• 대한금속재료학회지
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• 제46권1호
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• pp.20-25
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• 2008

The ionic equilibira in mixed solutions of cuprous and cupric chloride were analyzed by considering chemical equilibria, mass and charge balance equations. The activity coefficients of solutes were calculated by using Bromley equation. Required thermodynamic constants and interaction parameters were evaluated from the data reported in the literature. The effect of NaCl and CuCl concentrations on the pH and potential of the mixed solutions was explained in terms of the variation in the concentration of solutes and in the activity of hydrogen ion. The calculated pH values of the mixed solutions agreed well with the measured values. However, the calculated values for the potential of the mixed solutions were lower than the measured values, indicating the necessity of considering the complex formation between cuprous and chloride ion, such as $Cu^2Cl{_4}^{2-}$ and $Cu_3Cl{_6}^{3-}$.

• 생명과학회지
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• 제13권6호
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• pp.788-793
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• 2003

Rhodosporidium toruloides SJ-4의 epoxide hydrolase의 입체선택적 가수분해 반응을 이용하여 hollow-fiber 반응기에서 라세믹 phenyl oxirane 기질로부터 광학활성 phenyl oxirane을 생산하였다. 라세믹 에폭사이드 기질의 수용액 상에서의 낮은 용해도로 인한 저농도 반응의 문제점을 극복하기 위하여 dodecane 유기용매에 용해시켜 lumen 부위로 공급하였으며, 생촉매인 R. toruloides 세포 현탁액은 수용액강인 shell 부위에 위치시킴으로써 유기용매 사용에 따른 생촉매 활성 저하를 줄인 1단계 반응기 시스템에서는 200 mM의 고농도에서 (S)-phenyl oxirane을 생산할 수 있었다. 또한, 반응 산물로 생성되는 diol에 의한 생촉매 활성저해효과를 감소시키기 위하여 2단계 hollow-fiber 반응기에서는 완충용액을 이용하여 diol을 제거시킨 결과 300 mM에서 EH 활성을 이용한 입체선택적 가수분해반응을 수행할 수 있었으며, 200∼300 mM의 고농도 라세믹 기질로부터 99% ee 이상의 광학순도를 가진 (S)-phenyl oxirane을 이론 수율 대비 12∼35% 수율로 얻을 수 있었다.

• Nuclear Engineering and Technology
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• 제55권4호
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• pp.1439-1447
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• 2023

The fuel cycle characteristics of the IVG.1M reactor were studied within the framework of the research reactor conversion program to modernize the IVG.1M reactor. Optimum use of the nuclear fuel and reactor was achieved through routine methods which included partial fuel reloading combined with scheduled maintenance operations. Since, the additional problem in planning the fuel cycle of the IVG.1M reactor was the poisoning of the beryllium parts of the core, reflector, and control system. An assessment of the residual power and composition of spent fuel is necessary for the selection and justification of the technology for its subsequent management. Computational studies were performed using the MCNP6.1 program and the neutronics model of the IVG.1M reactor. The proposed scheme of annual partial fuel reloading allows for maintaining a high reactor reactivity margin, stabilizing it within 2-4 β_eff for 20 years, and achieving a burnup of 9.9-10.8 MW × day/kg U in the steady state mode of fuel reloading. Spent fuel immediately after unloading from the reactor can be placed in a transport packaging cask for shipping or safely stored in dry storage at the research reactor site.

• 수산경영론집
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• 제42권3호
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• pp.79-93
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• 2011

Water temperature of Oliver flounder farm affects Oliver flounder growth and mortality rate. In laboratory experimental tanks, optimal water temperature was $22.5^{\circ}C$($21{\sim}24^{\circ}C$) and cultivatable water temperature was $12{\sim}28^{\circ}C$. The purpose of this study is to identify applicable and useful water temperature of Oliver flounder farm in case of actual farming. The data applied in the analysis was collected from Jeju island. In the study, various analytical methods including productivity analysis, regression analysis, statistical analysis were conducted for 13 Oliver flounder culture farms. The result of analysis can be summarized as follows : First, growth rate on the Oliver flounder culture farms was related to mean of water temperature, variation of water temperature and low water temperature. Second, survival rate on the Oliver flounder culture farms was related to mean of water temperature. In case of including Oliver flounder stocking density, defined as the surface area of Oliver flounder per $m^2$ of water surface area, survival rate strongly related to mean of water temperature, variation of water temperature, cultivating capability and stocking density. Third, production weight per $m^2$ of water surface area was strongly related to mean of water temperature, low water temperature and cultivating capability. Growth rate and survival rate was analyzed into mediate variable character.

