• 한국환경보건학회지
• /
• 제22권2호
• /
• pp.25-31
• /
• 1996

The species of four heavy metals (Cr, Cu, Ni and Pb) associated with sediments (viz exchangeable, carbonates, reducible, organic and residual fractions) were determined with respect to the particle sizes and depths at four locations of the lower Kumho river. In the exchangeable fraction, 3.7~19.52% of Ni and 2.8~14.81% of Pb were found, and in the carbonates fraction 2.12~19.43% of Ni and 1.39~15.42% of Pb were found. The reducible fraction retained about 8.66~44.93% of Cr, 0.41~9.79% of Cu, 17.38~35.74% of Ni and 9.5~44.89% of Pb. In the organic fraction about 0~21.06% of Cr, 2.95~35.74% of Cu, 0~14.66% of Ni and 0~10.65% of Pb were found. The residual fraction retained about 52.6~83.53% of Cr, 63.86~86.39% of Cu, 39.66~66.16% of Ni and 39.97~71.75% of Pb. The order of release or mobility of heavy metals was Ni > Pb > Cr > Cu. Mobile fraction of heavy metals by particle sizes (1.0~0.5 mm and 0.5~0.25 mm) was found to be higher in particle sizes 1.0~0.5 mm than that of 0.5~0.25 mm. The release or mobility of heavy metals by depths (0~5 cm, 5~10 cm and 10~15 cm) was found to be higher in the upper sediments than in the lower sediments, except Cu.

• 한국지하수토양환경학회:학술대회논문집
• /
• 한국지하수토양환경학회 2000년도 창립총회 및 춘계학술발표회
• /
• pp.46-51
• /
• 2000

Environmental quality regulations are used to establish the maximum permissible concentrations of heavy metals before a site can be deemed to be polluted or contaminated. This paper compares the results obtained by 0.IN HCl extraction and acid extraction method(HNO$_3$+HClO$_4$.HCl). The leaching efficiency of 0.1N HCl extraction is directly proportional to the final pH of leachate, due to the different solubilities of the heavy metals at different pH values, The severe differences between 0.1N HCl-extractable and total metal contents result mainly from the buffering effect of carbonates, present in sediment. samples. Application of sequential extraction experiments to some sediments collected from gully pot in Seoul illustrates a much stronger scavenging effect by Fe and Mn-hydroxides, carbonates and organic phases. As deduced from both sequential extraction and leaching experiments, the relative mobility of heavy metals is found to be: Mn>Zn>>Co>Cd>>Cu>Pb>Cr>Fe, in spite of large differences in heavy metal content and localization. Changes in the physicochemical environments (such as acidification) caused by a traffic accident may result in the severe environmental pollution of heavy metals of surrounding area( surface water and rivers).

• 펄프종이기술
• /
• 제40권2호
• /
• pp.8-15
• /
• 2008

Wastewoods (logging residues) generated in Korea were used to make lignocellulosic fillers for papermaking. Lignocellulosic fillers could play great roles to increase retention efficiency and thus decrease turbidity of white water in papermaking process. In addition, lignocellulosic fillers could be used to improve physical properties of paper through their high affinity to cellulosic fibers, leading to the less use of chemical additives like retention aids. Wastewoods including Pinus densiflora and Quercus variabilis were chemically and mechanically treated for making fine particles passing through 100 mesh wire. The newly generated fillers showed larger particle size distribution than ground calcium carbonates but similar distribution to talc. In particular, pretreatment by hot water was more effective to generate smaller particle size than by alkali treatment. Lignocellulosic particles mixed with ground calcium carbonates under intense hybridizing condition greatly contributed to surface coverage of organic fillers in addition to filling to lumen and pits.

