• 자원환경지질
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• 제1권1호
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• pp.9-34
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• 1968

Manganese ore deposits of the Samhan Changgun Properties are located at the valley of west-lope-side of Changgun-bong (1132m) occupied over the Myon border between Sochon-myon and Jaesan-myon Pongwha-gun, Kyongsang-Pukdo. Geology of the more property and it's vicinity consists of Wonnan formation and Yulri formation of pre-Cambrain and Changgun limestone formation, Mica-schist formation, quartizite formation and Jaesan formation (containing coal bearing zone the unknown age. And granites and dykes were intruded into the above formation later. 1. Management deposits is embedded the formation of Janggun limestone especially Contact zone in the contact zone to of Chunyang Granite limestone enclosed by Granite, and Maginal zone of fault line in the limestone. Therefore, Chunyang Granite is Closely related to ore deposit. Pegmatite which is near by ore deposit was intruded before mineralization and it seems to be a channelway of ore solution. The most important ore deposits of property grouped into south deposit, east deposit, east-Gachon deposit, South-Gachon deposit, Durimgok deposit and West deposit, out-crops at several place. Besides these deposits there also are several prospects on outcrop scathered. Hydrothermal alteration take place strongly in the well rock and it's sequence are Characterized as following; 1) Dolomitization 2) Carbonization 3) Mamgamotozation 4) Pyritization 5) Silicification 6) Oxidation 2. The grade of manganese dioxide is up to Mn 45% in Maximum, but generally, averaging Mn 30~35% of high grade ore and averaging Mn 30~32% of manganese carbonates are mined in his property.

• 자원환경지질
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• 제28권2호
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• pp.155-164
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• 1995

The kriging model, one of the geostatistical models, has been used to evaluate the deep-sea manganese nodule deposits until now. The distribution of the manganese nodule deposits estimated by the model shows the smooth surface as well as much difference from the actual distribution. Subsequently, it estimates the deposit distribution roughly in terms of the limited data of surveyed zone. Therefore, this paper presents the interpretation methodology of the deep-sea manganese nodule deposit distribution by using the fractal model to overcome the problems caused by the geostatistical model. Also, the manganese nodule distributions are interpreted by using the manganese nodule data sampled in the GH82-4 zone, west longitude $165^{\circ}40^{\prime}-169^{\circ}00^{\prime}$, and south latitude $0^{\circ}00^{\prime}-2^{\circ}40^{\prime}$ neighboring Nova-Canton Trough in the Pacific Ocean which was surveyed by the Geological Survey of Japan in 1982.

• 한국표면공학회지
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• 제26권4호
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• pp.183-191
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• 1993

Diffusion coating(metalliding) of aluminium on steel from molten fluorides(29.2wt.% LiF-11.7wt.% NaF-59.1wt.% KF, FLINAK) was studied. The electrolytic cell consists of a steel cathode and a consumable aluminium anode. Effects of manganese on the aluminium deposition were also investigated. The quality of the deposit was analyzed by SEM, OM, EPMA, EDXA, and also examined by means of Micro-Vickers hardness and corrosion tests. Deposit layer was identified as an aluminium-rich iron alloy caused by diffusion process. The optimum condition for the metalliding was found to be the current density, 50 to $150mA/\textrm{cm}^2$, the bath tem-perature, $57.5^{\circ}C$, and the amount of AlF3, 10wt.%. Addition of manganese fluoride (up to 5wt.%) as a co-de-posit element improved significantly the quality of the deposit layer.

• Journal of Welding and Joining
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• 제8권2호
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• pp.27-39
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• 1990

The effect of silicon and manganese, in the ranges of 0.3% to 1.0wt% Si and 0.7 to 2.6wt%Mn, on the microstructure and mechanical properties of flux cored arc welded deposits have been investigated for the purpose of improving mechanical properties. Microstructure of weld metals was mainly influenced by manganese content, and manganese increased the volum fraction of acicular ferrite and refined the microstructure. Also, tensile properties were governed by manganese content, ultimate tensile strength and yield strength were increased by approximately 82MPa and 58MPa per 1% Mn addition to the deposit. Toughness was improved by increasing Mn content and lowering Si content. Optimal impact properties were obtained at above 1.8wt% Mn and below 0.5wt% Si. Acicular ferrite was predominant factor in improving mechanical properties. Formation of acicular ferrite was promoted by manganese and no direct relationship between AF(acicular ferrite) proportion and oxygen in weld metal was found.

