• Journal of the Korean Chemical Society
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• v.32 no.3
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• pp.233-242
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• 1988

The uranium(VI) complexes with new unsaturated macrocyclic ligands of cryptand types and the neodymium(III) complexes with cryptand 222 and DBC ligands have been investigated polarographically in dimethylsulfoxide solvent. The reduction states, electron numbers involved in the reduction process, effects of the added acid on the polarograms of complexes, and the mechanisms of the reduction electrode reactions have been examined. The stability constants and mole-ratio of new complexes were also obtained by polarographic method. The reaction of ligands was controlled by the diffusion in the reduction with four electrons at a step, whereas the redox reaction with six electrons at three steps in $UO_2\;^{2+}$ complexes with macrocyclic ligands and the redox reaction with one electron at a step in $Nd^{3+}$ complexes with cryptand 222 and DBC have been observed. The imine ligands formed stable complexes with uranium(VI) above pH 7.0, and the neodymium(III) complexes with cryptand 222 and DBC ligands were stable above pH 4.0.

• The Korean Journal of Zoology
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• v.15 no.2
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• pp.71-85
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• 1972

This investigation was undertaken to establish the ultrastructural organization of the retina in domestic fowl (Gallus domesticus B.) comparing with the ultrastructure that has been indicated in other Aves by several workers. The electron microscope observations were made on selected segments of retinal tissue prefixed for 2 hrs in 1.25% glutaraldehyde buffered with 0.2 M cacodylate at pH 7.2 and then postfixed in cold 1% osmium tetroxide in 0.4 M cacodylate buffer for 2 hrs. After postfixation, tissues were dehydrated in alcohol series, embedded in Epon 812 mixture from propylene oxide and stained with saturated uranyl acetate and $Pb(NO_3)_2$ solution. Specimens were examined with a Hitachi HS-7S electron microscope. The pigment epithelia cells contain numerous mitochondria with prominent dense granules and several changeful spaped Golgi bodies. The internal fine structure of the receptor outer segments revealed the characteristic stacks or arrays of bimembranous disks. The ellipsoid outer portion of the cone inner segments is composed of a tightly packed mass of extraordinarily large mitochondria. The outer limiting membrane is seen to contain many junctional complexes, the fibrillar material of which is electron-dense.

• The Journal of Engineering Geology
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• v.25 no.4
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• pp.557-576
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• 2015

Groundwaters in granite, gneiss, and two-mica granite formations, including faults, in the Hoengseong area are examined to determine the relationship between their uranium and radon-222 contents and rock types. The chemical compositions of 38 groundwater samples and four surface water samples collected in the study area were analyzed. Sixteen of the samples showing high uranium and radon-222 contents were repeatedly analyzed. Surface radioactivities were measured at 30 points. The uranium and radon-222 concentrations in the groundwater samples were in the ranges of 0.02-49.3 μg/L and 20-906 Bq/L, respectively. Four samples for uranium and 35 samples for radon had concentrations exceeding the alternative maximum contaminant level of the US EPA. The chemical compositions of groundwaters indicated Ca(Na)-HCO₃ and Ca(Na)-NO₃(HCO₃+Cl) types. The pH values ranged from 5.71 to 8.66. High uranium and radon-222 contents in the groundwaters occurred mainly at the boundary between granite and gneiss, and in the granite area. The occurrence of uranium did not show any distinct relationship to that of radon-222. The radon-222, an inert gas, appeared to be dissolved in the groundwater of the aquifer after wide diffusion along rock fractures, having been derived from the decay of uranium in underground rocks. The results in this study indicate that groundwater of neutral or weakly alkaline pH, under oxidizing conditions and with a high bicarbonate content is favorable for the dissolution of uranium and uranium complexes such as uranyl or uranyl-carbonate.

