• 한국토양비료학회지
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• 제12권2호
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• pp.83-89
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• 1979

토양의 이화학적 특성(特性)이 불량(不良)한 사질답(砂質畓)을 개량(改良)코저 규회석(珪灰石), Dolomite, 객토(客土), 퇴비등(堆肥等) 개량제를 병용했을때 이들 개량제가 수도수량에 미치는 영향(影響)을 밝히고저 시험한 결과(結果)는 다음과 같다. 1. 토양중의 무기성분(無機成分) 변화는 개량제 시용(施用)에 의(依)하여 석회(石灰), 고토(苦土), 규산함량(珪酸含量)이 증가되었고 pH도 높게 유지(維持)되었다. 2. 식물체 무기성분(無機成分) 함량중(含量中) 석회(石灰) 규산함량(珪酸含量)은 객토(客土) Dolomite 규회석등(珪灰石等)의 개량제 시용(施用)에 의하여 증가되었다. 3. 규회석(珪灰石)과 Dolomite 시용(施用)에 의(依)하여 식물체중 인산함량(燐酸含量)은 관행(慣行)에 비(比)해 전생육기간(全生育期間)을 통(通)하여 감소(減少)되었고 가리함량(加里含量)도 유수형성기(幼穗形成期) 이후(以後)부터 감소(減少)되었다. 4. 가장 증수된 개량제처리는 객토(客土)+Dolomlte+N 증시처리로서 19% 증수되었으며, 규회석(珪灰石)+유기물처리에서도 10% 증수되었다. 이들 증수요인은 등숙율증가에 기인(基因)되었다.

• 자원환경지질
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• 제45권6호
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• pp.623-641
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• 2012

장군 연-아연-은 광상은 열수교대형 광상이다. 모암변질시 원소 분산을 알아보기 위해 모암, 열수변질대 및 연-아연-은 광맥에서 시료를 채취하였다. 이 광상은 능망간석화작용과 돌로마이트화작용으로 구성된 열수작용이 현저히 인지된다. 모암은 돌로마이트와 석회암이며 구성광물은 방해석, 돌로마이트, 석영, 금운모 및 흑운모 이다. 연-아연-은 광맥과 접촉한 부분에서 관찰되는 능망간석대는 주로 능망간석이 산출되며 소량 방해석, 돌로마이트, 쿠트나호라이트, 유비철석, 황철석, 황동석, 섬아연석, 방연석 및 황석석 등이 산출된다. 연-아연-은 광맥으로부터 멀어짐에 따라 관찰되는 돌로마이트대는 주로 돌로마이트가 산출되고 소량 방해석, 능망간석, 황철석, 섬아연석, 황동석, 방연석 및 황석석 등이 산출된다. 모암변질시 주원소, 미량 및 희토류원소들간의 상관계수는 $Fe_2O_3(T)$/MnO, Ga/MnO 및 Rb/MnO(돌로마이트 및 석회암)가 정의 상관관계를 갖고 MgO/MnO, CaO/MnO, $CO_2$/MnO 및 Sr/MnO(돌로마이트)와 CaO/MnO 및 Sr/MnO(석회암)가 부의 상관관계를 갖는다. 모암변질시 이득원소들은 $Fe_2O_3(T)$, MnO, As, Au, Cd, Cu, Ga, Pb, Rb, Sb, Sc, Sn 및 Zn 이고 손실원소들은 CaO, MgO, $CO_2$ 및 Sr 이다. 따라서 CaO, $CO_2$, $Fe_2O_3(T)$, MgO, MnO, Ga, Pb, Rb, Sb, Sn, Sr 및 Zn 등의 원소들은 모암이 돌로마이트내지 석회암인 열수교대형 광상의 탐사에 지시원소로서 활용될 수 있을 것이다.

• The Korean Journal of Ecology
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• 제21권3호
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• pp.313-320
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• 1998

Ameliorating effects of dolomite and sludge on the polluted soil sampled from Ulsan and yeocheon Industrial Complexes were investigated. Ameliorating effects were analysed by changes of soil properties and plant growth after treatment of dolomite and sludge. Soil properties were investigated by analysing organic matter, N, P, K, Ca and Mg contents and pH. Growth of sample plants was investigated by leaf area calculated from length and breadth of leaves and by biomass from diameter and height of sample plants. Quercus serrata and Celtis sinensis selected as tolerant plants in field survey were used as experimental plants. Treatment with dolomite showed ameliorating effects by increassing n, Ca, and Mg com\ntents, and pH of soil and by decreasing Al content. Treatment of sludge showed similar effects by increasing N, Ca, Mg and organic matter contents, and by decreasing A1 content. But treatment of sludge did not show any effect on pH. Both soil ameliorators showed accelerating effects on the growth of experimental plants in Ulsan soil. But those effects in Yeocheon soil were somewhat different. Treatment of sludge showed accelerating effects of the growth of both sample plants but dolomitic liming did not so. From those results, we confirmed availability of sludge, a kind of industrial waste, as one of ameliorators of the polluted soil. In addition, we recognized that soil properties had to be considered to select soil ameliorators suitable for restoration of degraded ecosystems.

