• 한국전기전자재료학회논문지
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• 제16권6호
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• pp.522-531
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• 2003

Samples with the nominal composition, B $i_{1.84}$P $b_{0.34}$S $r_{1.91}$C $a_{2.03}$C $u_{3.06}$ $O_{10+{\delta}}$ high- $T_{c}$ superconductors containing MgO as an additive were fabricated by a solid-state reaction method. Samples with MgO of 5~30 wt% each were sintered at 820~86$0^{\circ}C$ for 24 hours. The structural characteristics, critical temperature, grain size and image of mapping with respect to MgO contents were analyzed by XRD(X-Ray Diffraction), SEM(Scanning Electron Microscope) and EDS(Energy dispersive X-ray spectrometer) respectively. As MgO contents increased, intensity of MgO Peaks and ratio of Bi-2212 phase in superconductors intensified and the proportion of the phase transition from Bi-2223 to Bi-2212 was increased.

• E2M - 전기 전자와 첨단 소재
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• 제7권4호
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• pp.306-311
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• 1994

In this study, the influence of the powder sintering, the 2nd sinteiing and the grinding time on the Superconducting properties in the Bi(Pb)SiCaCuO Superconductor has been studied. From the analysis of SEM and XRD patterns, it was known that the sample prepared by the process of powder sintering has a porous microstructure with the critical temperature(Tc) below 77K, while the sample prepared by the 2nd sintering has a highly oriented microstructure with the Tc above 100K. The Critical Current Density(Jc) of the sample prepared by the 2nd sintering was better than the sample prepared by the process of powder sinteiing, but it's Jc, was low in practical use. Also, the effect of grinding time from 0[min] to 120[min] was investigated. As the grinding time is increased, the samples degraded from high-Tc phase to low-Tc phase and nonsuperconducting phases.

• Bulletin of the Korean Chemical Society
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• 제11권6호
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• pp.560-563
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• 1990

A.c. susceptibility for $Bi_{1.4}Pb_{0.6}Sr_2Ca_2Cu_{3.6}O_x$ superconductor is measured as a function of temperature at different value of a.c. magnetic field amplitude. Two transition steps are attributed to the intergranular and intragranular properties. Based on Bean's critical state model, intergranular critical current density, $J_c^{gb}$ (11 $A/cm^2$ at 77 K) and intragranular critical current density, $J_c^g (7{\times}10^3\;A/cm^2$ at 100 K) are estimated. The low values of $J_c^{gb}$and $J_c^g$ reflect a poor nature of coupling between grains and the low pinning force density of intragrain in $Bi_{1.4}Pb_{0.6}Sr_2Ca_2Cu_{3.6}O_x$ superconductor.

• Applied Biological Chemistry
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• 제44권3호
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• pp.185-190
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• 2001

알긴산은 일반적으로 미생물의 고정화에 널리 사용되는 biopolymer이다. 본 연구는 구연산 생산균인 Aspergillus niger를 calcium alginate로 고정화한 beads로 납의 흡착 특성을 조사하였다. A. niger beads는 $CaCl_2$를 사용하여 주사기로 제조하였으며 이 beads를 납제거에 이용하였다. 그 결과는 다음과 같다. 즉, A. niger를 구연산 생성배지에서 1일에서 7일까지 배양한 후 제조한 beads로 납흡착량을 측정한 결과는 3일간 배양된 곰팡이 beads에서 가장 높았다. 발아되지 않은 beads와 3일간 배양된 beads로 시간에 따른 납흡착량을 정량한 결과 30분까지는 그 흡착량이 동일하게 급격히 증가하였으며 그 후 발아되지 않은 beads는 더 이상 흡착이 일어나지 않았으나 3일간 배양된 곰팡이 beads는 시간이 지남에 따라 천천히 계속 흡착하여 1시간 후에는 480 ppm까지 흡착하였다. 납흡착시 최적 pH와 온도는 각각 6과 $35^{\circ}C$로 나타났다. 납용액 50 ml (500 ppm)이 든 250 ml 삼각플라스크에 beads $50{\sim}100$개가 최적이었으며 그 이상에서는 납흡착율이 감소하였다. 중금속에 대한 흡착율은 납> 구리> 카드뮴 순이었으며 0.1 M $CaCl_2$, 0.1 M NaOH 및 0.1 M KOH의 전처리의 효과는 없었으며 0.1 HCI로 곰팡이 bead의 납탈착하여 beads를 재사용이 가능하였다.

