• 한국석유지질학회지
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• 제3권1호
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• pp.28-39
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• 1995

강원도 태백부근에 분포하는 조선누층군 풍촌층내에 나타나는 돌로마이트의 성인에 대해 연구하였다. 캠브리아기 풍촌층은 석회암, 돌로마이트질 석회암 그리고 돌로마이트로 이루어져 있으며, 이암(mudrock)과 판상석회질역암(Flat Pebble Conglmerate; FPC)이 협재되어 있다. 풍촌층의 돌로마이트는 조직적으로 4가지의 형태로 분류할 수 있는데, 이들은: 1) 괴상 돌로마이트내의 타형 돌로마이트, 2) 판상석회질역암내의 자형 돌로마이트, 3)우이드나 극피류를 치환하는 타형 돌로마이트, 4) 모틀구조를 보이는 돌로마이트이다. 특히 모틀구조를 보이는 돌로마이트는 다음과 같은 3가지로 세분되는데 이들은: a) 조립질의 타형 안장형 돌로마이트, b) 중립질의 자형 돌로마이트, c) 조립질의 자형 돌로마이트이다. 풍촌층 돌로마이트의 탄소동위원소성분은 $-2.8-1.4k\%_{\circ}$(PBD)이며, 이는 탄소동위원소가 퇴적당시 탄산염퇴적물의 값을 보존하고 있음을 나타낸다. 낮은 산소동위원소성분($\delta^{18}O -15.7-8.7\%_{\circ}, PBD$)은 풍촌층 돌로마이트가 매몰속성환경에서 형성되었음을 나타낸다. $^{87}Sr/^{86}Sr$의 초기비는 0.7101-0.7161 정도의 값을 보여주며, 이는 캠브리아기 해수의 성분보다 매우 높은_값이다. 이는 돌로마이트를 생성시킨 속성수가 대륙기원의 암석들과 반응하였던 것으로 생각된다. 돌로마이트의 Sr과 Na의 함량은 200ppm 이하의 낮은 값을 나타내는데, 이러한 낮은 미량원소 성분은 매몰속성환경에서 생성된 돌로마이트의 미량원소 성분과 잘 일치하며, 상대적으로 높은 Fe와 Mn의 함량은 풍촌층 돌로마이트가 환원환경 인 심부 매몰속성환경에서 형성되었음을 간접적으로 지시한다.

• 한국세라믹학회지
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• 제34권7호
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• pp.738-746
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• 1997

MgO clinker and two kinds of dolomite clinkers with different microstructures and CaO contents were used as starting materials, and the effects of Fe2O3 addition on the properties of MgO and dolomite were investigated in the range of 2 to 8 wt% of Fe2O3 content. Secondary phases contributed to densification of MgO-Fe2O3 and dolomite-Fe2O3 were magnesioferrite and dicalciumferrite, respectively. Sinterabilities of MgO-Fe2O3 and dolomite-Fe2O3 were directly proportional to the amount of secondary phases. Also, sinterability of dolomite itself was dependent on the microstructure of starting material including distribution of CaO and MgO as well as the addition amount of Fe2O3. The flexural strength of MgO-Fe2O3 content was almost constant. The hydration resistance of dolomite with large size of MgO and discontinuous distribution of CaO was higher than that of dolomite with small size of MgO and continuous distribution of CaO. Also, the minimum content of Fe2O3 to prevent they hydration of dolomite was about 4wt%. As increasing Fe2O3 content, the penetration resistance of MgO-Fe2O3 was improved by the increment of magnesioferrite. On the other hand, the penetration resistance of dolomite-Fe2O3 was decreased because of the increment of dicalciumferrite having low melting point.

• 상하수도학회지
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• 제26권3호
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• pp.443-451
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• 2012

Wastewater treatment plants need to reduce phosphorus in order to meet increasingly stringent regulations on phosphorus. This study evaluated the feasibility of dolomite as a coagulation aid to enhance phosphorus removal from secondary treated wastewater by chemical coagulation. Standard jar tests were conducted to evaluate the effect of dolomite addition on a coagulation process for phosphorus removal and to determine the optimum doses of coagulants and dolomite. Coagulants used with dolomite yielded a significant improvement in phosphorus removal and reduced total phosphorus concentrations below 0.02 mg/L in wastewater effluent. Dolomite has played an important role in enhancing phosphate adsorption and increasing pH, as a coagulation aid. The maximum removal efficiency of phosphorus in this study was yielded at 25 mg/l of dolomite and 20 mg Al/L of PAC dose. However, considering economic aspects, the optimum doses of dolomite and PAC were 10 mg/L and 15mg Al/L, respectively. Consequently, dolomite, a coagulation aid, can be used in coagulation processes to enhance the removal of phosphorus.

