of pores and grain growth. Also the inner layer had a second phase between alumina grain boundaries. By EPMA analysis, we confirmed that the grain boundary phase was a compound containing Mg.

• Journal of Powder Materials
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• v.30 no.5
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• pp.424-430
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• 2023

YAG phosphor powders were fabricated by the atmospheric plasma spraying method with the spray-dried spherical YAG precursor. The YAG precursor slurry for the spray drying process was prepared by the PVA solution chemical processing utilizing a domestic easy-sintered aluminum oxide (Al₂O₃) powder as a seed. The homogenous and viscous slurry resulted in dense granules, not hollow or porous particles. The synthesized phosphor powders demonstrated a stable YAG phase, and excellent fluorescence properties of approximately 115% compared with commercial YAG:Ce³⁺ powder. The microstructure of the phosphor powder had a perfect spherical shape and an average particle size of approx imately 30 ㎛. As a result of the PKG test of the YAG phosphor powder, the synthesized phosphor powders exhibited an outstanding luminous intensity, and a peak wavelength was observed at 531 nm.

• Applied Microscopy
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• v.18 no.2
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• pp.102-118
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• 1988

This study was carried out to examine in vitro first whether the storage proteins, which the fat bodies of last larvae from Hyphantria cunea secrete into haemolymph, can be uptaked by the fat body cells of prepupa and then how the uptaked storage proteins can be accumulated in the fat body cells, if uptaken. The fat bodies which had been isolated from last instar larvae were cultured in 1 ml of Grace's insect medium containing $50{\mu}l$ of $^{3}H$-leucine (5.0 mCi/mol, Dupont) at $28{\pm}2^{\circ}C$ for 6 hrs. After the homogenates of the cultured fat bodies were centrifuged at 10,000 rpm for 10 minutes, the proteins included in the supernatant were separated by polyacrylamide gel electrophoreses (non-SDS, 6%). The next treatment of the electrophoresed gel was followed by rinsing. A storage protein band of several bands in the rinsed gel was sliced off. With elution of sliced storage protein bands in Tris-glycine buffer, the purification of radioactive storage proteins from fat bodies was finished. After the purified radioactive storage proteins were added in Grace's insect midis containing fat bodies of the prepupae, they were cultured for the randomly following minutes given as 3, 5, 7, 10, 15, 20 and 30 and for the randomly following hours given as 1, 2, 3 and 4 respectively. The double fixations of the cultured fat bodies in aldehyde and $OsO_4$, were followed by preparation of ultrathin sections from Epon-Araldite blocks through dehydration and embedding. The electron microscope autoradiographic treatment of all prepared sections were performed by the dipping method (Kim et al., 1987). The finally prepared specimens were examined with electron microscope. The fat body cells of the prepupa could be found to uptake the storage preteins of the last instar larvae, which were included in the culture medium, mostly by formation of coated vesicles. The in vitro uptake of the storage proteins actively occurred by 30 minutes after the addition of purified storage proteins in the culture medium. After culture for 7 minutes with the storage proteins, the uptaked radioactive storage proteins labelled a number of lysosomal granules. After culture for 20 minutes with the storage proteins, the radioactive storage proteins were finally incorporated and accumulated in lipid droplets and protein granules. The frequency in the fat body cell of radiolabelled lipid droplets occurs approximately 60%, while the frequency, in which the radiolabelled protein granules occurs in a fat body cell, is approximately 40%.

• Journal of the Mineralogical Society of Korea
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• v.15 no.1
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• pp.22-32
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• 2002

Mineral composition and chemistry of the clay minerals in the three cores from the continental shelves of South Shetland Islands (NCS09) and Anberse Island (GC98-2), and from the fjord of King George Island (A10-01) were determined by X-ray diffraction and electron microprobe analysis in search of the distributions and origin of the clay minerals in the Antarctic marine sediments. Smectite content is relatively high in NCS09 regardless of core depths (av. 8.3%), but low in GC98-2 (1.1%). In Al0-01, smectite content is higher in the upper section than in the lower section. Kaolinite was not detected from all the cores in this study Yellow to yellowish green clay granules were commonly scattered in the sediments of NCS09 cores. The clays contain 16.97% and 2.53% $Fe_2$$O_3$와 $K_2$O. Average structural formula of the clay indicates ferrian beidellite . The (Fe, K)-rich smectite of NSC09 must have been derived from relatively young basaltic volcanics altered by reaction with seawater near Shetland Islands by glacial erosion or eolian process related to volcanic eruption. GC98-2 nearer to Antarctic continent is very low in smectite content. In A10-01, the lower diamicton was deposited from the glacial erosion of smectite-free ancient volcanics in the interior of King George Island, while the upper section was derived from the smectite-bearing terrestrial debris and eolian materials after retreat of glaciers in Marian Cove and ice cover in Barton Peninsula. Thehigh K contents of smectites suggest the interstratification of illite and smectite layers, which might be observed by future TEM lattice fringe imaging.