• 자원환경지질
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• 제57권1호
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• pp.25-39
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• 2024

The Téra manganese deposit represents the most significant manganese mineralization discovered in Niger up today. The main host rocks of this ore are gondites, which are a garnet and quartz rich metamorphic rocks. The supergene weathering developed an alteration profile on these gondites. This study aims to identify the mineralogical composition of gondites and associated rocks, in order to highlight the origine of rocks and the manganese enrichment. The methodological approach adopted involved a field study followed by polarizing microscopic analysis using transmitted and reflected lights. Additionally, quantitative X-ray diffraction (XRD) analysis was performed to assess the manganese ore minerals present in the gondite and associated rocks, including mica schists, amphibolites, and quartzites. The petrographic study revealed a paragenesis characterized by the presence of kyanite, staurolites, garnets and plagioclases that are generally poikiloblasts with quartz and opaque minerals inclusions, emphasizing the internal schistosity which is planar, helicitic or microfolded. These features indicate a prograde metamorphism until high-pressure amphibolite facies conditions. These conditions are followed by greenschist facies conditions marked by calcite, epidote, muscovite, chlorite and muscovite assemblage which emphasizes the vertical tectonics. Depending on the alteration process, the manganese ore exhibit a granular texture at the bottom of the gondite hills, transitioning to a colloform texture towards the top, passing through the epigenization and replacement texture. The XRD analysis further revealed that the studied rocks originated from a volcano-sedimentary complex, characterized by alternating marly, arenaceous and pelitic sequences associated with submarine exhalations.

• 한국광물학회지
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• 제5권1호
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• pp.1-5
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• 1992

太白山地區의 主要 망간鑛床에서 産出하는 酸化망간 鑛物들은 一次的으로 생성된 炭酸망간 또는 珪酸망간의 表成風化作用에 依하여 生成되었다. 이들 酸化망간 鑛石의 生成에 관여된 地質作用에는 溶解作用, 酸化作用, 運搬作用, 沈澱作用, 晶出作用 및 再結晶作用 等이 있다. 그러나 箇箇의 酸化망간 鑛物 生成은 交代作用, 溶液으로부터의 晶出作用 및 固體狀態에서의 晶出, 및 再結晶作用 等에 依하여 이루어졌다. 이들 鑛物生成作用에 依하여 多樣한 名種 鑛石의 組職이 形成되었으며, 母鑛石의 鑛物組成과 風化環境에 따라 特徵的인 鑛物 및 鑛物共生關係가 形成되었다. 그러나 一般的으로 風化殘留鑛床 중의 酸化망간 鑛物들은 $Mn^{2+}{\to}Mn^{3+}{\to}Mn^{4+}$의 方向으로 生成되었다.

• 한국측량학회지
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• 제27권6호
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• pp.679-688
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• 2009

최근 차세대 신에너지 자원으로 각광받고 있는 심해저 망간단괴에 대한 탐사와 연구가 전 세계적으로 진행되고 있다. 이에 국내에서도 한국해양연구원을 중심으로 수심 5,000m의 태평양에 광범위하게 분포된 망간단괴 채취를 위한 다양한 연구가 수행되고 있다. 정확한 채취량의 산정과 경제성을 분석하기 위해서는 정밀탐사가 요구되며, 이를 위하여 심해저 수중 카메라로부터 촬영된 영상을 처리하고 분석하여 망간단괴의 분포특성에 대한 정보를 추출할 수 있다. 본 연구는 심해저 영상에서 극심하게 발생하는 vignetting 현상을 효과적으로 제거하여 화질을 향상시키고, 영상에서 망간단괴를 추출하여 필요한 정보를 제공하는 방법을 제안하였다. 연구결과 vignetting 현상을 제거함으로써 보다 향상된 결과를 도출할 수 있었으며, 이를 기반으로 망간단괴에 대한 다양한 정보를 분석하여 향후 채취를 위한 계획수립 시 중요한 기초자료로 사용될 것으로 기대한다.