• 자원환경지질
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• 제21권3호
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• pp.235-255
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• 1988

Talc deposit of pipe-like form occurrs in the lower part of the Hyangsanri Dolomite with a strike of N40 -50 E and a dip of 40 -50 NW which is one formation of the Ogcheon Super Croup. The pipi-like ore body plunge at about $40^{\circ}$ to the west and are parallel to the lineation developed in the area. Structural formulae of tales occurred in this deposit are close to the ieal composition $Mg_6Si_8O_{20}(OH)_4$ showing limited deviation from ideal one. Substitution of Al for Si in tetrahedral site is of little or nothing ranging 0-0.04 and octahedral occupancy is close to six ranging 5.88-5.98 atoms per unit cell. Predominant octahedaral cation is Mg and proportion of divalent cations is generally over 97percent. Calcite -dolomite thermometry is obtained by determining the mol % $MgCO_3$using of EPMA and XRD methods. The peak metamorphic temperature can be estimated at $470{\pm}30^{\circ}C$ in the area whereas carbonates occurred at near talc ore show lower temperature than $400^{\circ}C$ that the calcite solvus limit is not well established. It indicates that the talc deposit was formed at the lower temperature that the metamorphic temperature. Cosequently, the formation of talc by metamorphism is questionable and the alteratin zone developed around the talc ore is very limited. The occurrence of talc ore in the dolomite as well as mineralogy, calcite-dolomite geothermometry, chlorite geothermometry, field and microscopic evidence suggest that siliceous ascending hydrothermal solution along the fracture is responsible for the formation of talc. It was considered that the slight fracturing of dolomite was formed by deformation prior to the mineralization.

• 광물과 암석
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• 제34권2호
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• pp.107-120
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• 2021

검덕 연-아연 광상은 한반도에서 가장 규모가 큰 연-아연 광상으로 지체구조상 고원생대의 마천령층군이 포함된 Jiao Liao Ji belt내 혜산-리원 광화대에 위치한다. 이 광상의 주변지질은 고원생대의 마천리층군 변성퇴적암류와 이를 관입한 중생대의 만탑산 관입암체 및 신생대의 현무암으로 구성된다. 이 광상은 고원생대의 마천리층 변성퇴적암류내에 층상광체 및 맥상광체로 산출되며 퇴적분기형 광상에 해당된다. 이 광상에서 산출되는 돌로마이트들은 산출 광물조합 및 정출순서를 기초로 1)모암인 돌로마이트(D₀), 2)각섬암상의 변성작용에 의한 초기의 돌로마이트(투각섬석, 양기석, 투휘석, 섬아연석, 방연석 등)(D₁), 3)각섬암상의 변성작용에 의한 말기의 돌로마이트(활석, 방해석, 석영, 섬아연석, 방연석 등)(D₂), 4)석영맥과 함께 산출되는 돌로마이트(백색운모, 녹니석, 섬아연석, 방연석 등)(D₃)으로 산출된다. 이들 돌로마이트의 화학조성은 각각 Ca_1.00-1.20Mg_0.80-0.99Fe_0.00-0.01Zn_0.00-0.02(CO₃)₂(D₀), Ca_1.00-1.02M_0.97-0.99Fe_0.00-0.01Zn_0.00-0.02(CO₃)₂(D₁), Ca_0.99-1.03Mg_0.93-0.98Fe_0.01-0.05Mn_0.00-0.01As_0.00-0.01(CO₃)₂(D₂) 및 Ca_0.95-1.04Mg_0.59-0.68Fe_0.30-0.36Mn_0.00-0.01(CO₃)₂(D₃)로써 이론적인 돌로마이트의 화학조성보다 미량원소들의 함량이 높다. 이 미량원소들은 FeO, MnO, HfO₂, ZnO, PbO, Sb₂O₅ 및 As₂O₅ 원소들이며 광화작용이 진행됨에 따라 FeO, MnO, ZnO, Sb₂O₅ 및 As₂O₅ 원소들의 함량이 증감 변화가 있으나 HfO₂와 PbO 원소들의 함량은 증감 변화가 없다. 검덕광상의 D_o, D₁ 및 D₂는 Ferroan 돌로마이트에 해당되며 D₃는 Ferroan 돌로마이트와 철백운석(ankerite)에 해당된다. 따라서 1)모암인 돌로마이트(D₀)는 고원생대(2012~1700 Ma) 해양증발환경에서 실리카와 함께 퇴적된 후 계속적인 속성작용에 의해 돌로마이트화 작용에 의해 형성되었다. 2)초기의 돌로마이트(D₁)는 고원생대의 리원암군 관입(1890~1680 Ma)에 의한 변성작용(최소 각섬암상)에 의한 열수교대작용에 의해 형성되었다. 3)말기의 돌로마이트(D₂)는 각섬암상의 변성작용에 의한 계속적인 온도와 압력의 감소에 의해 잔존 유체로부터 형성되었다. 또한 4)석영맥의 돌로마이트(D₃)는 중생대의 만탑산 관입암체의 관입(213~181 Ma)에 의해 형성되었다.

