• 한국지하수토양환경학회지:지하수토양환경
• /
• 제16권1호
• /
• pp.82-90
• /
• 2011

Reactive reductants of cement/Fe(II) systems in dechlorinating chlorinated hydrocarbons have not been identified. The previous studies showed that a hematite/CaO/Fe(II) system had TCE degradation characteristics similar to those of cement/Fe(II) systems with regard to degradation kinetics and that lime (CaO) plays an important role in enhancing the reactivity for TCE dechlorination. The current study shows identified the formation of gypsum ($CaSO_4$) in the hematite/CaO/$FeSO_4$ system through the XRD analysis. The amounts of the gypsum increased with increment of the initial CaO dose. However, when CaO in the hematite/CaO/$FeSO_4$ system was replaced with gypsum, TCE degradation was not observed. Ca-removed Portland cement extracts (CPCX) in combination with $FeSO_4(CPCX/FeSO_4)$ showed no TCE degradation. On the other hands, the Portland cement extracts (PCX) in the presence of $FeSO_4(PCX/FeSO_4)$ and CPCX/CaO/$FeSO_4$ systems degraded 0.2 mM TCE within 5 days, indicating that CaO also played an important role dechlorination reactions in the systems. The pseudo-first-order rate constants (k) of the CPCX/CaO/$FeSO_4$ systems were 0.20, 0.24, and 0.72 $day^{-1}$, when the CaO dosages were 25, 50 and 75 g/L, respectively. The XRD analyses showed identified the common peaks having the d-values of 3.02, 2.27, and 1.87 in the reaction systems that showed TCE degradation. However, it was not possible to clearly identify the crystalline minerals having the three peaks from the references in JCPDS cards. This study reveals that the reactive agents in the cement/Fe(II) and the hematite/Fe(II) systems are likely to be those containing CaO and Fe(II).

• 한국세라믹학회지
• /
• 제30권6호
• /
• pp.499-509
• /
• 1993

Structures of hematite(${\alpha}$-Fe2O3), Ba-ferrite(BaFe12O19) and Zn2Y(Ba2Zn2Fe12O22) were studied by powder X-ray diffraction(XRD) method. Powder XRD patterns of the ferrites were analyzed with the Rietveld method, and the final refined R-factors were RWP<0.01 and RI<0.03. The lattice parameters refined with hexagonal crystal system were a=5.0342${\AA}$, c=13.746${\AA}$ for hematite, a=5.8928${\AA}$, c=23.201${\AA}$ for Ba-ferrite, and a=5.8763${\AA}$, c=43.567${\AA}$ for Zn2Y. In the hematite, the oxygen parameter is 0.3072 and the Fe-O distances in FeO6octahedron are 1.941${\AA}$ and 2.118${\AA}$, close to the single crystal data of Blake et al.. In the Ba-ferrite, the Fe atom in oxygen trigonal bipyramid is displaced 0.155${\AA}$ away from the BaO3 mirror plane into 4e position. In the Zn2Y, 75% of Zn is located at the oxygen terahedral site in S-block.

• 한국자기학회지
• /
• 제17권5호
• /
• pp.205-209
• /
• 2007

제주도 중북부 산간 지대 일원에 형성된 오름에서 채취한 스코리아의 화학적 조성, 산화철의 원자가상태와 자기적 성질을 조사하였다. X-선 형광분석으로부터 철 함유량은 $12.01{\sim}13.57\;wt%$ 이었고, X-선 회절법을 이용하여 $SiO_2$와 같은 규산염 외에 소량의 철산화물을 확인할 수 있었다. $M{\ddot{o}}ssbauer$ 분광법을 통해 광물 내의 철 성분들이 어떤 형태를 이루는지 확인하였다. 측정한 시료들로부터 olivine인 규산염과 pyroxene, ilmenite와 같은 상자성 철산화물 및 상온에서 반강자성 및 강자성 물질인 hematite와 magnetite 산화철 광물을 확인하였다. 철 화합물의 원자가 상태는 일부 $Fe^{2+}$인 olivine, pyroxene 그리고 ilmenite와 $Fe^{3+}$인 hematite, magnetite 등을 포함하고 있으며 주성분으로 볼 수 있는 hematite의 총 면적비는 평균 51.77 wt% 이었고 스코리아 내에 존재하는 철의 주 원자가 상태는 대부분 $Fe^{3+}$임을 알 수 있었다.