• Corrosion Science and Technology
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• 제13권3호
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• pp.102-106
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• 2014

Nickel electrodeposition from sulfamate bath has several benefits such as low internal stress, high current density and good ductility. In nickel deposited layers, sulfur induces high temperature embrittlement, as Ni-S compound has a low melting temperature. To overcome high temperature embrittlement problem, adding manganese is one of the good methods. Manganese makes Mn-S compound having a high melting temperature above $1500^{\circ}C$. In this work, the mechanical properties of Ni-Mn deposited layers were investigated by using various process variables such as concentration of Mn$(NH_2SO_3)_2$, current density, and bath temperature. As the Mn content of electrodeposited layers was increased, internal stress and hardness were increased. By increasing current density, internal stress increased, but hardness decreased. With increasing the bath temperature from 55 to $70^{\circ}C$, internal stress of Ni deposit layers decreased, but hardness didn't change by bath temperature. It was likely that eutectoid manganese led to lattice deformation, and the lattice deformation increased hardness and internal stress in Ni-Mn layers. Increasing current density and decreasing bath temperature would increase a mount of $H_2$ absorption, which was a cause for the rise of internal stress.

• 자원환경지질
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• 제17권1호
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• pp.17-34
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• 1984

어상천 망간광상은 조선계 홍훨리층의 돌로마이트와 삼태산층의 석회암내에 발달한 단층 파쇄대를 따라 형성된 표성산화망간광상이다. 본 산화망간광상의 하부에는 백악기 석영반암에 의하여 형성된 열수교대 내지 충진광상이 본 단충파쇄대를 따라 발달한다. 석영반암은 주성분으로 부터 계산한 노음치를 Q-K-F-PI 삼각도에 점시하면 북서단은 화강섬록암의 영역에 그리고 주암체는 화강암의 영역에 점시되고 D.I.치는 상기 북서단에서 부터 주암체쪽으로 증가한다. 따라서 이것은 마그마의 분화작용과 관계되는 것으로 보인다. 본 석영반암내 암질의 차이는 미량성분에도 반영이 되어 나타나고 있는 데 북서단에서 아연, 닉켈, 크롬, 몰리브텐의 함량이 높고 주암체에서는 동, 연의 함량이 높은 현상은 산성암과 염기성암에서 일반적으로 볼 수 있는 함량의 변화와 일치한다. 경상분지내 백악기 화강암류와 비교해 보면 동, 연, 아연, 닉켈, 크롬의 함량은 석영반암쪽이 분지내 동광상구의 화강암류보다 낮으나 동과 닉켈의 함량은 연 아연 광상구의 화강암류보다도 높은 경향을 보인다. 석회암 및 돌로마이트로 구성된 모암은 석영반암에 의한 광화작용으로 단층파쇄대에서는 망간, 연, 아연, 동등의 함량이 현저히 높고 멀어짐에 따라 감소되는 일차후생분산형태를 보인다. 토양중 미량원소의 함량은 토양의 생성조건 및 물리화학적조건과 밀접한 관계를 보이며 모암에서의 그들이 형성하는 탄산염의 용해도와도 주목할만한 관계를 보인다. 즉 난용성의 탄산염을 형성하는 미량원소는 토양중의 함량도 낮은 경향을 보인다.

• 자원환경지질
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• 제43권5호
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• pp.455-466
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• 2010

한국이 현재 탐사하고 있는 해저광물자원의 유형은 망간단괴, 망간각, 다금속황화광체 등으로 구분된다. 망간단괴에 함유되어 있는 주요 희소금속은 Pt로 지각함량 대비 최대 400 배까지 부화되어 있다. 망간단괴의 총 희토류 함량은 0.037~0.302 REO %, 평균 0.12 REO %를 보인다. 망간각의 주요 희소금속은 Te 및 Pt로 각각 10800 배, 150배 정도의 부화량을 보인다. 총 희토류 함량은 0.013-0.387 REO %, 평균 0.18 REO %로 망간단괴 보다 다소 높은 함량을 보인다. 다금속화황광체의 주요 희소금속은 Se 및 In으로 각각 1300 배, 110 배의 높은 부화량을 보이며, 금(0.8~26.3 g/t), 은(0.9~348.0 g/t) 등의 귀금속이 함유된다. 해저광물자원에 함유되어 있는 희유금속은 채광 예상 금속 종인 Co, Ni, Cu 등의 채광 경제성을 높여 줄 것으로 생각되며 첨단산업을 위한 희유금속 확보 차원에서 의미가 있다.