• 수산경영론집
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• 제42권2호
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• pp.85-96
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• 2011

Oliver flounder population density affect Oliver flounder growth and mortality rate. In laboratory pilot experiment, Oliver flounder growth rate is inversely proportional to stocking density. But previous study has not proved external validity. This study is aimed to analyze the effect of stocking density on the Oliver flounder culture farms in Jeju Island. In order to do this, I selected 13 farms in Jeju island as a sample. In the study, various analytical methods including productivity analysis, regression analysis, statistical analysis were conducted for 13 Oliver flounder culture farms. The result of analysis can be summarized as follows. First, in case of the Oliver flounder culture farms, Bertalanffy equation is not applicable to the Oliver flounder growth. Second, the Oliver flounder stocking density, defined as the surface area of Oliver flounder per $m^2$ of water surface area, is preferred to density definition defined as the weight of Oliver flounder per $m^2$ of water surface area on the Oliver Flounder Culture Farms case. Third, growth rate and production weight on the Oliver flounder culture farms are inversely proportional to stocking density on spearman rank correlation test. When extensive comparable biological and culture condition data become available, analysis model can be easily modified to yield more accurate results.

• 한국작물학회지
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• 제38권3호
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• pp.228-234
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• 1993

벼 건답휴립직파재배에서 발아시 토양수분과 입묘율과의 관계를 구명하기 위하여 칠성벼, 가유벼, 삼강벼, 영산벼, 영덕벼, 화진벼, 팔공벼, 섬진벼, 도진벼, 밀양 9005, M101, M202, Newbonnet, Tebonnet, Lemont 등 15개 품종을 공시하여 여러가지 토양수분함량과 복토심을 달리하여 파종시험을 하여 얻은 결과를 요약하면 다음과 같다. 1. 파종 후 4일간 담수하였다가 배수하여도 출아율에는 영향이 없었다. 2. 담수조건에서 1.5cm 복토하였을 때 출아율은 40%이하로 토양표면에 파종한 것보다 출아율이 현저히 낮았고, 품종간에는 영산벼와 섬진벼의 출아율이 가장 높았다. 3. 국장에서 파종 후 상면 10cm까지 관수하여도 출아율에 영향을 미치지 않았다. 4. 토양수분은 관수 및 강우 후 3～6일간은 pF0이었고, 산화환원전위는 443～453mV로 무관수보다 낮았다.

• 한국환경과학회지
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• 제20권8호
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• pp.963-975
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• 2011

For this research, they were monitored $CO_2$ flux and environmental factors ($CO_2$ concentration, soil temperature, soil moisture, soil organic carbon, soil pH, soil Eh) in foreshore, paddy field and woods sites at the winter season (January 2009) and the summer season (September 2009). Seasonal and spatial variations for monitored data were analyzed, and linear regression functions of $CO_2$ flux as environmental factors were estimated. $CO_2$ fluxes averaged between surface and atmosphere monitored in foreshore and paddy field at the winter season were shown $-8\;mgCO_2m^{-2}hr^{-1}$ and $-25\;mgCO_2m^{-2}hr^{-1}$, respectively. $CO_2$ fluxes averaged between surface and atmosphere monitored in foreshore and paddy field at the summer season were shown $47\;mgCO_2m^{-2}hr^{-1}$ and $117\;mgCO_2m^{-2}hr^{-1}$, respectively. Thus, $CO_2$ was sunk from atmosphere to surface at the winter season and it was emitted from surface to atmosphere at the summer season. $CO_2$ fluxes in woods site were emitted $145\;mgCO_2m^{-2}hr^{-1}$ at the winter season and $279\;mgCO_2m^{-2}hr^{-1}$ at the summer season.

• 지질공학
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• 제23권4호
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• pp.363-373
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• 2013

