• 한국산업보건학회지
• /
• 제25권2호
• /
• pp.146-155
• /
• 2015

Objectives: The aims of this study were to set up benzene exposure matrices according to industry and process and to assess the risk of those occupational exposure to benzene. Methods: The benzene exposure matrices were assembled depending on industry and process, based on an exposure database provided by KOSHA(the Korean Occupational Safety and Health Agency), which was gathered from a workplace hazards evaluation program in Korea. These exposure matrices were assessed by Hallmark Risk Assessment tool. Results: The benzene was treated 412 industries sector(36%), 2,747 business places, and 471 industrial processes according to database. The arithmetic mean of past decade 8 hours time-weighted average of airborne benzene concentrations in the workplace was 0.10722 ppm. 1.07% of the total sample were greater than OEL, and 59.8% were showed less than the limit of detection. The highest risk values(Danger Value) were seen 36 industries including manufacture of general paints and similar product and 12 processes, such as other painting of manufacture of metal fabricated members. Exposure matrices based on employee exposure data base may provide exposure histories and can be used in epidemiological studies. Conclusions: It was found that more attentions should be paid to 36 among 412 industries and 12 of 471 processes, with a higher risk value.

• 한국광물학회지
• /
• 제19권3호
• /
• pp.139-151
• /
• 2006

캐나다 온타리오주 코발트지역에는 시생대의 화산암을 부정합으로 피복하고 있는 원생대의 휴로니안 퇴적암 내에는 황화물이 농집된 광화작용이 발달한다. 황화광물들은 원생대에 발달했던 퇴적분지에 쌓인 기저역암 내에 농집되어 있다. 황화광물은 기저역암과 Coleman 역암에서는 파편형태로, 퇴적암 전체에서는 광범위한 산점상 형태, 그리고 Ag-Co-Ni-As 탄산염맥 주변의 산점상 형태 등으로 산출된다. 황화광물 파편들의 형태가 모가 나있고 사암과 이질암에서 점이적 퇴적구조를 나타내고 있는 것으로 보아 황화광물들이 기계적 운반작용에 의해 이동된 후 퇴적암 내에서 광화작용을 이루었음으로 시사한다. 한편, 탄산염맥 근처에서 발견되는 산점상 광석광물들은 열수작용에 의해 형성된 것으로 추정된다. 기반암인 시생대 화산암에 발달한 대규모의 화산성 황화물 광상이 퇴적암에 존재하는 광석광물의 공급원이었음을 알 수 있다. 사암 및 이질암에 존재하던 광석광물들은 후기에 관입한 휘록암에 수반된 열에 의해 재결정작용을 받았다.

• International Journal of Automotive Technology
• /
• 제5권1호
• /
• pp.55-59
• /
• 2004

Spot welding is a very important and useful technology in fabrication of thin sheet structures such as the parts in an automobile. However, because the fatigue strength of the spot welding point is considerably lower than that of the base metal due to stress concentration at the nugget edge, the nugget size must be estimated to evaluate a reasonable fatigue strength at a spot welded lap joint. So far, many investigators have experimentally studied the estimation of fatigue strengths of various spot weldments by using a destructive method. However, these destructive methods poses problems so testing of weldments by these methods are difficult. Furthermore, these methods cannot be applied to a real product, and are time and cost consuming, as well. Therefore, there has been a strong, continual demand for the development of a nondestructive method for estimating nugget size. In this study, the effective nugget size in spot weldments have been analyzed by using thermoelastic stress analysis adopting infrared thermography. Using the results of the temperature distribution obtained by analysis of the infared stress due to adiabatic heat expansion under sinusoidal wave stresses, the effective nugget size in spot welded specimens were estimated. To examine the evaluated effective nugget size in spot weldments, it was compared with the results of microstructure observation from a 5％ Nital etching test.

