• International Journal of Concrete Structures and Materials
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• 제7권2호
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• pp.119-125
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• 2013

Carbonation is a natural ageing process for cement. This study focuses on how the carbonation rate varies with selected hydration times and atmospheric conditions during the early stages of reacting dried cement paste. Diffuse reflection Fourier transform infrared spectroscopy is shown to be a suitable technique to monitor the formation of carbonates in cement. Combined with a previously developed freeze drying technique, carbonation can be studied at specific hydration stages. In ambient air both calcium hydroxide and calcium silicate hydrate (C-S-H) in cement are carbonated. Increased hydration time enhances the carbon dioxide uptake, which indicates that the calcium in the hydration products reacts more easily than the calcium in the clinker phase. In a humid $CO_2$ atmosphere, the carbonation process is so pronounced that it decomposes C-S-H into calcium carbonate and silica. In a moist $N_2$ atmosphere no carbonation occurs, but the sulfate chemistry of the cement seems to be affected due to the formation of ettringite.

• Bulletin of the Korean Chemical Society
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• 제27권8호
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• pp.1171-1174
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• 2006

Various off-the-shelf Lewis acids in conjunction with various onium salts are screened for coupling reaction of $CO_2$ with epoxides. Among the tested ones, $VCl_3/n-Bu_4NOAc$, $VCl_3/(n-Bu_4NCl$ or PPNCl), $FeCl_3/ n-Bu_4NOAc$, and $FeCl_3/ n-Bu_4NOAc$are proved to be highly active. Propylene oxide, epichlorohydrin, styrene oxide, and cyclohexene oxide can be converted over 90% yields to the corresponding cyclic carbonates without the use of organic solvents under mild conditions by 0.1-1.0 mol% catalyst charge.

• 펄프종이기술
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• 제36권2호
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• pp.47-53
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• 2004

In this experiment the effects of the packing structure of pigment on the surface characteristics (smoothness and gloss) of coated paper are studied. Four different kinds of inorganic pigments(clay), ground calcium carbonate(GCC), two of precipitated calcium carbonates(PCC), and two organic pigments(solid bead and hollow type) were used. The method of measuring the relative sediment volume(RSV) was used to analyze the packing structure of coating layer. The relative sediment volume was measured, using the pressure dewatering dry-cake method(PDDM) and centrifuge method. Also, the particle size distribution of coating pigment was determined. The results showed that small amount of organic pigment, added to inorganic pigment, improved smoothness and its effect was greater when GCC was used as inorganic pigment. The efficiency of organic pigment depended upon the inorganic pigment since the organic pigment is packed in the pores formed by the inorganic pigment.

• 자원환경지질
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• 제18권1호
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• pp.11-22
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• 1985

The Daehwa and Donsan tungsten-molybdenum deposits are composed of numerous fissure-filling veins developed in Precambrian gneiss and Cretaceous granite and quartz porphyry. K-Ar age of biotite in granite and that of muscovite in ore veins are $105{\pm}5\;Ma$ and 88.2~88.6 Ma respectively. Occurrence of ore deposits shows that relevant igneous rock is possibly quartz porphyry rather than above mentioned granite in temporal view point. Vein structure and mineralogy suggest that ore veins were formed by continuous vein filling, not by repeated mineralization. Three distinct depositional stages with decreasing age can be devided on the basis of mineral paragenesis and fluid inclusion studies: Stage I, deposition of oxides and silicates; stage II, deposition of base-metal sulfides and sulfosalts with carbonates; stage III, deposition of barren calcite and fluorite. Tungsten, molybdenum and tin mineralization occurred in stage I.

• 한국산학기술학회:학술대회논문집
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• 한국산학기술학회 2007년도 추계학술발표논문집
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• pp.347-349
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• 2007

지구 온난화를 일으키는 온실 가스 중의 하나인 이산화탄소($CO_2$)를 Epoxide와 Tetrabutylammonium bromide를 촉매로 하여 합성하여, 초임계 $CO_2$ 상태($Tc=31.06^{\circ}C$, Pc=7.38MPa)에서 반응하여 그에 따른 수율을 측정한 결과 초임계하에서는 현저한 수율의 증가를 확인하였다.

• 한국산학기술학회논문지
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• 제5권5호
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• pp.480-483
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• 2004

cyclic carbonate 가운데 하나인 4-ethyl-1,3-dioxolan-2-one가 poly(butylene carbonate)의 열분해에 의하여 합성되었다. poly(butylene carbonate)는 1,2-Epoxybutane라 이산화탄소로 합성되어졌다. 합성된 4-ethyl-1,3-dioxolan-2-one는 GC-Mass를 이용하여 분석 확인되었다. 이러한 새로운 합성법은 cyclic carbonate 계의 합성에 새로운 정보를 제안할 수 있다.