• 한국세라믹학회지
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• 제40권5호
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• pp.405-409
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• 2003

The effect of substitution of Gd ions for Ca ions in the B $i_{1.84}$P $b_{0.34}$S $r_{1.91}$(C $a_{1-x}$ G $d_{x}$)$_{2.03}$ C $u_{3.06}$ $O_{ 10+{\delta}}$/ (x=0.0~0.06) was investigated by measuring x-ray diffraction patterns, lattice constants, do resistivity and Hall effect. We found the solubility limit of Gd in the 110 K phase to be x < 0.015. Within the solubility limit, the c-axis seemed to decrease with increasing x. In the region of the 110 K single phase, the critical temperature $T_{c}$ gradually decreased with an increasing the Gd concentration x, corresponding to a small change of the carrier concentration.

• 한국표면공학회지
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• 제39권6호
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• pp.302-311
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• 2006

Nowadays the open-type lead-acid battery for vehicle use is being replaced with the sealed-type because it needs no maintenance and has a longer cycle life. Thus researches on this battery are being conducted very actively by many advanced battery companies. There is, however, a serious problem with the maintenance free(MF) battery that its cathode electrode has a limited cycle life due to a corrosion of grid. In this study, it was aimed to improve a corrosion resistance of the cathode grid which is commonly made of Pb-Ca alloy for a mechanical strength. For this purpose, various amounts of alloying elements such as Sn, Ag and Ba were added singly or together to the Pb-Ca alloys and investigated their corrosion behaviors. Batteries fabricated by using these alloys as cathode grids were subjected to life cycle test and their corrosion layers appeared at the interface between the grids and the active materials were carefully observed in order to clarify effects of alloying elements.

• 한국환경보건학회지
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• 제30권5호
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• pp.455-468
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• 2004

The purpose of this paper is to understand the time series and origin of a chemical component and to compare the difference during yellow sand episodes for analysis $PM_{10}$ chemical components in the region of west in Korean Peninsula, 1999-2001. An annual mean concentration of $PM_{10}$ is $29.1\;{\mu}g/m^3$. A monthly mean and standard deviation of $PM_{10}$ concentration are very high in spring but there is no remarkably seasonal variation. Also, water soluble ionic component of $PM_{10}$ be influenced by double more total anion than total cation, be included $NO_{3}^-\;and\;SO_{4}^{2-}$ for the source of acidity and $NH_{4}^+$ to neutralize. Tracer metals of $PM_{10}$ slowly increases caused by emitted for soil and ocean (Fe, Al, Ca, Mg, Na) and Zn, Pb, Cu, Mn for anthropogenic source. According to method of enrichment factor (E.F) and statistics, assuming that the origin of metal component in $PM_{10}$ most of element in the Earth's crust e.g. Mg, Ca, Fe originates soil and Cu, Zn, Cd, Pb derives from anthropogenic sources. The ionic component for $Na^{+}\;Cl^-,\;Mg^{2+}\;and\;Ca^{2+}$ and Mg, Al, Ca, Fe originated by soil component largely increase during yellow sand period and then tracer metal component as Pb, Cd, Zn decrease. According to factor analysis, the first group is ionic component ($Na^+,\;Mg^{2+},\;Ca^{2+}$) and metal component (Na, Fe, Mn and Ni) be influenced by soil. The second group, Mg, Cr also be influenced by soil particle.

• 박물관보존과학
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• 제14권
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• pp.37-60
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• 2013

국립중앙박물관 소장 고구려 벽화는 국립중앙박물관 도록에 소개된 벽화 모사도와 일제 강점기에 촬영한 유리건판 사진으로만 제공되어 왔다. 그러나 이번에 수행한 국립중앙박물관 소장 고구려 벽화 편의 보존과학적 처리와 분석을 통해 전모를 파악할 수 있게 되었다. 보존과학적 처리는 벽화 편의 바탕층의 구조와 성분, 균열 등의 손상 파악과 퇴색된 채색 부분에 광학현미경과 적외선 조사를 했으며, 취약한 벽체와 박락된 채색층 강화에 중점을 두고 수행하였다. 더불어 적외선 조사한 결과를 국립중앙박물관 소장 벽화 모사도와 유리건판사진과 비교하여 고분의 위치를 조사했으며, 일부 벽화 편에서 감신총, 개마총, 고산리1호분, 운봉리고분으로 확인되었다. 고구려 벽화 편에 채색된 안료의 성분 원소와 벽체층의 광물구조를 분석하였다. 분석결과, 모든 측정 위치에서 방해석[calcite, CaCO₃]이 확인되었다. 이는 벽화의 바탕재료로 보이며, 석회층 위에 안료를 채색한 것으로 판단된다. 안료 색상 중 갈색을 포함한 황색은 산화철[hematite, Fe₂O₃]로 검출되었고 일부 편에서는 백연석[cerussite, PbCO₃]과 산화납[lead oxide, PbO]이 확인되었다. 이는 연백[lead white, 2PbCO₃·Pb(OH)₂]의 산화물로 추정된다. 또한 적색에서는 주사[cinnabar, HgS], 흰색에서는 방해석[calcite, CaCO₃]과 백연석[cerussite, PbCO₃]이 확인되었다.

