• 한국광물학회지
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• 제24권3호
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• pp.189-194
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• 2011

화성의 암권 진화 연구에서 최근 각광받는 광물은 적철석으로 대표되는 3가철 산화물이다. 물리적 방법의 하나인 잔류자화기억도 실험은 비파괴적이고 지구 기원이 아닌 고체 시료의 자화특성 규명에 유용하게 사용된다. 금번 연구에서는 알루미늄 농도를 조절하며 열수반응과 탈수반응을 통해 총 8개 성분의 3 가철 산화물을 합성하였다. 이들 시료에 대해 잔류자화기억도와 자화상실온도($T_N$)를 측정하였다. 3가철 산화물의 격자상수는 알루미늄의 3가철 함량이 증가하며 감소한다. 3 가철 산화물의 자화상실 온도 역시 알루미늄의 몰농도가 증가하며 감소한다. 알루미늄이 거의 첨가되지 않은 적철석의 $T_N$은 광물의 합성방법과 무관하게 대략 $690^{\circ}C$로 수렴한다. 탈수반응으로 합성된 3가철 산화물의 잔류자화기억도는 알루미늄의 함량에 거의 무관하게 매우 높지만, 열수반응으로 합성된 3가철 산화물의 잔류자화기억도는 알루미늄 함량이 증가하며 동반 상승한다. 상대적으로 쉽고 측정이 간단하며 비파괴적인 잔류자화기억도를 이용하면 추후 암석 내 3가철 산화물 입자의 성인 유추가 가능하며, 특히 화성의 암권 진화 규명에도 일조하리라 예상된다.

• Bulletin of the Korean Chemical Society
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• 제30권11호
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• pp.2577-2583
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• 2009

Presented are the formation of iron oxide layers on evaporator tubes in an actual fossil power plant operated under all volatile treatment (AVT) condition and an experimental simulation of iron oxide formation in the presence of ferrous and ferric ions. After actual operations for 12781 and 36326 hr in the power plant, two iron oxide layers of magnetite on the evaporator tubes were found: a continuous inner layer and a porous outer layer. The experimental simulation (i.e., artificial corrosion in the presence of ferrous and ferric ions at 100 ppm level for 100 hr) reveals that ferrous ions turn the continuous inner oxide layer on tube metal to cracks and pores, while ferric ions facilitate the production of porous outer oxide layer consisting of large crystallites. Based on a comparison of the oxide layers produced in the experimental simulation with those observed on the actually used tubes, we propose possible routes for oxid layer formation schematically. In addition, the limits of the proposed corrosion routes are discussed in detail.

• 한국세라믹학회지
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• 제48권2호
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• pp.117-120
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• 2011

In this study, the redox state of iron in sodium silicate glasses was varied by changing the melting conditions, such as the melting temperature and particle size of iron oxide. The oxidation states of the iron ion were determined by wet chemical analysis and UV-Vis spectroscopy methods. Iron commonly exists as an equilibrium mixture of ferrous ions, $Fe^{2+}$, and ferric ions $Fe^{3+}$. In this study, sodium silicate glasses containing nanoparticles of iron oxide (0.5% mol) were prepared at various temperatures. Increase of temperature led to the transformation of ferric ions to ferrous ions, and the intensity of the ferrous peak in 1050 nm increased. Nanoparticle iron oxide caused fewer ferrous ions to be formed and the $\frac{Fe^{2+}}{Fe^{3+}}$ equilibrium ratio compared to that with micro-oxide iron powder was lower.

• 한국세라믹학회지
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• 제24권3호
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• pp.215-222
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• 1987

${\alpha}$-Ferric Hydrous Oxide and ${\alpha}$-Ferric Oxide were obtained as following processes that Ferric Nitrate solution was adjusted to pH 6-8 with Ammonium Hydroxide, refluxed the Iron precipitate for 1 hr. at 80$^{\circ}C$, washed it with water and Methanol (95%), dried it to obtain ${\alpha}$-Ferric Hydrous Oxide at 60$^{\circ}C$, and then heated in atmosphere to prepare ${\alpha}$-Ferric Oxide for 1 hr. at 450$^{\circ}C$. Mica particles cleaned with ultrasonicator (45KHz) in water were mixed with Ferric Nitrate solution and treated it to adsorb ${\alpha}$-Ferric Oxide on the surface of mica particles by using the abovementioned processes, but the heated temperature was at 500$^{\circ}C$. The maximum wavelength of reflected light on the surface of mica-${\alpha}$-Ferric Oxide (50%) was appeared at 546nm but -Ferric Oxide free mica only was at 436 nm. The maximum wavelength was shifted to longer when the weight ratios of ${\alpha}$-Ferric Oxide to mica was changed from 1% to 50%.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2002년도 총회 및 춘계학술발표회
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• pp.250-253
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• 2002

Remediation of groundwater using zero valent iron filings has received considerable attention in recent years. However, zero valent iron is gradually transformed to iron(III) oxides at permeable reactive barriers, so the reduction of iron(III) oxides can enhance the longevity of the reactive barriers. In this study, microbial reduction of Fe(III) was performed in anaerobic condition. A medium contained nutrients similar to soil solution. The medium was autoclaved and deoxygenated by purging with 99.99% $N_2$ and pH was buffered to 6, while the temperature was regulated as 2$0^{\circ}C$. Activity of iron reducing bacteria were not affected by chlorinated organics but affected by iron(III) oxide. Although perchloroethylene(PCE) was not degraded with only ferric oxide, PCE was reduced to around 50% with ferric oxide and microorganism. It shows that reduced iron can dechlorinate PCE.

