• Bulletin of the Korean Chemical Society
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• 제19권3호
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• pp.324-327
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• 1998

The mechanisms of Cu2+ adsorption onto goethite, hematite and kaolinite are different. Goethite and hematite showed a similar adsorption behavior (ionic-strength independent), but kaolinite gave somewhat different result (ionic-strength dependent). These experimenal results were successfully simulated using a surface complexation model, TLM, which defines the inner- or outer-sphere complex. The chemical nature of Cu2+ adsorption onto kaolinite was qualitatively identified by EPR spectroscopy.

• 한국재료학회:학술대회논문집
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• 한국재료학회 1992년도 춘계학술발표회
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• pp.36-37
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• 1992

• 한국원자력학회:학술대회논문집
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• 한국원자력학회 1998년도 추계학술발표회요약집
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• pp.280-280
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• 1998

• 한국결정성장학회지
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• 제24권1호
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• pp.21-26
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• 2014

일본에서 적색 라꾸용 원료로 사용중인 황토는 장기간 사용으로 매장량이 감소되어 대체 원료를 개발하고자 노력중에 있다. 본 연구에서는 현재 일본 라꾸요장에서 사용되는 일본 시가현 고우가시 시가라끼 황토를 분석하여 이와 동일한 색상의 화장토를 개발 하고자 하였다. 일본 시가라끼 황토에 함유된 Goethite와 Wustite의 양을 Raman에 의한 "상대 정량분석법"으로 분석한 결과 일본 시가라끼 황토 내에 함유된 산화철 9.4 %에는 Goethite가 5 %, Wustite가 4.4 %로 구성되어 있으며 이를 $900^{\circ}C$에 넣어 10분간 소성 시 적색을 나타내는 것은 Goethite가 Hematite로 전이되면서 Hematite에 Alumina와 Silica가 고용되기 때문이다. 일본 시가라끼 황토에 함유된 산화철의 양을 기초로 일본 적색 화장토와 같은 색상을 나타내는 것은 하동 White Kaolin 100 g에 Goethite를 5 g, Wustite를 9 g을 첨가한 것이었으며 UV측정결과 $L^*a^*b^*$값은 각각 56.83, 27.22, 23.28이었다.

• 한국전기전자재료학회논문지
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• 제31권5호
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• pp.300-306
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• 2018

The rod-shaped $Ni_{0.5}Zn_{0.5}Fe_2O_4$ particles were synthesized via a topotactic reaction, in which goethite (${\alpha}-FeOOH$) particles are the main constituents. The phases, microstructures and magnetic properties of these particles were studied using XRD, FE-SEM and VSM. The precursor solution consisted of $NiSO_4{\cdot}xH_2O$, $ZnSO_4{\cdot}xH_2O$, goethite and D.I. water werereacted at four different temperatures (50, 70, 90, $100^{\circ}C$) to generate four differently precipitated particles respectively. During the co-precipitation reaction, the pH of the solution was maintained at 8.0 using NaOH. The particles co-precipitated and calcined at a temperature of $700^{\circ}C$, exhibited a rod-shape similar to its original goethite, which means that the shape of Ni-Zn ferrite particles can be topotactically controlled by the goethite. The particles synthesized at 70 and $90^{\circ}C$ have a saturation magnetization of 29 and 35 emu/g respectively; representing better values than the ones synthesized at the 50 and $100^{\circ}C$, in which some second phases such as $Fe_2O_3$ were observed.

• Nuclear Engineering and Technology
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• 제31권2호
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• pp.182-191
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• 1999

The sorption of UO$_{2}$$^{2+}$ onto goethite and kaolinite under various experimental conditions was successfully interpreted using surface complexation modeling (SCM). The SCM approach used in this work is the triple-layer model (TLM) in which weakly bonded ions are modeled as outer-sphere (ion-pair) complexes and strongly bonded ions as inner-sphere (surface coordination) complexes. The change of ionic strength did not affect the U(VI) sorption onto goethite, thus the formation of inner-sphere surface complexes, (FeO)$_2$UO$_2$ and (FeO)$_2$(UO$_2$)$_3$OH$_{5}$ was assumed to simulate the effects of ionic strength and goethite concentration. On the other hand, the U(VI) sorption onto kaolinite showed ionic strength dependence, thus the formation of AlO-UO$_{2}$$^{2+}$(outer-sphere complex) and SiO(UO$_2$)$_3$OH$_{5}$ (inner-sphere complex) was assumed to simulate the experimental data. In the presence of carbonates, the sorption of U(VI) onto kaolinite decreased in the weakly alkaline pH range. This was well simulated assuming the formation of a outer-sphere surface complex, A1OH$^{2+}$- (UO$_2$)$_2$CO$_3$OH$_3$. Since SCM approach uses thermodynamic data such as surface complexation constants, it is more predictive than empirical modeling approach in which conditional values such as partition coefficient are used. used.