• Bulletin of the Korean Chemical Society
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• 제15권12호
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• pp.1118-1121
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• 1994

Reactions of alkaline metal carbonates with sulfur are investigated in detail. The evolution of CO and a trace of $SO_2$ were observed in the course of reaction with major component of polysulfides. Some evidences that the reaction proceeds with breaking of terminal sulfur-sulfur bond in the sulfur polymer, and forming CO, $SO_2$ and polysulfide are presented. Polysulfides have the role of keeping free sulfur and allow it to react with other chemicals to rather high temperatures.plexes, whereas the binuclear and mononuclear complexes of Mn$^{2+}$ and Co$^{2+}$

• 태양에너지
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• 제7권1호
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• pp.61-74
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• 1987

This review evaluates the state of art in the field of high-temperature energy storage materials and systems. The physical and chemical properties, corrosion data and practical applications of the phase change materials, especially the inorganic salts applicable to storage temperature in the range of $100-850^{\circ}C$ have been summarized. Fluoride salts have excellent thermal storage properties, but these are less attractive in terms of cost and corrosion problem of container materials. The nitrate and nitrite have attractive properties in the temperature range up to $600^{\circ}C$, at which the rate of decomposition becomes unacceptable. Carbonates euteutic salts can be considered as the most promising energy storage material on the basis of their low cost and excellent material compatibility for corrosion in the temperature range up to $850^{\circ}C$.

• Bulletin of the Korean Chemical Society
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• 제9권4호
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• pp.240-243
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• 1988

Degradation of the 90 K superconductor $YBa_2Cu_3O_{7-{\delta}}$ in water and humid atmosphere were studied and its decomposition products were identified as $BaCO_3$, CuO, $Y_2(CO_3)_3{\cdot}3H_2O$ and $O_2$. XRD analysis, iodometric titration and IR-spectroscopy of the degraded samples suggest that the $YBa_2Cu_3O_{7-{\delta}}$ decomposes in three steps such as the reduction of $Cu^{3+}$ to $Cu^{2+}$, followed by the hydroxylation of $Ba^{2+}$ and $Y^{3+}$ via hydration and finally the formation of carbonates through the uptake of ambient $CO_2$.

• 한국석유지질학회지
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• 제4권1_2호
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• pp.27-39
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• 1996

백악기 당시 미국 걸프만 퇴적분지는 대륙연변부의 색(sag)형 퇴적분지로서의 진화과정을 거치고 있었다. 두꺼운 백악기의 쇄설성과 탄산염 퇴적층은 상승 교란작용을 받은 암염층을 덮고 있다. 당시 걸프만 퇴적분지의 염분도는 넓게 발달하고 있는 초조간대의 경석고 퇴적층의 분포로 보아 현생의 페르시아만 환경과 유사했던 것으로 추정된다. 하부 백악기의 주요 저류암 (reservoir)으로는 쇄설성 퇴적암층인 카튼밸리(Cotton Valley), 허스톤(Hosston), 트래비스픽(Travis Peak)층과 탄산염 퇴적암층인 슬리고(Sligo), 트리니티(Trinity) - 파인아일랜드(Pine Island), 피어살(Pearsall), 글랜로스(Glen Rose), 에드워드(Edwards), 조오지타운(Georgetown)/부다(Buda) 층이 있다. 이 시기 저류암층에 탄화수소를 공급했던 근원암(source rock)으로는 경사방향 하부(down-dip)에 위치하고 있는 셰일과 이회암층이 꼽히고, 덮개암(seal)은 대개 경사방향 상부(up-dip)에 위치하고 있는 계일과 치밀한 석회암층, 그리고 증발암으로 보인다. 하부 백악기 동안 전 걸프만 퇴적분지는 천해환경하에 있었는데, 남서부 지역은 백악기 말까지 계속 이어졌던 천해 탄산염 환경이,북쪽과 서쪽지역에서는 육성기원의 세립질 퇴적물이 주로 집적되는 환경이었다. 상부 백악기동안에는 걸프만 퇴적분지는 주요한 해수면 상승기와 연관되어 비교적 수심이 깊었던 환경하에 있었으며 이 때 형성된 주요 저류암층으로는 우드바인(Woodbine)/투스칼루사(Tuscaloosa) 사암층, 테일러(Taylor) 나바로(Navarro) 사암층과 오스틴(Austin) 백악 및 탄산염암층이 있다. 이 저류암층에 탄화수소를 공급했던 근원암층으로는 경사방향 하부의 셰일층이, 그리고 덮개암층은 경사방향 상부의 계일층이 그 역할을 담당했던 것으로 해석된다. 뗘악기 하부와 상부 퇴적층의 주요 트랩(trap)으로는 완만한 기둥형(pillow)으로부터 복잡한 다이아피어(diapir) 형태의 암염층 관련 배사구조와 하단 단층블록위에 놓여 있으며 롤오버(rollover) 배사구조를 갖는 성장단층이 있다. 투수 장애(permeability barrier), 상부 경사방향으로 첨멸하는 사암체(up-dip pinch-out sand body깥 침식부정합면(unconformity truncation)도. 걸프만 석유부존에 중요한 역할을 한 트랩들이다. 백악기의 주요한 저류암층들은 범세계 해수면곡선의 하강시기와 잘 일치하고 있는데 이는 백악기동안 형성된 걸프만의 퇴적층서가 범세계 해수면곡선을 전반적으로 잘 반영하고 있음을 의미한다. 즉 퇴적작용을 주로 지배하는 세 즌요 변수인 지구조적인 분지의 침강운동,퇴적물의 공급,해수면 변동오그÷중에서 해수면 변동요소가 이 시기동안 가장 중요한 역할을 했음을 의미한다.