• 상하수도학회지
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• 제21권1호
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• pp.37-46
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• 2007

A feasibility test was conducted to evaluate the addition of turbidity substance in a coagulation process to remove natural organic matters (NOM), the precursor of disinfection by-products (DBPs). The experimental water sources were synthetic water containing 5 mg/L of humic acid and 50 mg/L of NaHCO3 and drinking water resource of Ulsan city (S Dam water, D Dam water and Nak-Dong raw water). The examined turbidity substances were kaolin, acid clay, and modified clay (0.38 meq $NH_4{^+}-N/g$ clay). In Jar tests at different concentrations of the turbidity substances (5, 10, 15, 20, 30 mg/L) using the synthetic water, the turbidity substances improved the removal of turbidity, UV-254 absorbance and dissolved organic carbon (DOC) by 23.8-38.1%, 17.0-24.5% and 2.5-44.5%, respectively. The modified clay showed higher removal efficiencies than other substances. In Jar tests using the drinking water, 10 and 20 mg/L of modified clay enhanced the removal efficiencies of turbidity, UV-254 absorbance, DOC, trihalomethane formation potential (THMFP), and haloacetic acid formation potential (HAAFP) by 3.0~4.3%, 19.1~29.0%, 12~34.9%, 4.9~36.7%, and 1.6~30.2%, respectively.

• 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.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2010년도 춘계 학술발표회
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• pp.971-980
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• 2010

Evaluation of permeability and coefficient of consolidation of clayey sand is critical to analyze ground stability or environmental problems such as diffusion and dispersion in groundwater flow. Permeability tests using a flexible wall permeameter were performed to derive the coefficient of consolidation and permeability of reconstituted soil samples with various mixing ratios of kaolin clays and two different types of sands, Jumunjin sand and Ottawa sand. The test results indicated that coefficient of consolidation and permeability in log scale have linear relationships with clay contents in low clay mixing ratio. It is also recognized that coefficient of consolidation and permeability of sand and clay mixture are also dependent on the soil structure.

• 보존과학회지
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• 제38권4호
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• pp.327-333
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• 2022

Sri Lanka has four types of mural painting styles; Classic, Late Classic, Kandyan, and Southern styles, but there is little research on scientific analysis for mural paintings. In this study, we analyze white, yellow, and red clay pigments which were collected from ancient producing sites. Analyzing pigment samples shows that samples are containing aluminum oxide(Al₂O₃) and silicon dioxide(SiO₂) which are connected to the soil. And a degree of iron oxidation determines yellow or red colors. To understand the characteristics of clay pigment samples, we go over previous pigment analyses of mural paintings in Sri Lanka. Kaolin is identified after the 17^th century, yellow and red ochre are applied in early periods, Classic and Late Classic styles. The change in raw materials of pigments occurred in the 17^th century.

• 한국광물학회지
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• 제30권1호
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• pp.11-19
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• 2017

전남 나주시 장동리 지역의 화강암 풍화대를 피복하는 적갈색 점토-실트 퇴적물 단면(~2 m)에 대하여 광물학적 및 지화학적 특성 분석을 실시하였다. 퇴적물은 주로 석영(50%)과 점토광물(45%)로 구성되어 있으며, 소량의 K-장석, 침철석, 적철석, 깁사이트로 구성되어 있다. 점토광물은 일라이트(일라이트, 일라이트-스멕타이트 혼합층), 질석(질석, 수산화-Al 질석), 고령석(캐올리나이트, 할로이사이트) 계열의 점토광물로 구성되어 있다. 광물 및 화학조성의 수직 함량변화는 미미하며, 사장석과 녹니석이 전반적으로 결핍되어 있으나 최상부에 소량 함유되어 있다. 점토광물의 주성분이 일라이트 계열이므로 퇴적물의 기원물질은 주변 고령토질 화강암 풍화물이 아니라, 먼 기원지에서 유래한 풍성퇴적물로 판단된다. 현생 황사의 광물조성과 비교하면, 퇴적 후의 심한 화학적 풍화작용으로 사장석과 K-장석이 거의 없어지고, 석영과 점토광물로 구성된 광물학적 특성을 갖게 되었다. 풍화과정에서 사장석과 녹니석은 각각 고령토 광물과 질석으로 변질되었으며, 함철 유색광물의 풍화과정에서 침철석과 적철석이 침전되어 퇴적물이 적갈색을 띠게 되었다. 이 지역의 적갈색 점토-실트는 한반도 타지역 풍성퇴적물과 광물학적 및 지화학적 특성을 공유하므로 풍성퇴적물로 추정되지만, 이에 대해서는 퇴적물 연대측정이나 동위원소 분석 등의 추가 검증이 필요하다.