• 자원환경지질
• /
• 제32권1호
• /
• pp.53-62
• /
• 1999

The possibility of heavy metal pollution by contaminated roadside soils was studied under controlled conditions. The soil samples from roadside and those from a retention pond consisting of settling particles were characterized by the XRD analyses and the sequential extraction experiments. Characterization by sequential extraction, for roadside soil indicates elevate total concentrations of heavy metals. The leaching behavior of the samples under different pH and time conditions were also studied. Differences between both types of samples result mainly from the buffering effect of carbonates, present in roadside soils and lacking from settling particles. Acid leaching of the settling particles is equivalent to the sum of FI+FII+FIII, while the amounts leached from roadside soil are lower probably from kinetic reasons. The buffering effects of carbonates were found to greatly delay the onset of the leaching reactions and the extent of dissolution in most metals except for Ca and Mn. The study of leaching kinetics at pH of 6.5 and 5 showed that Cd and Zn reached the maximum possible concentration within 3 days, while Pb did not show any sign of dissolution at both ph values. The absolute amounts of dissolved Cd and Zn increased by 7 to 9 times by decreasing the pH from 6.5 to 5, indicating slightly acidified rain may result in significant metal dissolution. As deduced from both sequential extraction and leaching experiments, the relative mobility of heavy metals is found to be : Mn=Cd>Zn>>Pb>Fe, in spite of large differences in heavy metal contents and localizations.

• 한국세라믹학회지
• /
• 제18권3호
• /
• pp.171-181
• /
• 1981

Alkaline-earth porcelains have been prepared from mixture of kaolin, quartz, and synthetic calcines obtained by calcining a mixture of kaolin and more than two different kinds of alkaline-earth carbonates. They were magnesium, calcium and barium carbonates which are inexpensive and readily available. The vitrification behavior of the batch mixes was investigated in the firing range of 1240$^{\circ}$to 1380$^{\circ}$, in relation to the body compositions. It appeared that the density and the firing temperature depended largely on the content of alkaline-earth oxides in the body. These porcelains posses excellant dielectric properties, and are especially valuable as bases for deposited carbon resistors for which they were developed. An illustrative composition is 50% Dong Hwa kaolin, 22.4% Chang Shin quartz, 27.6% calcine. The composition of the calcine is 70% Dong Hwa kaolin, 10.7% BaCO3, 13.5% CaCO3, 5.8% MgCO3. The specific resistance of this body is $1.2{\times}10^{15}$ ohm-cm at 5$0^{\circ}C$, $2.5{\times}10^{14}$ ohm-cm 10$0^{\circ}C$, $2.5{\times}10^{13}$ ohm-cm at 15$0^{\circ}C$, $1.8{\times}10^{12}$ohm-cm at 20$0^{\circ}C$.

• Bulletin of the Korean Chemical Society
• /
• 제28권11호
• /
• pp.2025-2028
• /
• 2007

Homogeneous zinc tetrahalide complexes, highly active catalysts for the coupling reactions of alkylene oxide and CO2 produce alkylene carbonates, were heterogenized due to their tendency to decompose produced alkylene carbonates during the distillation process. Heterogenization of homogeneous zinc tetrahalide complexes was achieved by polymerizing 1-alkyl-3-vinylimidazolium zinc tetrahalides. These polymerized zinc tetrahalide catalysts displayed similar activities to their corresponding monomeric analogues for the coupling reactions of carbon dioxide with ethylene oxide (EO) or propylene oxide (PO) to produce ethylene carbonate (EC) or propylene carbonate (PC). TGA studies showed that the polymer-supported zinc tetrahalide catalysts are thermally stable up to 320 oC. The catalyst recycle test showed that the supported catalysts could be reused over six times. After removal of the polymer-supported catalyst through a simple filtration, EC was able to be isolated without decomposition.

• 한국광물학회지
• /
• 제20권4호
• /
• pp.255-260
• /
• 2007

중국 서부에 분포하는 황토대지의 뢰스(loess)는 아시아 내륙에서 발생하는 광물먼지의 퇴적물일 뿐만 아니라, 우리나라 봄철 황사의 기원물질이기도 하다. 간빙기의 뢰스는 퇴적 후에 고토양으로 풍화되는 과정에서 풍성 일차 탄산염 광물 입자들이 용해되어 이차 탄산염광물로 재침전된다. 뢰스 및 고토양의 광물학적 분석에 의하면 풍성 탄산염 입자는 대부분 실트 크기이나, 재침전된 이차 탄산염광물은 너비가 $30{\sim}50nm$ 정도로 일정하고 다양한 길이를 갖는 나노 크기의 방해석들이었다. 나노방해석은 황토대지에서 점토광물과 함께 실트질 뢰스와 고토양의 세립 기질을 구성하는 주요 자생 광물로서, 우리나라에서 채집된 황사 입자에서 확인된 나노 방해석들의 기원물질로 해석된다.