• 한국세라믹학회지
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• 제56권2호
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• pp.146-152
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• 2019

In order to study the transport behavior of tripolyphosphate (TPP) in aqueous solutions, the adsorption process of TPP on synthetic goethite, which exists stably in supergene environment, has been systematically studied. The adsorption properties under different conditions (pH, electrolyte presence, and temperature) were investigated. The adsorption of TPP in the presence of humic acid (HA)/fulvic acid (FA) has also been discussed in this paper. The results indicated that the adsorption capacity quickly increased within the first hour and equilibrium was reached within 24 h. The adsorption capacity decreased from 1.98 to 0.27 mg·g^-1 upon increasing the pH from 8.5 to 11.0, whereas the adsorption of TPP on goethite hardly changed with increasing electrolyte concentration. The results of analysis of the kinetic and isothermal models showed that the adsorption was more in accord with the pseudo second-order equation and Freundlich model. The adsorption capacity decreased obviously regardless of the order of addition of TPP, HA, and goethite. Subsequent addition of FA led to a large increase in the adsorption capacity, which might be attributed to the adsorption ability of FA. According to the predictions of the kinetic and isothermal models and the spectroscopic evidence (X-ray diffraction (XRD), Fourier Transform infrared spectroscopy (FT-IR), and scanning electron microscope (SEM)), the adsorption mechanism may be mainly based on surface complexation and physical adsorption.

• 한국광물학회지
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• 제24권2호
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• pp.63-71
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• 2011

슈베르트마나이트로부터 침철석으로의 전이 시 일어나는 광물학적 변화 및 이와 연관된 중금속의 거동을 알아보기 위하여 달성광산의 광산배수 정화시설 소택지에 침전된 침전물을 대상으로 광물학적 연구와 지구화학적 연구를 수행하였다. XRD 연구결과 초기에 광산배수로부터 침전된 슈베르트마나이트는 대부분 침철석으로 전이되어 상부 일부에서만 슈베르트마나이트가 관찰되었다. SEM으로 광물 전이에 따른 외부형태 변화를 관찰한 결과 눈에 띄는 변화가 없는 것으로 보아 광물전이는 용해-챔전의 과정보다는 고체상에서의 전이가 있었음을 알 수 있었다. 슈베르트마나이트와 침철석에 흡착 또는 공침된 중금속들 중 Pb와 Cu의 경우 광산배수의 중금속 농도에 비교하여 상대적으로 높은 농도를 보였으며 나머지 중금속들은 상대적인 양에 있어서 비슷한 값을 보였다. 상부 슈베르트마나이트에서 하부의 침철석으로 전이가 일어나면서 광물 내 함유된 중금속의 함량은 일부 시료를 제외하고 전체적으로 눈에 띄는 변화를 보이지 않았으며 이는 슈베르트마나이트에서 침철석으로 전이되는 과정에서 고체 상태에서 전이가 일어나면서 추가적인 중금속의 용출이나 흡착이 없었음을 지시한다.

• 한국세라믹학회지
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• 제28권12호
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• pp.996-1004
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• 1991

In this study, we tried to synthesis iron hydroxide suitable for longitudinal magnetic recording media from waste acid, which is a by-product of an iron works factory. Effects of initial pH of reactants, reaction temperature, reaction time for the synthesis of acicular iron hydroxide were studied in relation to particle properties of iron hydroxide and magnetic properties of maghemite powders. As the pH in reactant solution increased, $\beta$-FeOOH(pH=4.5), mixture of $\beta$-FeOOH and $\alpha$-FeOOH(4.5$\alpha$-FeOOH and Fe3O4(6.4$\alpha$-FeOOH (pH>13) was found to from in order. Especially, $\alpha$-FeOOH formed above pH 13 was single phase with superior acicularity. The temperature range over which the single-phase goethite can be formed increased as the initial pH of reactants increased (pH 13:10~5$0^{\circ}C$, pH 13.2:10~7$0^{\circ}C$, pH 13.5:0~8$0^{\circ}C$). The goethite formed between 40~6$0^{\circ}C$ has superior characteristics because the acicularity increased with increasing temperature but at high temperature (>6$0^{\circ}C$) Fe3O4 (pH=13) was found to start to form. Generally, single phase of goethite was found to form after one hour when an optimized condition. The particle size of goethite did not change as the reaction time increased over one hour. Accordingly, the magnetic properties of ${\gamma}$-Fe2O3 produced from goethite were not altered.

• 대한화학회지
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• 제19권2호
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• pp.142-146
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• 1975

황산제일철을 원료로 해서 함수산화철 안료를 제조하기 위한 실험이다. 황산제일철을 암모니아로 중화해서 Mohr's salt(ferrous ammonium sulfate)을 만들고 Mohr's salt의 농도를 Fe(II) 이온농도, 14${\sim}$72g/l, 수소이온농도를 pH3 또는 6으로 조절한뒤, 반응온도는 $90{\sim}100^{\circ}C$로 일정하게 유지하고 반응시간 2시간, 3기압으로 공기 가압한 결과는 다음과 같다. Mohr's salt의 농도가 진하고, 중성으로 갈수록 함수산화철의 수득율이 증가되며, Mohr's salt 농도가 Fe(II) 이온농도, 42.81g/l 일때, 91.5% 이상의 수득율을 얻었다. 이렇게하여 생성된 함수산화철의 결정형은 $\alpha$-goethite형이며, 색상도 천연 ${\alpha}$-goethite와 유사하였다. 이것을 $500^{\circ}C$로 하소(calcination)하니 미려한 적갈색을 띤 ${\alpha}-Fe_2O_3$가 생성되었다.