본 연구에서는 폐광된 전남 광양 본정광산의 토양, 산성광산배수 및 수계에 형성된 하상퇴적물에 대해서 거리에 따른 Au 및 중금속의 분포 및 거동특성을 파악하고자 하였다. AMD와 하상퇴적물로부터 Au의 화학적 존재형태 및 지구화학적 특성을 확인하기 위해 왕수분해, 연속추출, XRD 및 이화학 분석을 실시하였다. 폐석적치장 토양과 하상퇴적물에 대한 XRD분석을 실시한 결과 토양에서는 석영, 고령석, 하상퇴적물에서는 석영, 침철석이 관찰되었다. 거리에 따른 산성광산배수의 물리화학분석을 실시한 결과 수계의 pH와 Eh 범위는 각각 3.00에서 3.19, 396에서 450 mV를 나타나고 있다. 산성광산배수의 Au 함량은 0.68~0.97 mg/L 범위로 상류에서 하류로 갈수록 감소하는 경향을 보이며, 하류에서는 불검출로 나타났다. 이는 수계의 Au 함량이 환경적 영향(pH, 산화환원전위, 침전, 흡착)을 받기 때문이다. 거리에 따른 하상퇴적물의 Au 함량은 13.76~22.85 mg/kg의 범위를 보인다. 연속추출을 통한 하상퇴적물의 Au 존재형태는 이온교환성 형태 10.84%, 탄산염 결합형태 11.09%, 철-망간 수산화물 형태 25.53%, 유기물-황 결합형태 26.62% 및 잔류성 형태 24.61%로 나타난다.

• 자원환경지질
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• 제32권5호
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• pp.469-483
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• 1999

Two different types of deep groundwaters occur together in the Jungwon area: $CO_2$-rich water and alkali water. Each water shows distrinct hydrogeochemical and environmental isotopic characteristics. The $CO_2$-rich waters are characterized by lower pH(6.0~6.4), higher Eh (25~85mV) and higher TDS content (up to 3,300 mg/l), whereas the alkali type waters have higher pH (9.1~9.5), lower Eh (-136~-128mV) and lower TDS content (168~254 mg/l). The CO2-rich waters ($Pco_2$=up to 1atm) were probably evolved by the local supply of deep $CO_2$ during the deep circulation, resulting in enhanced dissolution of surrounding rocks to yield high concentrations of $Ca^{2+}, Na^+, Mg^{2+}, K^+\; and \;HCO_3\;^-$ under low pH conditions. On the other hand, the alkali type waters ($Pco_2$=about 10-4.6 atm) were evolved through lesser degrees of simple wate/rock (granite) interaction under the limited suppy of $CO_2$. The alkali waters are relatively enriched in F- (up to 14mg/l), whereas the F- concentration of$CO_2$-rich water is lower (2.2~4.8 mg/l) due to the buffering by precipitation of fluorite. The oxygen-hydrogen isotopes and tritium data indicate that compared to shaltion ($\delta$18O=-9.5~-7.8$\textperthousand$),two different types fo deep groudwaters (<1.0TU)were both derived from pre-thermonuclear (more than 40 years old) meteoric waters with lighter O-H isotopic composition ($\delta$18O=-9.5~-7.8$\textperthousand$) and have evolved through prolonged water/rock interaction. The $CO_2$-rich waters also show some degrees of isotopic re-equilibration with $CO_2$ gas. The $\delta^{34}S$ values of dissolved sulfates (+24.2~+27.6$\textperthousand$) in the $CO_2$-rich waters suggest the reduction of sulfate by organic activity at depths. The carbon isotope data show that dissolved carbon in the $CO_2$-rich waters were possibly derived either from dissolution of calcite or from deep $CO_2$ gas. However, strontium isotope data indicate Ca in the $CO_2$-rich waters were derived mainly from plagioclase in granite, not from hydrothermal calcites.

• 한국광물학회지
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• 제24권2호
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• pp.91-99
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• 2011

울산시에 삼동면에 위치한 천부 관정 지하수들 중 일부는 탁도가 음용수 기준을 크게 초과한다. 광물학적 분석결과, 극미립 부유입자는 지름 $0.5\;{\mu}m$ 이하의 구상 페리하이드라이트(ferrihydrite), 페리하이드라이트로 교대된 나선형 철산화 박테리아 섬유, 그리고 이들의 집합체였다. 페리하이드라이트는 거의 비정질로서 2개의 전자회절환만 관찰되었고, Si와 P가 함유되어 있었다. 나선형 철산화 박테리아는 지하수의 용존 $Fe^{2+}$의 산화뿐만 아니라 페리하이드라이트의 침전 장소를 제공하였다. 주변의 보통 지하수와 비교하여 pH와 Eh가 낮고, Ca 함량과 알칼리도가 높아서 한국 탄산약수의 일반적 수질 특정과 잘 부합되어, 용존철이 풍부한 심부 기원 탄산수의 유입이 추정된다. 따라서 높은 페리하이드라이트 탁도는 pH, Eh, 알칼리도 등의 수질인자와 함께 천부 지하수 관정을 이용한 심부 기원 탄산지하수 추적의 지시자로 활용될 가능성이 있다.