• 한국광물학회지
• /
• 제24권3호
• /
• pp.195-204
• /
• 2011

용출구조를 보이는 티탄철석-적철석 광석시료에 대한 구조분석을 리트벨트법을 이용하여 시행하였다. 구조유사체인 두 광물의 분석결과, 기본구조인 팔면체의 형태는 티탄철석의 Ti를 중심으로 한 팔면체(M2)가 정팔면체에 가장 가까운 형태를 보여주며, 다음은 티탄철석의 Fe를 중심으로 한 팔면체(M1)이다. 적철석 팔면체의 경우 M1과 M2 중간정도이다. 고압실험은 두 광물의 회절선이 중첩되는 5.8 GPa까지 시행하였다. 이 압력구간에서 티탄철석은 정상적인 압축성을 보이나, 적철석의 압축은 미미하게 발생하는 비정상적인 거동을 보인다. 이러한 이상거동은 두 광물의 압축성 차이에 의한 차등대응에 의한 것으로 판단된다.

• Journal of Magnetics
• /
• 제7권2호
• /
• pp.25-28
• /
• 2002

Slowly cooled $Cu_xFe_{3-x}O_4$ ($\chi$=0.1, 0.2) have been investigated over a temperature range from 82 to 700 K using the M$\ddot{o}$ssbauer technique. X-ray diffraction shows that these have a single-phase cubic spinel structure of lattice parameters $\alpha$=8.396 and 8.398${\AA}$, respectively. Since Cu ions prefer B (octahedral) sites to A (tetrahedral) sites, the ionic distribution is $(Fe)_A[Fe_{2-x}Cu_x]_BO_4$. M$\ddot{o}$ssbauer spectra consisted of two sets of 6-line pattern from. A site in ferric state and B site in ferrous-ferric state. Intensity ratio of B to A subspectra is 1.0 at 82 K and increases to 2.0 at 700 K with increasing temperature. After annealing the samples under vacuum at $450^circ{C}$ for a half hour, x-ray diffraction patterns have the peaks of magnetite- and hematite-phase. Lattice constants of magnetite-phase are 8.395 and 8.392 ${\AA}$ smaller than 8.396 and 8.398 ${\AA}$ before annealing, respectively. M$\ddot{o}$ssbauer spectra reveal the conventional magnetite pattern with the additional hematite pattern. Intensity ratios of B to A subspectra fur magnetite-phase become 1.9-2.0 over all temperature ranges and Cu ions are distributed over A and B sites randomly. Ratios of hematite to total intensity in M$\ddot{o}$ssbauer spectra for $\chi$= 0.1 and $\chi$= 0.2 are 10 and 21%, respectively. These hematite ratios may be due to annealing under vacuum at $450^circ{C}$, which transforms $Cu^{2+}$ ionic states into $Cu^{1+}$. Verwey temperatures far $\chi$= 0.1 and $\chi$= 0.2 are $123\pm2$ K and $128\pm2$ K.

• 한국광물학회지
• /
• 제25권4호
• /
• pp.197-210
• /
• 2012

철 (산수)산화물들 중 지표환경에서 가장 안정된 형태로 알려진 적철석의 비소에 대한 흡착제로서의 다양한 특성을 조사하고 비소와의 흡착특성을 규명하였다. 본 연구에서 합성된 적철석은 $31.8g\;m^2/g$의 비표면적을 가졌으며, 전위차 적정법(potentiometric titration)에 의해 측정된 영전하점(point of zero salt effect, PZSE)은 8.5로 비소에 대한 높은 흡착능은 이러한 적철석의 특성들에 기인한 것으로 판단된다. 동일한 수용상 농도와 pH 2.0~12 범위에서 3가 비소와 5가 비소의 적철석에 대한 흡착량을 비교한 결과 3가 비소가 5가 비소보다 큰 흡착량을 보였다. 그리고 pH에 따른 흡착경향은 3가 비소의 경우에는 pH 9.2까지 지속적으로 흡착량이 증가하다가 그 이상의 pH에서는 흡착량이 급격하게 감소한 반면, 5가 비소는 pH 2.0에서 가장 높은 흡착량을 나타내다가 pH가 증가하면서 지속적으로 감소하는 것으로 조사되었다. 이러한 pH에 따른 흡착특성은 pH에 따라서 적철석의 표면전하 특성과 비소 화학종의 존재형태가 변화하기 때문인 것으로 판단된다. 흡착 반응속도에 대한 실험 결과에 의하면, 두 비소 종 모두 20시간 이내에 평형 흡착에 도달하는 것으로 나타났다. 그리고 비소의 화학종과 관계없이 적철석과의 흡착반응속도를 가장 잘 모사하는 반응속도 모델로는 유사이차(Pseudo-second-order) 모델로 평가되었으며, 5가 비소가 3가 비소보다 반응속도상수가 크게 나타났다.