• 한국광물학회지
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• 제20권2호
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• pp.71-81
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• 2007

접촉변성과 열수변질 작용이 중첩되어 형성된 자성 광산의 대리암형 백운석은 대개 98 wt.% 이상의 매우 높은 백운석 함유도를 보이는 고품위백운석으로서 부수적으로 석영, 백운모, 활철석과 같은 불순물을 미량 함유한다. 열수변질 산물로 여겨지는 황철석으로 인해 0.4 wt.% 정도의 상당히 높은 철분 함유 수준을 보이는 것이 특징이다. 대체로 백색을 띠는 이 백운석은 $0.35{\sim}0.46mm$의 결정 입도를 보이며 반자형의 등립상 조직을 이룬다. 이 백운석의 분체 특성은 전형적인 고품위석회석인 풍촌층 석회석에 비해 분쇄 효율, 미분체의 형성 및 입도 분포 면에서는 다소 우수한 것으로 나타난다. 또한 철분 함량을 제외하고는 기타 충전재로서의 품질상의 주요 요소들 즉, 백색도, 흡유율 및 비표면적은 물론 신장비, 형상비, 구형도와 같은 형상 특성 면에서도 결코 뒤떨어지지 않는 분체 특성을 보인다. 이 같은 자성 백운석의 양호한 분체 특성은 원광에서의 기본적으로 높은 백운석 함유도와 비교적 높은 결정도에 기인한 것으로 여겨진다. 이 백운석은 비교적 높은 철분 함량과 황화광물의 혼재로 인해서 금속제련용을 제외한 소성용 용도로는 적합하지 않은 것으로 판단된다. 그렇지만 적절한 선광 공정이 적용된다면 현재 중탄용 석회석이 차지하고 있는 대부분의 충전재 응용 부문에서는 고품위석회석의 대체재로써 충분히 활용이 가능할 것으로 평가된다.

• 한국재료학회지
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• 제19권2호
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• pp.115-118
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• 2009

The use of dolomite refractories has increased during the past several years in the manufacturing of clean steel during the stainless steelmaking process. However, at the same time, the use of dolomite refractories has led to what is known as the skull formation. In the present work, to understand the skull formation, the wetting characteristics of dolomite substrates by liquid Fe-19wt%Cr-10wt%Ni alloys in various oxygen partial pressures were initially investigated at 1753K using the sessile drop technique. For comparison, the wetting characteristics of alumina substrates were investigated with the same technique. It was found that the wetting index, (1+$cos{\theta}$), of dolomite is approximately 40% higher compared to those of alumina. In addition, the oxygen partial pressure to generate the surface oxide, which may capture the liquid metal on the refractory surface, for dolomite is much lower than that for alumina. From this study, it was concluded that the use of dolomite is much more closely associated with the skull formation compared to the use of alumina due to the stronger wettability and the surface oxide formation at a lower oxygen partial pressure of dolomite.

• 한국태양에너지학회 논문집
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• 제22권1호
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• pp.9-21
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• 2002

To develope chemical heat pump using available energy sources, solar heat and other kinds of waste thermal energy, we have studied the heat transfer rate in cylindrical bed reactor packed with calcined Dolomite. Two dimensional (radial and circumferential) Partial differential equations, concerning heat and mass transfer in packed bed of calcined Dolomite, are solved numerically to describe the characteristics of the reaction of calcined Dolomite and heat transfer. The results obtained by numerical analysis about two dimensional profiles of temperature and conversion of reactant in the packed bed reactor and the amount of exothermic heat released from the reactor are follows. It was found that all of calcined Dolomite packed bed kept the reaction temperature of about 750K throughout the entire part of the bed, immediately after the steam was introduced exothermic reaction of hydration was proceeded from the packed bed inpu to output and from wall side to center. The rate of thermochemical reaction depends on the temperature and concentration and it is also governed by the boundary conditions and heat transfer rate in the particle packed bed.

