• 자원환경지질
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• 제32권3호
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• pp.293-306
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• 1999

The lower Permian jungseong Formation, Taebaegsan basin (Baegunsan Syncline), represents a coal-bearing siliciclastic succession which was later modified by the Songrim or Dabo orogeny. Sandstone perography and clay mineralogy were studied to understand the thermal history of the Jangseong Formation during basin evolution. Petrographic study indicates the Jangseong sandstones are composed of quartz, feldspar, lithic fragments (metamorphic and sedimetary), and varying proportions of matrix and cement. The dominance of quartz(<97%) over feldspar (<1%) and lithic fragments (<2%) classifies most Jangseong sandstones as quartz arenotes or quartzwackes, but lithic graywackes and sublithic arenite locally occur. The diagentic features of these sandstones include mechanical compaction, cemenation by quartz and clay minerals indentified in the Jangseong Formation by X-ray diffraction analysis are late-stage clay pore-filling. Clay minerals isdentified in the Jangseong Formation by X-ray diffaction analysis are illite, kaolinte, and pyrophyllite with a minor amount of chlorite and micas. The illite, kaolinite, and pyrophyllite appear to be largely autjigenic based on their well-crystallinity forms. There authigenic clay minerals form clay minerals form clay coats/rims and late-stage pore-filling cements, Illitecrystallinity shows that the Jangseong formation has been in late-diagenetic zone to early-epizone, which ranges in temperature from $200^{\circ}C$ to $300^{\circ}C$. In assition, kaolinite-pyrophyllite transition suggests that paleotemperature of the formation has reached at least $265^{\circ}C$. Such temperatureis likely to be consistent with homogenixation temperatures of fluid inclusions in quartz veins in the formation. Thus, the Jangseong Formation has been subjected to paleotemperature of about $265^{\circ}C$. The major heat source responsible for paleotemperature may be hydrothermal solutions. The passage of hydrothermal solutions was probably assisted by fractures created during the basin-modifying tectonism of the taebaegsan basin.

• 한국추진공학회지
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• 제22권1호
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• pp.66-71
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• 2018

에너지 물질의 수명평가는 중요하게 여겨지지만, 여러 가지 어려움을 갖고 있다. 먼저 노화시험에 매우 긴 시간이 소요되고, 에너지 물질이기 때문에 취급 시 항상 위험이 존재한다. 이런 이유들로 인해서 예측이나 계산 방법들이 발달되어 왔다. 에너지 물질은 열을 내놓으면서 분해되기 때문에, 에너지 물질의 열적 특성을 분석하는 것은 에너지 물질의 분해와 노화 특성을 이해하는데 매우 중요하다. 이번 연구에서는 첫째, DSC를 기초데이터로 하여 AKTS software를 이용하여 간단한 열분석으로부터 열적인 노화 특성을 예측하는 결과들을 발표하고, 둘째, AKTS software를 통해 물성측정 점 데이터로부터 적절한 kinetic 모델을 설정하고, 그 모델로부터 노화에 따른 특성변화를 예측하는 결과를 나타내었다.

• 한국산업보건학회지
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• 제33권2호
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• pp.93-102
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• 2023

Objectives: With the evolution of direct reading sensors, it is possible to monitor several substances through telecommunication. However, there are some limitations on the use of direct reading technologies in the Occupational Safety and Health Act in South Korea, which only applies to detector tubes, noise, heat, and carbon monoxides. The number of chemicals and their amount of use have been continuously increasing in South Korea. The Ministry of Employment and Labor (MoEL) has concerns about worker's health because exposure is only covered for about 1.2% of all distributed chemicals. Using a direct reading monitor with photoionization detectors (PID-DRMs), gases and vapors chemicals can be measured. Based on the data, business owners are able to create corrective strategies, provide better working routines, and select correct respiratory equipment. PID-DRMs are less expensive and easier to handle for an owner voluntarily controlling chemicals emitted in the workplace. However, there are several limitations on using these PID-DRMs to the degree that the MoEL has not been able to select a legal monitor. The aim of this study was to review previous studies related to PID-DRMs and identify the characterization and limitation on PID-DRMs. Methods: To search for related studies on PID-DRMs, key words were used including direct reading monitors/instruments and/or photoionization detectors. Through that, four domestic and 15 international studies were reviewed. Results: Studies on PID-DRMs were conducted by chamber (enclosed, dynamic, walk-in) and in the field (experimental environment, actual environment). The concentration of PID-DRMs and charcoal tubes were compared for a single substance or mixture, or within the PID-DRMs. There was a high correlation between the two concentrations, but it did not meet the accuracy criteria (95% confidence interval, within 25%) of the NIOSH technical report (2012). In addition, differences in measured values occurred according to environmental factors (temperature, humidity) and high concentration, and concentration values tended to be underestimated due to contamination of the sensor. As a way to improve the accuracy of PID concentration, it was proposed to use correction factors, charcoal tube-based correction factors, or to calibrate the PID-DRMs in the same environment as the workplace. Conclusions: PID-DRMs can likely be used by business owners for the purpose of voluntarily managing the workplace environment, and it is expected that it will be possible to use them as legal equipment if a PID sensor can be upgraded and the limitations of the sensor (temperature, humidity, high concentration evaluation, sensor pollution) can be overcome in the near future.

• 자원환경지질
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• 제24권2호
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• pp.131-150
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• 1991

시간적-공간적으로 가대리 화강암과 관련되어 형성된 월성 다이아튜림은 천수에서 유래된 용액에 의해 광화되어 있다. 이 광상에서 광석광물은 황철석, 유비철석, 섬아연석이 대부분이고 극소량의 자철석, 자류철석, 황동석, 석석과 Pb-Sb-Bi-Ag 계의 광문이 있다. 유체포유물, 유비철석에서의 비소함량과 섬아연석의 철 함량에 의해 계산된 비소-아연 광화 온도는 약 $350^{\circ}C$에 이르며, 염농도는 0.8에서 4.1 equ. wt % NaCl이다. 공생을 이루는 황철석-자류철석-유비철석은 $H_2S$ 주요 환원황으로 작용했으며, $300^{\circ}C$에서 산출한 광황용액은 $10^{34.5}$ < ${alpha}_{O_2}$ < $10^{-3}$, $10^{-11}$ < $f_{S_2}$ < $10^{-8}$, $10^{-2.4}$ < ${alpha}_{H_2S}$ < $10^{-1.6}$이고 pH는 견운모 안정범위인 5.2이하이다. 유화광물의 유황동위 원소비는 1.8에서 5.5%로서 유황은 마그마에서 기원되었다. 광화대에서의 탄산염 광물의 탄소 동위 원소비는 -7.8에서 -11.6%이고 산소 동위원소 값은 천수의 유입이 있었음을 의미한다. 지화학적 자료로 보아 광화용액은 마그마에 천수가 유입되어 마그마 열원의 영향하에 지하 심부 순환관정을 거쳐 형성된 것으로 해석된다.