• 자원환경지질
• /
• 제12권1호
• /
• pp.13-15
• /
• 1979

Iron ore waste discarded around Choong-ju iron district, Choongchong-Bukdo is as low as 25 per cent of iron, mainly consisting of hematite and magnetite. In this mineral dressing test procedure 93 per cent of magnetite was separated and concentrated into the magnetite concentrate as high as 62 per cent. The remaining sample, mostly, hematite averages about 19.8 per cent of iron which can be concentrated with very good results with the optimum flotation conditioning-pH 3.0 and 3 cc per litre of aero-promoter #845 (0.5% sol.) and 1.5cc per litre of hydro-fluoric acid (40% sol.) and four times of cleaning flotation. Hematite concentrate averages 64.2 per cent of iron. The overall iron concentrate averages 63 per cent of iron with recovery 86 per cent of iron contained.

• 한국광물학회지
• /
• 제2권1호
• /
• pp.11-17
• /
• 1989

The kaolin deposits in Hadong-Sancheong area, have been formed by supergene weathering of anorthositic rocks including anorthosite, leucogabbro, and gabbro. Kaolin consists chiefly of halloysite(10$\AA$) and kaolinite with other minerals such as illite, vermiculite, plagioclase, hornblende, quartz amorphous materials(allophane and siica), goethite, and hematite. Goethite and hematite are the major coloring agents of the reddish brown and other colored kaolins. Other common accessory minerals are magnetite, ilmentite, anatase, gibbsite, I/S, C/V, chlorite, lithiophorite, and birnessite. Paragonite, dravite, laumontite, clinozoisite, muscovite, scolecite, stellerite are locally found. Al substitution of Fe in goethite and hematite decreases from the surface zone toward the deeper zone. The kaolin deposits show three horizontal zoning; the upper reddish brown, middle pink, and lower white zones. All the zones are characterized by somewhat different mineralogy. The factors for the formation of kaolin deposits in Hadong-Sancheong area are 1) the presence of anorthositic rocks, 2) the low flat or gentle topography, 3) the favorable climate, and 4) the long-continued preservation of kaolins with-out erosion.

• 한국분말야금학회:학술대회논문집
• /
• 한국분말야금학회 2006년도 Extended Abstracts of 2006 POWDER METALLURGY World Congress Part 1
• /
• pp.472-473
• /
• 2006

Maghemite and hematite nanospheres were synthesized by using the Sol-gel technique. The structural properties of these nanosphere powders were characterized by X-ray diffraction (XRD), transmission electron microscopy (TEM), field emission scanning electron microscopy (FESEM), and pore size distribution. Hematite phase shows crystalline structures. The mean particle size that resulted from BET and XRD analyses were 4.9 nm and 2 nm. It can be seen from transmission electron microscopy that the size of the particles are very small which is in good agreement with the FESEM and the X-ray diffraction. The BET and pore size method were employed for specific surface area determination.

• 보존과학연구
• /
• 통권16호
• /
• pp.129-138
• /
• 1995

For the study of the pigments on lacquer with wooden for comparing a characteristics and chemical structures have been selected samples from tombs at Tanwol-dong, Ch′ungch′ong-do, Hwang-namtaech′ong, Anapchi Lake in Kyongju-shi and Miruksa Site. Analysis showed that red pigments on the lacquer with wooden from Anapchi Lake and Tomb at Tanwol-dong was found to Cinnabar, and those sample sexcavated from Hwang-namtaech′ong have been analyzed to calcite, maghematite and kornelite. In general, red pigments have two components like cinnabar and hematite. Hematite was found that red lacquer at Hwang-namtaech′ong was to beidentified Maghematite caused by their environment air pollution. Cinnabar was handled more valuable than hematite for unchanging characteristics for their colour under same condition since old times.