• 한국세라믹학회지
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• 제52권3호
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• pp.180-185
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• 2015

Low-cost ceramic membrane supports with pore sizes in the range of $0.52-0.62{\mu}m$ were successfully prepared by uniaxial dry compaction method using inexpensive raw materials including kaolin, bentonite, talc, sodium borate, and alkaline-earth oxides in carbonate forms (e.g., $MgCO_3$, $CaCO_3$, and $SrCO_3$). The prepared green supports were sintered at $1000^{\circ}C$ for 8 hr in air. The effect of alkaline-earth oxide additives on the flexural strength of clay-based membrane supports was investigated. The porosity of the clay-based membrane supports was found to be in the range of 33-34%. The flexural strength of the clay-based membrane supports with 1% alkaline-earth carbonates was found to be in the range of 42.8-52.7 MPa. The addition of alkaline-earth carbonates to clay-based membrane supports resulted in large increases (47-80%) in the flexural strength of the membrane supports, compared to that of membrane supports without alkaline-earth carbonates. The typical flexural strength of the clay-based membrane support with 1% $SrCO_3$ was 52.7 MPa at 33.8% porosity.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2001년도 추계학술발표회
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• pp.191-194
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• 2001

The electrokinetic apparatus for remediation of the soil contaminated with Cs$^{+}$was designed. After kaolin clay was compulsorily contaminated by Cs$^{+}$ solution, the remediation characteristics by electrokinetic method were analyzed. After remediation experiment, the pH of the cathode side of the soil column was increased to 12.7 due to the generation of OH in cathode reservoir, but no hydroxide cesium form in the cathode side. Effluent rate from the cathode almost was constant and cesium concentration of effluent decreased with time passage. The 49% of a total of Cs$^{+}$ in the column was decontaminated for 0.4 day, the 72% of a total of Cs$^{+}$ in the column was decontaminated for 0.8 day, the 83% of a total of Cs$^{+}$ in the column was decontaminated for 1.2 days, the 89% of a total of Cs$^{+}$ in the column was decontaminated for 1.6 days, and the 93% of a total of Cs$^{+}$ in the column was decontaminated for 2.1 day Meanwhile, the predicted values of residual concentration by the developed model were quite similar to those obtained from experiments.m experiments.

• 대한전기학회:학술대회논문집
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• 대한전기학회 2004년도 하계학술대회 논문집 A
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• pp.527-529
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• 2004

This paper researched leakage current characteristics of EHW insulators(36,000lbs) to artificially contaminated clay and kaolin through construction of long-periods testing facility. Insulators were contaminated and classified into the ESDD level(B, C and D) under IEC Pub. 60507 standards method. As a result of tests, leakage current of the heavily contaminated D level to clay was approximately 2,260 $[\muA]$, which is contaminated to kaolin was approximately 3,200 $[\muA]$, during initial rainfall. However after raining, leakage current of naturally washed contamination insulators was lower at approximately 300 $[\muA]$. As regular temperature $20^{\circ}C$, leakage current increased greatly in case humidity density was over $72\%$. But, leakage current was not influenced by temperature variation in case of regular $\%$ humidity.

