• 대한한의학방제학회지
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• 제14권1호
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• pp.82-104
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• 2006

Objectives: The aim of this study is to find the therapeutic meaning of the Pyrite in herbal medication. Methods: About the origin, the component, the processing the drug, the properties and tastes of drugs, the meridian tropism, the effects, the treating disease, the contraindication and the method of administration. We have researched thirty three literatures to mention the pyrite in time sequence. Results: 1. The pyrite belongs to the metallic herbs and it consists of Iron sulfide, sometimes containing small amounts of cobalt, nickel. silver, and gold. 2. The processing the drug are the tempering, the annealing with vinegar. the refining drug with water or RADIX GLYCYRRHIZAE and et cetra, and accoring to these methods, the pyrite classified into three groups - the rough pyrite, the tempered pyrite, the annealed pyrite. 3. The properties and tastes of drugs is pungent and regular. If pyrite is well refine, it is nearly safe form the metallic virulence. the meridian tropism is mainly liver meridian. 4. From old times, pyrite has come into general use to treat the injury of muscles and tendons and bone facture because it is effective on dissipating blood stasis, alleviating pain and reunion of bone, muscles and ligament. 5. When the symptom is gone, a medicine to contain pyrite must be stoped taking. Because of pyrite's effect on regulateing Gi and promoting blood flow. Conclusions: This study showed that the pyrite is useful herb to treat the injury of muscles and tendons and bone facture.

• 자원환경지질
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• 제54권2호
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• pp.213-232
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• 2021

Ore criteria at the Sheba Deposit indicate orogenic mineralization type. Rocks and mineral assemblages suggest low formation-temperature of green-schist facies. Pyrite found in two generations; Type1 is irregular grains, contains higher arsenic and gold contents, compared to the relatively younger phase Type2 pyrite, which is composed of euhedral grains, found adjacent to late quartz-carbonate veins or at rims of type1 pyrite. Two gold generations were identified; type1 found included in sulphides (mainly pyrite). The second gold type was remobilized (secondary) into free-lodes within silicates (mainly quartz). Gold fineness is high, as gold contains up to 95 wt. % Au, Ag up to 3.5 wt. %, and traces of Cu, Ni, and Fe. Pyrite type2 contains tiny mineral domains (rich in Al, Mn, Hg, Se, Ti, V, and Cr). Zoning, and replacement textures are common, suggesting multiple mineralization stages. The distribution and relationships of trace elements in pyrite type2 indicate three formation patterns: (1) Al, Mn, Hg, Se, Ti, V, Cr, and Sn are homogeneously distributed in pyrite, reflecting a synchronous formation. (2) As, Ni, Co, Zn, and Sb display heterogeneous distribution pattern in pyrite, which may indicate post-formation existence due to other activities. (3) Au and Ag show both distribution patterns within pyrite, suggesting that gold is found both in microscopic phases and as chemically bounded phase.

• Ecology and Resilient Infrastructure
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• 제3권4호
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• pp.279-284
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• 2016

선광 및 제련과 같은 광산활동 과정에 발생하는 광미는 고농도의 중금속을 함유하고 있고, 그 중 황철석을 함유한 광미는 광산주변 수계 및 토양 오염의 주요 원인이다. 이러한 황철석을 함유한 광미의 무해화를 위해 화학전지 (연료전지)의 개념을 활용할 수 있다. 화학전지에서 황철석의 자발적인 산화, 즉, 갈바닉 산화를 통해 황철석이 용해되면서 $Fe^{3+}$와 황산이 생성되어 pH가 감소하게 된다. 이는 황철석 함유 광미 내 중금속의 용출 촉진 효과를 가져올 수 있다. 본 연구에서는 $23^{\circ}C$ 조건에서 4주 간 산성용액과 갈바닉 반응기를 이용해 황철석을 처리하며 총 용존 철 농도와 용액의 pH를 확인하였다. 또한 주사전자현미경을 이용해 처리 후 황철석 표면을 관찰하였다. 갈바닉 반응기를 이용한 황철석의 용해가 산성용액을 이용한 황철석의 용해에 비해 약 2.9배 높은 총 철을 용출시킨 것을 확인하였고, pH 저감 효과도 더 큰 것을 확인하였다. 또한 표면 분석 결과 갈바닉 반응기 내에서 반응한 황철석의 표면에서 더 많은 홈을 발견되었다. 본 연구를 통해 갈바닉 산화에 의해 황철석의 용해가 촉진된 것을 확인하였으며, 갈바닉 산화가 황철석 함유 광미의 무해화 기술로 사용될 수 있는 가능성을 확인하였다.