• Bulletin of the Korean Chemical Society
• /
• 제20권12호
• /
• pp.1413-1417
• /
• 1999

Chemical poisoning of Ni/MgO catalyst was induced by hot alkali carbonate vapor in molten carbonate fuel cell (MCFC), and the poisoned (or contaminated) catalyst was characterized by TPR/TPO, FTIR, and XRD analysis. Carbonate electrolytes such as K and Li were transferred to the catalyst during DIR-MCFC operation at 650 ℃. The deposition of alkali species on the catalyst consequently led to physical blocking on catalytic active sites and structural deformation by chemical poisoning. TPR/TPO analysis indicated that K species enhanced the reducibility of NiO thin film over Ni as co-catalyst, and Li species lessened the reducibility of metallic Ni by chemical reaction with MgO. FTIR analysis of the poisoned catalyst did not exhibit the characteristic ${\vector}_1$$(D_{3h})$ peaks (1055 $cm^{-1},\;1085\;cm{-1})$ for pure crystalline carbonates, instead a new peak (1120 $cm^{-1})$ was observed proportionally with deformed alkali carbonates. From XRD analysis, the oxidation of metallic Ni into $Ni_xMg_{1-x}O$ was confirmed by the peak shift of MgO with shrinking of Ni particles. Conclusively, hot alkali species induced both chemical poisoning and physical deposition on Ni/MgO catalyst in DIR-MCFC at 650 ℃.

• 분석과학
• /
• 제12권4호
• /
• pp.284-289
• /
• 1999

지하수 중에 용존된 무기탄소 화합물을 기체 방출 법을 이용하여 정량적으로 추출하였다. 기체 방출법은 직접 침전법에 비하여 소요시간이 적으며, 대기중의 이산화탄소 및 수중에 존재하는 황산이온의 영향도 무시할 수 있어 보다 효과적임을 알 수 있었다. 기체 방출법에 의한회수율 측정 결과 분당 4리터의 유량 율로 2시간 방출시켰을 때 99% 정도의 회수율을 나타내었다. 포집 시간에 따른 동위원소 분별효과를 측정하기 위하여 방출 초기 1시간과 이후 30분 간격으로 2회 포집 분석한 결과, 각각의 ${\delta}^{13}C$는 각각 -7.9‰, -3.0‰, +0.4‰로 측정되어 기체 방출법을 이용한 수중의 무기탄소 회수시 방출 초기에는 보다 가벼운 탄소의 방출이 우세하며, 보다 무거운 탄소의 방출은 후기에 이루어지는 것을 나타내었다. 그러나 이러한 동위원소 분별효과는 탄소화합물의 거의 완전한 회수에 의해 무시될 수 있었다.

• 광물과 암석
• /
• 제35권3호
• /
• pp.183-197
• /
• 2022

한반도의 판 내부 기원 신생대 후기 현무암류(백두산, 전곡, 백령도, 평택, 아산, 간성, 울릉도, 독도, 제주도 등)에 대해 그 동안에 보고된 Sr-Nd-Pb-Mg-Zn 동위원소를 포함한 지구화학 자료를 종합정리하고, 그 근원 맨틀 속에 포함된 암상을 파악한 후 필요한 맨틀 단성분의 종류와 그 성인에 대해서 고찰하였다. Sr-Nd 동위원소 상관도에서 제주도는 EM2형 해양도 현무암의 영역에 도시되는 반면 다른 지역 현무암류는 EM1형 해양도 현무암의 영역에 도시된다. Pb-Pb 동위원소 상관도에서 제주도는 인도양 중앙해령 현무암과 EM2 단성분 간의 혼합 배열을 보이는 반면, 다른 지역 현무암류는 인도양 중앙해령 현무암과 EM1 단성분 간의 혼합 배열을 보인다. 한반도 현무암류는 석류석 러어조라이트와 함께 과거에 섭입하여 맨틀 전이대에 정치하고 있는 해양판 물질(에클로자이트/휘석암, 원양 퇴적물, 탄산염)이 혼합된 맨틀에서 유래되었다. EM1형 단성분의 역할을 하는 물질은 오래전(~2.0 Ga)에 섭입되어 중성 부력으로 맨틀 전이대에 정치되어 있는 (함)K-Hollandite 원양 퇴적물로 추정된다. EM2 단성분은 맨틀 속에 섭입된 후 빠른 시간 안에 재활성된 상대적으로 젊은(아마도 태평양판의) 원양 점토 퇴적물일 가능성이 높다. 에클로자이트와 탄산염은 EM 구성요소는 아니나 한반도 현무암의 근원 맨틀 속에 공통 인자로 포함되어 있다.