• 약학회지
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• 제29권4호
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• pp.176-182
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• 1985

As a part of the studies on adsorptive properties of Korean halloysite clays, Hadong white clays of premium grade were examined for geometric pore structured by mercury porosimetry and for specific surface areas by nitrogen adsorption according to the BET procedure. Three size fractions of the native clay sample were derived from passage BS #100, #200 and #325 meshes, respectively. Several parameters lhus observed in relation to the pore structures are shown below: 1. The size fraction of BS #100, #200 and #325 show internal pore volumes of 25.3, 30.2 and $35.0m^2g^{-1}$, respectively. 2. In the distribution curves of the cumulative pore volume against pore diameter, it has been shown that the larticle sizes, the steeper the distribution over the larger ranges of pore diameters. The converse is true the smaller particles. 3. Internal pore areas increase with decrease in pore sizes. It follows that the pores having diameters of $\leq$0.1$\mu\textrm{m}$ are responsible for more than 90% of the total pore area. 4. The behaviour of nitrogen adsorption can be best described by BET type IV isotherm. Further, the hysteresis loops of the adsorptiondesorption curves become narrower with decresing particle sizes. 5. The specific surface areas observed for the fractions of BS #100, BS #200 and BS #325 are 34.6, 35.4 and 43.2m $^2g^{-1}$, respectively. and the calcined clay of BS #325 has a specific surface area near $30.4m^2g^{-1}$.

• 한국토양비료학회지
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• 제6권3호
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• pp.141-152
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• 1973

화강암(花崗岩), 화강섬록암(花崗閃綠岩), 섬록암(閃綠岩), Arkose 질사암(質砂岩), 및 Tertiary 혈암(頁岩)등에 유래(由來)된 사과과수원(果樹園) 11개처(個處)의 하층토(下層土)에 대(對)해서 광물(鑛物)의 풍화과정(風化過程)과 토양생성작용(土壤生成作用) 및 광물조성(鑛物組成)과의 관계(關係)를 밝히기 위(爲)하여 일(一), 이차광물(二次鑛物)에 대(對)한 광물학적(鑛物學的) 연구(硏究)를 시도(試圖)한 결과(結果)는 다음과 같다. 1. 일차광물(一次鑛物)로서 Quartz, Changed-feldspar, Plagioclase, Alkali-feldspar 등은 거의 모든 시료(試料)에 존재(存在)하였고, 또 시료(試料)에 따라 Hornblende, Biotite, Muscovite 및 Plant opal를 가진 것도 있었으며, 그 밖에 양(量)은 적으나마 Pyroxene group, Tourmaline, Epidote, Cyanite, Magnetite, Volcanic glass 및 Zircon 등도 찾아 볼 수 있었다. 토양(土壤)의 광물학적조성(鑛物學的組成)은 모재(母材)의 특성(特性)을 어느정도(程度) 반영(反映)하고 있어서, 주(主)로 Granite, Granodiorite, Diorite, Arkose 또는 그들의 풍화생성물(風化生成物)이 서로 혼입(混入)된 것에 유래(由來)된 것으로 추정(推定)할 수 있었다. 2. 점토광물조성(粘土鑛物組成)은 팽창형(膨脹型) 또는 비팽창형(非膨脹型) ${\AA}14$광물(鑛物), Illite 및 Kaolin 광물(鑛物)이 주성분(主成分)으로 되고, 시료(試料)에 따라서는 Chlorite, Christobalite, Gibbsite와 일차광물(一次鑛物)인 Quartz 및 Feldspar를 가지고 있었으나 양적(量的)으로는 모재(母材)에 따라 차(差)가 있었다. 3. 비팽창형(非膨脹型) $14{\AA}$광물(鑛物)로는 2, 8면체(面體) Vermiculite가 주(主)이고, 그 층격자간(層格子間)에 Gibbsite 모양의 수산화(水酸化) Aluminium 층(層)을 끼워 있는 것으로 추정(推定)된다. 4. Arkose 또는 Tertiary 혈암계암석(頁岩系岩石) 풍화생성물(風化生成物)에 유래(由來)된 것은 Montmorillonite가 주성분(主成分)이 였다. 그러나 Arkose만으로 된 것은 Kaolin 광물(鑛物)과 Vermiculite가 주(主)이고, 또 산성암풍화생성물(酸性岩風化生成物)이 주(主)로 된 곳은 Kaolin 광물(鑛物)을 주성분(主成分)으로 하는 것과, Kaolin 광물(鑛物) 및 Vermiculite를 주성분(主成分)으로 하는 두 Group로 크게 나눌 수 있었다.