• Applied Microscopy
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• v.24 no.2
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• pp.48-62
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• 1994

The acute irradiation effect on rat Purkinje cell was carried out. Anesthetized rats, weighing 200-250g each, were exposed their heads to the linear accelerator (ML-4MV) with the doses of 3,000 rads or 6,000 rads respectively. Irradiated rats were sacrificed by perfusion fixation under anesthesia, six hours, two days and six days following the irradiations. Rats were perfused with the fixative of 1% glutaraldehyde-1% paraformaldehyde solution (pH 7.4). Small pieces of cerebellar cortices were taken out. Tissue blocks were washed out, and were refixed in the 2% osmium tetroxide solution. After dehydration, tissues were embedded in the araldite mixture. Ultrathin sections stained with uranyl acetate-lead citrate solution, were examined with an electron microscope. The results observed were as follow; 1. Many dark Purkinje cells exhibited most severe cellular alterations on 6 hours. But after the 2 or 6 days, the cells exhibited only some alterations of cytoplasmic organelles. 2. Many granular and agranular endoplasmic reticula exhibited the fusion of cisterns. These reticular alterations were most severe on 6 hours following irradiation. But the alterations were hardly found on 6 days. 3. In the Golgi region, alterations including the adhesion of lamelliform cisterns, enlarged saccules, and increased number of vesicles, etc, were seen on 6 hours. But the Golgi complexes were almost recovered on 6 days. 4. Lysosomes were abundant on 6 hours or 2 days, but some residual bodies were found on 6 days. 5. Mitochondrial changes were also most severe at on hours, and they were recovered thereafter. From the results, it was concluded that the cerebellar Purkinje cells reacted to the high doses of irradiation by hyperactive protein synthesis, autolytic activities and energy metabolism. The reaction was most active in the early stage. It implies that motor-control function of Purkinje cells are severely disturbed in the early stage of irradiation.

• Economic and Environmental Geology
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• v.56 no.5
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• pp.603-618
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• 2023

This study focused on evaluating the suitability of the WRK (waste repository Korea) bentonite as a buffer material in the SNF (spent nuclear fuel) repository. The U (uranium) adsorption/desorption characteristics and the adsorption mechanisms of the WRK bentonite were presented through various analyses, adsorption/desorption experiments, and kinetic adsorption modeling at various pH conditions. Mineralogical and structural analyses supported that the major mineral of the WRK bentonite is the Ca-montmorillonite having the great possibility for the U adsorption. From results of the U adsorption/desorption experiments (intial U concentration: 1 mg/L) for the WRK bentonite, despite the low ratio of the WRK bentonite/U (2 g/L), high U adsorption efficiency (>74%) and low U desorption rate (<14%) were acquired at pH 5, 6, 10, and 11 in solution, supporting that the WRK bentonite can be used as the buffer material preventing the U migration in the SNF repository. Relatively low U adsorption efficiency (<45%) for the WRK bentonite was acquired at pH 3 and 7 because the U exists as various species in solution depending on pH and thus its U adsorption mechanisms are different due to the U speciation. Based on experimental results and previous studies, the main U adsorption mechanisms of the WRK bentonite were understood in viewpoint of the chemical adsorption. At the acid conditions (＜pH 3), the U is apt to adsorb as forms of UO₂²⁺, mainly due to the ionic bond with Si-O or Al-O(OH) present on the WRK bentonite rather than the ion exchange with Ca²⁺ among layers of the WRK bentonite, showing the relatively low U adsorption efficiency. At the alkaline conditions (>pH 7), the U could be adsorbed in the form of anionic U-hydroxy complexes (UO₂(OH)₃^-, UO₂(OH)₄^2-, (UO₂)₃(OH)₇^-, etc.), mainly by bonding with oxygen (O^-) from Si-O or Al-O(OH) on the WRK bentonite or by co-precipitation in the form of hydroxide, showing the high U adsorption. At pH 7, the relatively low U adsorption efficiency (42%) was acquired in this study and it was due to the existence of the U-carbonates in solution, having relatively high solubility than other U species. The U adsorption efficiency of the WRK bentonite can be increased by maintaining a neutral or highly alkaline condition because of the formation of U-hydroxyl complexes rather than the uranyl ion (UO₂²⁺) in solution,and by restraining the formation of U-carbonate complexes in solution.