• 자원환경지질
• /
• 제18권4호
• /
• pp.331-342
• /
• 1985

The Dongbo tungsten-molybdenum deposits are fissure-filling veins emplaced in granites of late Cretaceous age. Integrated field, mineralogic and fluid inclusion studies were undertaken to illuminate the characters and origin of the ore deposits. Mineral paragenesis is complicated by repeated fracturing, but four distinct depositional stages can be recognized; (I) tungsten-molybdenum minerals-quartz-chlorite stage, (II) iron-oxide and sulfides-quartz stage, (III) iron -oxide-base metal sulfides-sulfosalts-quartz-carbonates stage, (IV) barren rhodochrosite-zeolite stage. Fluid inclusion studies were carried out for stage I quartz and stage III quartz, sphalerite and calcite. Fluid inclusion studies reveals highly systematic trends of homogenization temperature and salinity throughout the mineralization. Ore fluids during stage I were complex, NaCl rich brine and salinity reached values as high as 34.4 weight percent equivalent NaCl, but the later ore fluids were more dilute and reached to 9.7 weight percent equivalent NaCl during stage III. Intermittent boiling of ore fluid during stage I is indicated by the fluid inclusions in stage I quartz. Depositional temperatures and pressures during stage I range from $520^{\circ}C$ to $265^{\circ}C$and from 600 to 400 bars. Homogenization temperatures of the stage III quartz, sphalerite and calcite range from $305^{\circ}C$ to $190^{\circ}C$. Fluid inclusion data from the Dongbo mine are nearly similar to those from other hydrothermal tungsten deposits in the Kyeongsang basin. Depositional temperature and salinity of ore fluids during precipitation of tungsten-molybdenum minerals in Dongbo mine were much higher, but $CO_2$ contents were much lower than those from hydrothermal tungsten-molybdenum deposits of late Cretaceous plutonic association in central parts of Korean peninsula.

• 자원환경지질
• /
• 제24권2호
• /
• pp.151-165
• /
• 1991

The Au-Ag deposits of the Euiseong area occurred in quartz veins which filled fissures in Cretaceous sedimentary and volcanic rocks. These ore veins can be classified in two types of deposits based on metallic mineral assemblages as follow: a pyrite type gold-silver deposit (Hoedong mine), characterized by Cu sulfides with Au-Ag alloy, and a Sb-rich silver deposit (Keumdongdo mine), characterized by base metal with Ag-bearing sulfosalts. Mineralogic and fluid inclusion evidences suggest that the ore minerals of these deposits was deposited from initial high temperatures (near $350^{\circ}C$) to later lower temperatures ($200^{\circ}C$) with moderate salinity fluids ranging from 5.8 to 3.8 eq. wt. % NaCl. The gold-silver mineralization of the Hoedong mine occurred at temperatures between 300 and $200^{\circ}C$ from fluids with log $f_{s_2}$ of -10 ~ -16 atm. The antimony - silver mineralization of the Keumdongdo mine were deposited at the higher temperatures (350 to $250^{\circ}C$) and $f_{S_2}$ (-10 ~ -13 atm) than gold mineralization of the Hoedong mine. The calculated log f02 of fluids at $250^{\circ}C$ in two deposits are -32 to -34 atm and -36.5 to -38.5 atm, respectively. Boiling evidences indicate that the ore mineralization of the Hoedong mine occurred at more shallow depth (0.5km) than that (1km) of the Keumdongdo mine. The above differences of depositional environments between two deposits caused the compositional changes of ore minerals such as electrum and sphalerite.

• 자원환경지질
• /
• 제24권2호
• /
• pp.107-129
• /
• 1991

The Yonghwa gold-silver deposits are emplaced along $N15^{\circ}{\sim}25^{\circ}W$ trending fissures in middle Cretaceous porphyritic granite or Precambrian Sobaegsan gneiss complex. The results of paragenetic studies suggest that vein filling can be subdivided into four identifiable stages; state I: the main sulfide stage, characterized by base-metal sulfide minerals, iron oxides and minor electrum, stage II: electrum stage, stage III: electrum and silver-bearing sulfosalts stage, stage IV: post ore stage of carbonates and quartz. The ore mineralogy suggests that depositional temperature of the formation of the gold and silver minerals are estimated as 200 to $250^{\circ}C$ and 140 to $180^{\circ}C$, respectively. Sulfur fugacity of the formation of the gold and silver minerals are estimated as $10^{-14.0}$ to $10^{-12.2}$ atm and $10^{-18.5}$ to $10^{-17.2}$ atm, respectively. A consideration of the pressure regime during ore deposition bases on the fluid inclusion evidence of boiling suggests lithostatic pressure of less than 180 bars. This range of pressure indicate that vein system lay at depth of 700m below the surface at the time during mineralization. Salinities of ore-bearing fluids range from 0.4 to 6.9 wt.% equivalent NaCl. The sulfur and carbon isotopic data reveal that these elements were probably derived from a deep-seated source. The ${\delta}^{18}O$ of the hydrothermal fluid was determined from ${\delta}^{18}O$ values of quartz and calcite. Oxygen and hydrogen isotopic studies reveal that meteoric water dominate over ore-bearing fluid.