• 한국결정성장학회:학술대회논문집
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• 한국결정성장학회 1997년도 Proceedings of the 12th KACG Technical Meeting and the 4th Korea-Japan EMGS (Electronic Materials Growth Symposium)
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• pp.53-60
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• 1997

The roasting of pyrite with a cyclone reactor have been studied in terms of investigating the reaction behavior of pyrite. The development of a fundamental model for pyrite oxidation and lime sulfation in a vertical cyclone reactor. The model assumes a chemical control shrinking core behavior for the pyrite and a fluid film control shrinking core behavior for the lime. The oxygen and sulphur dioxide concentrations and the energy balance for the gas, pyrite and lime particles are solved. The model was solved and characterized numerically. Experiments have been performed to study the influence of reaction parameters such as reactor temperatures, pyrite particle sizes, air flow rates, feeding rates, and mixing ratio of pyrite and lime. The oxidation and sulfation products were characterized chemically and physically.

• 공업화학
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• 제25권2호
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• pp.161-166
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• 2014

본 연구에서는 열전지용 양극활물질로 사용되는 $FeS_2$ (Pyrite) 분말을 볼밀링법으로 분쇄하여 단위전지를 제작하고, 볼밀 전, 후 입자크기변화가 열전지의 전기화학적 특성에 미치는 영향을 고찰하였다. $450^{\circ}C$ 시험결과, 분쇄된 $1.46{\mu}m$ $FeS_2$ 분말을 사용한 단위전지가 분쇄 전 $98.4{\mu}m$의 $FeS_2$ 분말을 사용한 단위전지에 비해서 전지용량이 크게 향상되었으며, 내부저항도 감소되었다. 이러한 결과는 볼밀로 인한 비표면적 증가의 영향으로 판단된다. 반면, $500^{\circ}C$에서 방전시 1단계의 Z-phase 반응구간($FeS_2{\rightarrow}Li_3Fe_2S_4$)에서 $1.46{\mu}m$ 분말을 사용한 단위전지 전압 및 저항특성이 우수하였지만, 2단계의 J-phase 반응($Li_3Fe_2S_4{\rightarrow}LiFe_2S_4$)에서는 볼밀된 $1.46{\mu}m$ 분말을 사용한 전지의 전압이 감소하고, 전지 내부저항도 급격하게 증가하는 경향을 보였다. 이러한 현상은 $500^{\circ}C$ 방전시 미분화된 $FeS_2$가 Z-phase 영역에서 방전반응과 동시에 열분해에 의한 자가방전($FeS_2{\rightarrow}FeS_{1.14}$ (pyrrhotite))이 일어나 볼밀 전 조대한(coarsen) $FeS_2$ 분말에 비해 용량이 감소하고 내부 저항도 증가되기 때문으로 사료된다.

• 한국토양비료학회지
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• 제44권2호
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• pp.297-302
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• 2011

Acid drainage generated by pyrite oxidation has caused the acidification of soil and surface water, the heavy metal contamination and the corrosion of structures in abandoned mine and construction sites. The applicability of Na-acetate (Na-OAc) buffer and/or Na-silicate solution was tested for suppressing pyrite oxidation by reacting pyrite containing rock and treating solution and by analyzing solution chemistry after the reaction. A finely ground Mesozoic andesite containing 10.99% of pyrite and four types of reacting solutions were used in the applicability test: 1) $H_2O_2$, 2) $H_2O_2$ and Na-silicate, 3) $H_2O_2$ and 0.01M Na-OAc buffer at pH 6.0, and 4) $H_2O_2$, Na-silicate and 0.01M Na-OAc buffer at pH 6.0. The pH in the solution after the reaction with the andesite sample and the solutions was decreased with increasing the initial $H_2O_2$ concentration but the concentrations of Fe and $SO_4^{2-}$ were increased 10 - 20 times. However, the pH of the solution after the reaction increased and the concentrations of Fe and $SO_4^{2-}$ decreased in the presence of Na-acetate buffer and with increasing Na-silicate concentration at the same $H_2O_2$ concentration. The solution chemistry indicates that Na-OAc buffer and Na-silicate suppress the oxidation of pyrite due to the formation of Fe-hydroxide and Fe-silicate complex and their coating on the pyrite surface. The effect of Na-OAc buffer and Na-silicate on reduction of pyrite oxidation was also confirmed with the surface examination of pyrite using scanning electron microscopy (SEM). The result of this study implies that the treatment of pyrite containing material with the Na-OAc buffer and Na-silicate solution reduces the generation of acid drainage.