• 환경위생공학
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• 제18권1호
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• pp.41-50
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• 2003

Traditionally the supernatant after chemical treatment of metal acid wastewater is discharged in environment. The supernatant can be used as a coagulant as it contains effective metals. The aim of this study is to investigate the feasibility of treatment of dyeing wastewater using the supernatant after treatment by magnesium hydroxide and dolomite($Ca{\cdot}Mg(CO_3)_2$), of acidic metal wastewater. In dyeing wastewater treatment with the supernatant, optimum pH and dosage were determined. COD, turbidity and color were analyzed to evaluate the performance of treatment. In the case of magnesium hydroxide, the optimum dosage was 10%(v/v) for supernatant A and 3%(v/v) for supernatant B. Color, turbidity and COD removal was 99~100%, 85~97% and 43~53%, respectively. In the case of dolomite, the optimum dosage was 10%(v/v) for supernatant A and 3% for supernatant B. Color, turbidity and COD removal was 96~99%, 62~9l% and 52~53%, respectively.

• 대한화학회지
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• 제19권4호
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• pp.252-257
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• 1975

無煙炭 炭分을 肥料로서 利用하기 爲하여 硏究를 하였다. 無煙炭 炭粉은 2% 시트르산 溶液中에서는 可溶物質이 大端히 적으나 ?燒된 dolomite를 添加한 無煙炭炭粉은 마그네슘, 칼슘, 황, 無水珪酸 等의 拘溶性 可溶分이 많아 지므로 肥料로서의 效果가 있음을 알았다.

• 대한화학회지
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• 제9권1호
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• pp.49-54
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• 1965

One of the difficult and time consuming problems in the production of magnesia from sea water is a settling rate of magnesium hydroxide. In this experiments, authors attempted to accelerate its settling rate by addition of various sedimenting agents as C.M.C., Separan and Starch, and sought for optimum calcination temperature for domestic dolomite, as alkali source, mole ratio of dolomite milk to bittern. It is observed through experiments that the small amounts of sedimenting agents, C.M.C., Separan, starch, 20 mg/l, 40 mg/l, 400mg/l, respectively increase the settling rate of magnesium hydroxide by 8 times or more. The following conditions resulted in good yield of magnesium hydroxide from sea water with relatively tolerable calcium oxide contaminated for the magnesium clinker. Calcinating temperature, $1,100{\sim}1,200^{\circ}C$, mole ratio of 10% dolomite milk to magnesium salts in sea water or bittern, 1. 2 : 1.

• 자원환경지질
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• 제13권1호
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• pp.65-68
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• 1980

Dolomite and quartz, starting materials, were mixed by the mole ratio of dolomite versus quartz with 1 : 0, 1 : 1, and 2 : 1, and of which was heated under saturated water vapor pressure of $20kg/cm^2(211.4^{\circ}C)$, $80kg/cm^2(293.6/C)$ and $120kg/cm^2(323.1^{\circ}C)$, respectively, during 20 hours. The results of the hydrothermal syntheses are as follows: 1) calcite crystals were formed at all cases of the reation 2) brucite crystals were formed when dolomite was heated under the saturated vapor pressure of $80kg/cm^2$ during 20 hours. 3) talc, tremolite, xonotlite, and antigorite were formed under saturated vapor pressure of $80kg/cm^2$ by 20 hours reaction.

• 에너지공학
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• 제20권4호
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• pp.298-302
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• 2011

In this study, Catalytic reforming with vapor and biomass gasification was simultaneously performed in a same fixed bed reactor at $600-800^{\circ}C$. Light gases were produced from reformation of the tar (fuel gases) in biomass gasification by using limonite and dolomite, as catalysts. Hydrogen and carbon dioxide are main components in light gases. Hydrogen yields increased with temperature increasing in the range of $650-800^{\circ}C$, because the water shift reaction was promoted by catalyst. The yield of hydrogen gas was increased about 160% under catalyst with the mixture of limonite and dolomite comparing to limonite only.