• 센서학회지
• /
• 제10권2호
• /
• pp.108-117
• /
• 2001

폭발성 및 가연성 가스의 종류 및 그 정량화론 위한 10개의 개별 센서가 하나의 기판 위에 집적시킨 센서 어레이를 개발하였다. 이 센서어레이는 여러 가지 가연성 가스(부탄, 메탄, 프로판, 일산화탄소, LPG)에 대해서 차별화 된 감도 패턴을 가지도록, 나노 사이즈의 grain를 가지는 $SnO_2$를 모 물질로 하는 10개의 서로 다근 감지 물질로 구성하였고, 센서어레이 전반에서 균일한 온도 분포가 되도록 히터를 기판에 내장시켰다. $400^{\circ}C$에서 동작하는 어레이상의 센서들은 저농도에서도 고감도와 재현성의 특성을 보여 주었다. 이들 감도패턴을 이용하여, 주성분 분석 기법을 통해 환경기준치(LEL, TLV) 범위에서 부탄, 프로판, 메탄, LPG의 폭발성 및 가연성 가스의 종류 인식 및 정량화 할 수 있었다. 그리고, 주성분 분석 기법으로 치적 센서 개수 선정에 응용하였다.

• 공업화학
• /
• 제10권2호
• /
• pp.225-230
• /
• 1999

Li(DPM)을 원료로 hot wall 수평 관형 반응기를 이용하여 질소-산소 및 아르곤-산소의 분위기에서 $Li_2O$ 고체박막을 LPMOCVD법으로 합성하였다. XRD와 ESCA 분석으로부터 질소-산소 분위기에서는 $Li_2CO_3$막이, 아르곤-산소의 분위기에서는 $Li_2O$막이 성장하였음을 알아냈다. 성막된 산화리튬과 리튬카보네이트는 기판의 실리콘 성분과 반응하여 실리케이트를 형성하였다. 마이크로 trench법과 Monte Carlo 시뮬레이션에 의해 기상반응 속도상수 및 표면반응 속도상수가 얻어졌으며 이를 이용한 성막속도 계산치와 실험치를 비교한 결과 실험조건범위 내에서 잘 일치하였다.

• 자원환경지질
• /
• 제18권3호
• /
• pp.225-237
• /
• 1985

Mineralization of Daehwa and Donsan W-Mo deposits can be devided into three distinct depositional stages on the basis of mineral paragenesis and flnid inclusion studies; stage I, deposition of oxides and silicates ; stage II, deposition of base-metal sulfides and sulfosalts with carbonates; stage III, deposition of barren calcite and fluorite. Tungsten, molybdenum and tin mineralization occurred in stage I. Fluid inclusion studies reveal that ore fluid of stage I were homogeneous $H_2O-CO_2$ fluids containing 3.5~14.6 mol % $CO_2$. Minimum temperature and pressure of stage I ore fluids were $240^{\circ}C$ and 500 bars respectively. Salinities of aqueous type I inclusions in minerals of stage I range from 3.7 to 7.6 wt. % equi. NaCl. whereas those of $CO_2$-containing type III inclusions range from 0.3 to 4.4 wt. %. Temperatures of stage II ore fluids range from 200 to $305^{\circ}C$ on the whole and salinities were in the range of 3.2~7.2 wt. %. Homogenization temperatures of fluid inclusions in calcite and fluorite of stage III range from 114 to $186^{\circ}C$ and salinities were in the range of 0.9~4.3 wt. %. Sulfur fugacities during stage II deduced from mineral assemblages and tamperature data from fluid inclusions declined from earlier to later in the range of $10^{-11}{\sim}10^{-18}atm$. Fluid inclusion evidences suggest that the dominance of $CO_2$ in ore fluid during W-Mo mineralization is the characteristic features of Cretaceous W-Mo deposits of central district of Korea compared to those of Kyeongsang basin district.

• 분석과학
• /
• 제11권6호
• /
• pp.452-459
• /
• 1998

수산계 폐기물로부터 분리한 chitin을 epichlorohydrin과 반응시켜 가교 chitin을 제조한 후 탈아세틸화하여 가교 chitosan을 제조하였다. 가교 chitosan-OH를 가교 chitosan-Cl로 전환시킨 뒤 킬레이트 시약인 2,2'-Iminodibenzoic acid 염과 반응시켜 킬레이트 흡착제인 2,2'-Iminodibenzoic acid-가교 chitosan을 합성하였다. 그리고 합성된 흡착제를 이용하여 Pb(II), Cu(II), Cd(II)의 흡착과 회수 특성을 연구하였다. 흡착특성에 대한 실험 결과, pH가 증가할수록 흡착되는 금속 이온의 양이 증가함을 알 수 있었다. 최적 반응시간은 1시간, 흡착력은 Cu(II)