• Advances in nano research
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• 제1권4호
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• pp.219-228
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• 2013

We report on the preparation of iron pyrite ($FeS_2$) using pulsed electron ablation of two targets, namely, a mixture of sulfur and iron compound target, and a natural iron pyrite target. Thin films of around 50 nm in thickness have been deposited on glass substrates under Argon background gas at 3 mTorr, and at a substrate temperature of up to $450^{\circ}C$. The thin films have been analyzed chemically and examined structurally using x-ray diffraction (XRD), x-ray photoelectron spectroscopy (XPS), and visible Raman spectroscopy. The morphology and thickness of the films have been assessed using scanning electron microscopy (SEM) and visible spectroscopic reflectance. The preliminary findings, using a synthetic target, show the presence of iron pyrite with increasing proportion as substrate temperature is increased from $150^{\circ}C$ to $250^{\circ}C$. The data have not shown any evidence of pyrite in the deposited films from a natural target.

• 한국결정성장학회지
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• 제9권1호
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• pp.119-125
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• 1999

본 연구는 싸이클론 반응로에서 $FeS_{2}$의 반응 특성에 관한 조사를 연구하였다. 수학적인 모형도로 이 반응로에서 $FeS_{2}$의 oxidation과 suifation 등을 전개하엿다. 모형은 $FeS_{2}$에서 chemical control shrinking core로서 그리고 ${Ca(OH)}_{2}$에서 fluid film control shrinking core로서 가정하였으며 수식으로서 발전시켰다. 본 실험은 이 반응 파라메터들의 영향에 연구로서 진행하였으며 즉 반응로의 온도변화, $FeS_{2}$의 입자크기, 공기 주입비율, 시료 주입비율, 그리고 $FeS_{2}$와 ${Ca(OH)}_{2}$ 비율 등이다. Oxidation과 Sulfation에 의한 반응물들은 화학적 및 물리적으로 특성을 기술하였다.

• KSBB Journal
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• 제16권3호
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• pp.295-301
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• 2001

Thiobacillus ferrooxid,$\alpha$ns와 pyrite 광석을 연마하여 resin에 고정한 시편을 대상으로 침출 시간에 따른 표면의 특성 변화를 EPMA 및 SEM-EDS를 이용하여 이미지와 원소구성비율에 따라 살펴보았다. 침출이 진행됨에 따라 표면의 철성분은 전체적으로 증가한 반면 원소황은 감소하는 경향을 나타냈다. 고배율에 익한 SEM 이미지에서 침출이 진행됨에 따라 도덧모양의 생성물이 침출 13일 경과 시점에 서 나타나 23일 경과 후까지 자라났으나 30일 경과 시점 에서는 표면전체에 새로운 층 생성된 결과로 나타났다. SEM 이미지 상에서 spot과 배경 지접의 원소 구성비를 EDS에 의하여 분석한 후 비교한 결과 초기에는 원소 구성비의 차이가 큰 값을 보이나 침출이 증가함에 따라 좌이가 나 지 않으며 이는 칩풀이 진행됨에 따라 pyrite 표면변이 접차 생성불이 칩착 되는 것으로 볼 수 있었다.

• 한국제4기학회:학술대회논문집
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• 한국제4기학회 2005년도 추계학술대회
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• pp.34-39
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• 2005

A 120-cm core recovered from Lake Hovsgol, the northern Mongolia provides evidence for climate variability since the Marine Isotope Stage 3, representing a sharp lithological change. The lowermost part of the core consists of diatom-barren calcareous silty clay without coarse sands, framboidal pyrite, and biogenic components deposited during the MIS 3. Following the last glacial maximum, in-situ moss is included in the sediments, as lake-level was retreated by cold and dry environment with low precipitation. The AMS radiocarbon ages of the plant fragments match a marked lithologic boundary between 14,060 and 14,325 $^{14}C$ yr BP. The contents of coarse sands abruptly increase, indicating probably wind-derived sandy dust or coarse grains contributed from floating icebergs. And abundant framboidal pyrite grains were deposited in an anoxic environment, as reflected by high accumulation of organic matters at a low lake stand. During the deglaciation, quantities of coarse sands, ostracod, shell fragments, framboidal pyrite, and diatom markedly varies by regional and global scale climate regimes. Some allochthonous coarse sands were probably ice-rafted debris derived from floating icebergs. A rapid increase in diatom productivity probably marked the onset of Bolling-Allerodwarming. Subsequent high concentration of framboidal pyrite probably represents a dry and cold condition, such as Younger Drays events. Consistent warm period with high precipitation at Holocene is documented by diatomaceous clayey ooze without framboidal pyrite, coarse sands, and ostracod.