• Clinical and Experimental Reproductive Medicine
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• 제24권1호
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• pp.67-81
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• 1997

To determine the concentration and the physiologic role of metal components in blood plasma and seminal plasma in relation to male infertility, the concentrations of twelve metal components in blood plasma and seminal plasma including Na, Mg, K, Ca, Cr, Mn, Fe, Cu, Zn, Se, Cd and Pb were measured by atomic absorbance spectrophotometery or ion selective electrode analysis. Semen and blood samples were obtained from a total of 110 men including 70 male infertility patients, 20 vasectomized persons and 20 fertility proven volunteers visited to the Male Infertility Clinic of Pusan National University Hospital. The concentrations of Ca, Zn, Mg, Cr and Cd in control group were higher in seminal plasma than in blood plasma, and additionally Pb were higher in infertility group. The concentrations of all metal components revealed no significant difference according to patients' age, resident, occupation, sperm density, motility and hormone level in blood plasma, but some metal components including Ca, Mg, Cu, Mn, Cd and Pb revealed a significant difference according to each these parameters except patient's age in seminal plasma. The concentrations of Mn, Cd and Pb in the vasectomy persons were higher than in the infertility group III including testicular and epididymal factors, but not in blood plasma. We conclude that the quantitative changes of metal components in the seminal plasma may have effects on not only spermatogenesis and sperm function, but also contribute to diagnostic parameter according to organ specificity of the metal in the male reproduction.

• 자원환경지질
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• 제25권3호
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• pp.245-258
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• 1992

The variations of certain major and trace elements of the Onjong granite mass was studied on the basis of petrological and geochemical characteristics and compared with those of the Eonyang-Yucheon granite masses in order to investigate the geochemical differences of the granitic rocks in relation to mineralization between Pb-Zn ore district and Pb-Zn-Mo-W ore district in Kyeongsang basin. The Onjong granite mass is classified into granodiorite and monzo-granite, and the Eonyang-Yucheon granite masses into monzo-granite by the Streckeisen's diagram. Between both granite masses there are clear differences in contents of certain major elements and lithophile trace elements. The former have high contents of Ca (2.94%), Mg (1.66%) and Sr (365 ppm), and low contents of K (3.52%), Na (3.51%), Rb (116 ppm), Ba (640 ppm) and Li (18.9 ppm), whereas the latter have high contents of K (4.02%), Na (4.28%), Rb (145 ppm), Ba (695 ppm) and Li (19.3 ppm), and low contents of Ca (1.42%), Mg (0.43%) and Sr (161 ppm). Except for Mo, there are not clear differences in chalcophile trace elements between two granite masses: the Onjong granite mass has higher Mo content (7.1 ppm) lnan that (1.7 ppm) of the Eonyang-Yucheon granite masses, but Pb and Zn contents are similar between the Onjong granite mass (Pb=8.7 ppm, Zn=37.1 ppm) and the Eonyang-Yucheon granite masses (Pb=7.8 ppm, Zn=39.8 ppm). Ca and Sr contents of the Onjong granite mass (Ca> 1.5%, Sr> 270 ppm) are higher than those of the Eonyang- Yucheon granite masses (Ca<1.5%, Sr<270ppm), and Rb/Sr, Rb-Rb/Sr and K-Rb/Sr ratios are clearly distinguishable between the Onjong granite mass(Rb/Sr<0.51, Rb-Rb/Sr>250 and K-Rb/Sr>5.2) and the Eonyang- Yucheon granite masses (Rb/Sr>0.51, Rb-Rb/Sr<250 and K-Rb/Sr<5.0). Thus, variations of certain major and trace elements and ratios are applicable as geochemical index to distinguish the types of mineralization of the ore districts related to the Cretaceous granitic rocks in the Kyeongsang basin.