• 한국재료학회지
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• 제20권6호
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• pp.301-306
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• 2010

The chemical formula of magnetite ($Fe_3O_4$) is $FeO{\cdot}Fe_2O_3$, t magnetite being composed of divalent ferrous ion and trivalent ferric ion. In this study, the influence of the coexistence of ferrous and ferric ion on the formation of iron oxide was investigated. The effect of the co-precipitation parameters (equivalent ratio and reaction temperature) on the formation of iron oxide was investigated using ferric sulfate, ferrous sulfate and ammonia. The equivalent ratio was varied from 0.1 to 3.0 and the reaction temperature was varied from 25 to 75. The concentration of the three starting solutions was 0.01mole. Jarosite was formed when equivalent ratios were 0.1-0.25 and jarosite, goethite, magnetite were formed when equivalent ratios were 0.25-0.6. Single-phase magnetite was formed when the equivalent ratio was above 0.65. The crystallite size and median particle size of the magnetite decreased when the equivalent ratio was increased from 0.65 to 3.0. However, the crystallite size and median particle size of the magnetite increased when the reaction temperature was increased from $25^{\circ}C$ to $75^{\circ}C$. When ferric and ferrous sulfates were used together, the synthetic conditions to get single phase magnetite became simpler than when ferrous sulfate was used alone because of the co-existence of $Fe^{2+}$ and $Fe^{3+}$ in the solution.

• 대한환경공학회지
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• 제27권2호
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• pp.123-129
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• 2005

철을 이용한 반응벽체 (permeable reactive barrier, PRBs) 기술은 유기 화합물로 오염된 지하수를 환원적 반응에 의해 정화시키는 공법이다. 벽체의 매질로 주로 사용되는 영가 철은 반응이 진행됨에 따라 점차 2가 및 3가 철로 산화되어 제거능이 점차 저감된다. 자연계에 존재하거나 동정된 철 환원 박테리아는 산화된 Fe(III)를 Fe(II)로 환원시키는 능력을 가지고 있으며 이와 같이 환원된 Fe(II)는 반응 표면적을 넓히고 다시 할로겐 유기 화합물을 환원적으로 제거할 수 있도록 한다. 본 연구는 철 환원 박테리아로 순수균인 Shewanella algae BrY에 의한 산화철의 환원 경향을 aqueous phase와 solid phase로 나누어 관찰하고 환원된 철이 TCE 제거에 미치는 영향을 iron(II,III) oxide와 iron(III) oxide를 대상으로 하여 파악하는 것을 목표로 하였다. 박테리아는 배지 내에 존재하는 Fe(III)를 우선적으로 사용하여 Fe(II)로 환원시켰으며 선택성은 떨어지지만 입자상의 산화철 표면에 존재하는 Fe(III)도 환원시켰다. 또한 동량의 산화철이 존재할 때 iron(II,III) oxide에 비해 박테리아가 전자수용체로 사용할 수 있는 Fe(III)가 풍부한 iron(III) oxide의 환원이 더 잘 일어남을 알 수 있었고, 환원된 Fe(II)는 박테리아 또는 다른 철 산화물과 침전을 형성하였으며 TCE와의 반응속도 및 제거 능력을 향상시키는 것으로 판단된다.

• 한국추진공학회지
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• 제22권3호
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• pp.65-71
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• 2018

황색 산화철과 적색 산화철을 적용한 추진제의 초기점도는 각각 5.4, 5.6 kps로 특이한 차이점이 없었다. 또한 황색 산화철을 첨가한 물질의 열분해 속도가 적색 산화철을 첨가한 것 보다 빠르게 진행되며, 특히 고온 고압에서의 압력지수가 18% 낮은 것을 확인하였다. 황색 산화철을 적용한 추진제의 산화제 비율 변화에 따른 점도를 비교하면 큰 입자/작은 입자 비율 71%일 때 초기점도가 가장 낮았다.

• Nuclear Engineering and Technology
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• 제51권3호
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• pp.738-745
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• 2019

Coprecipitation using hydrous ferric oxide (HFO) has been effectively used for the removal of radionuclides from radioactive wastewater. This work studied the dynamic behavior of HFO floc formation during the neutralization of acidic ferric iron in the presence of several radionuclides by using a photometric dispersion analyzer (PDA). Then the coagulation-flocculation system using HFO-anionic poly acrylamide (PAM) composite floc system was evaluated and compared in seawater and distilled water to find the effective condition to remove the target nuclides (Co-60, Mn-54, Sb-125, and Ru-106) present in wastewater generated in the severe accident of nuclear power plant like Fukushima Daiichi case. A ferric iron dosage of 10 ppm for the formation of HFO was suitable in terms of fast formation of HFO flocs without induction time, and maximum total removal yield of radioactivity from the wastewater. The settling time of HFO flocs was reduced by changing them to HFO-PAM composite floc. The optimal dosage of anionic PAM for HFO-anionic PAM floc system was approximately 1-10 ppm. The total removal yield of Mn-54, Co-60, Sb-125, Ru-106 radionuclides by the HFO-anionic PAM coagulation-flocculation system was higher in distilled water than in seawater and was more than 99%.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 INTERNATIONAL SYMPOSIUM ON SOIL & GROUNDWATER ENVIRONMENT
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• pp.123-125
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• 2005