• 한국세라믹학회지
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• 제36권1호
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• pp.30-35
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• 1999

155$0^{\circ}C$~1$650^{\circ}C$의 온도범위에서 stampwo의 원료로서 사용되는 돌로마이트 클링커의 Fe2O3의 함유유무에 따른 slag에 의한 침식거동을 연구하였다. Slag 성분중에서 CaO-SiO2계 저융점 화합물 보다는 Fe2O3가 선택적으로 돌로마이트 클링커의 입계로 깊숙히 침투되었다. 돌로마이트 클링커의 가동면에 존재하는 치밀한 magnesioferrite는 slag중의 Fe2O3 성분보다는 클링커중에 함유되어 있는 Fe2O3 성분에 의하여 우선적으로 생성되었다. 돌로마이트 클링커의 slag에 의한 손상은 돌로마이트 클링커의 입계에 존재하는 CaO가 slag중의 Fe2O3 성분과 반응하여 dicaciumferrite를 생성$\longrightarrow$dicalciumferrite가 slag 성분중의 CaO-SiO2계 화합물에 의하여 용출되는 단계로 진행되었다. Slag의 온도가 상승됨에 따라 Fe2O3가 함유되어 있지 않는 돌로마이트 클링커의 경우에는 돌로마이트 클링커의 가동면에 생성되는 magnesioferrite의 층은 미양하였다. 반면에, Fe2O3가 함유된 돌로마이트 클링커는 slag의 온도가 상승됨에 따라 magnesioferrite의 층이 두꺼울 뿐문아니라 magnesioferrite의 입성장도 수반되었다.

• 자원환경지질
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• 제4권3호
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• pp.113-119
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• 1971

The Daeheung Dolomite Mine, which is about 6km south of Danyang, Chungcheongbugdo, is coincided with almost central portion of the Danyang quardrangle scaled in 1 : 50,000. The purpose of this report is to prepare a information for the economic evaluation on the mine. Geology of the region is composed of worm-eaten limestone, crystalline limestone, crystalline dolomite rock, sandstone and shale from bottom, those are applicable to socalled Dumugol and Maggol formation of Ordovician, and batholithic biotite granite is intruded the west-side of the ditto sedimentary rocks. The dolomite bed, emplaced in bottom of the upper limestone formation, so-called Maggol formation, is about 270m in thickness, and dips $30^{\circ}{\sim}50^{\circ}$ northwest. The facies of the dolomite rock contained many brucite crystals is not only coarse-grained crystalline, but also micro crystalline in contact metasomatic parts. 25 samples were taken from the two series, A and B, in the nearly crossed direction to the strike of the dolomite bed as shown in the geological map. They were chemically analysed on the components of MgO, CaO, and $SiO_2$ as shown in Table 2. The estimate ore reserves total some 107,200,000 metric tons above the 320m level with the following average contents: MgO 21.80%, CaO 29.27% and $SiO_2$ 0.64%. It is caused by brucite minerals that MaO content in the dolomite rock is higher than pure dolomite (21.7%). The dolomite ore is possible in use for magnesian fertilizer, magnesian cement and refractory material, especially the microcrystalline dolomite ore is useful for a refractory material in furnaces of iron industries.

• 한국태양에너지학회 논문집
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• 제23권1호
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• pp.29-38
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• 2003

To develope chemical heat pump using available energy sources, solar heat and other kinds of waste thermal energy, we have studied the material and heat transfer rate in the cylindrical bed reactor packed with Calcined Dolomite. Our results from the studies are as follows ; 1 The time needed to complete dehydration reaction at the wall side of the cylindrical reactor(r/rL=0.5) was shorter than that of the center(r/rL=0.0) as much as 12%. 2. Two dimensional (radial and circumferential) partial differential equations, concerning heat and mass transfer rate in the packed bed of calcined Dolomite, are solved numerically to describe the characteristics of the reaction in the cylindrical reactor. The solution reads rate of reaction in the packed bed reactor depends on the temperature and concentration of reactants. These results read the supplied heat transfers from the wall side of the cylinder to the center, dehydration reaction begins at the inner side of the wall of the cylindrical reactor and the dehydration reaction proceeds from the wall side to center of cylinder.

• Advances in concrete construction
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• 제1권4호
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• pp.273-288
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• 2013

The main objective of this research was to evaluate the potentials of self-compacting concrete (SCC) mixes to develop bond strength. The investigated mixes incorporated relatively high contents of dolomite powder replacing Portland cement. Either silica fume or fly ash was used along with the dolomite powder in some mixes. Seven mixes were proportioned and cast without vibration in long beams with 10 mm and 16 mm steel dowels fixed vertically along the flowing path. The beams were then broken into discrete test specimens. A push-put configuration was adopted for conducting the bond test. The variation of the ultimate bond strength along the flowing path for the different mixes was evaluated. The steel-concrete bond adequacy was evaluated based on normalized bond strength. The results showed that the bond strength was reduced due to Portland cement replacement with dolomite powder. The addition of either silica fume or fly ash positively hindered further degradation as the dolomite powder content increased. However, all SCC mixes containing up to 30% dolomite powder still yielded bond strengths that were adequate for design purpose. The test results demonstrated inconsistent normalized bond strength in the case of the larger diameter compared to the smaller one.