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구룡광산 광미층의 심도변화에 따른 물리.화학적 및 광물학적 특성
문용희,김정연,송윤구,문희수,Moon, Yong-Hee,Kim, Jeong-Yeon,Song, Yun-Goo,Moon, Hi-Soo 대한자원환경지질학회 2008 자원환경지질 Vol.41 No.2
본 연구에서는 구룡광산에 적치된 광미층으로 부터 채취된 대표 비교란 코어시료를 대상으로 체계적인 물리 화학적 및 광물학적 특성을 심도별로 정량적으로 파악, 중금속 거동 핵심 영향요소를 기준으로 광미층 수직분대를 시도하고, 이를 기초로 광미층 비포화대-포화대에 걸친 원소 거동과 지화학적 조건과의 상관모델을 제시하고자 한다. 구룡광산의 대상 광미층은 화학적으로 지하수면을 경계로 상부층 구간에서의 낮은 pH(4)와 20wt.% 이상의 높은 $Fe_2O_3$ 및 $SO_3$ 함량에 의해 특징지어진다. 물리 화학적 및 광물학적 분석 자료를 고려하여 구룡광산 광미층을 심도증가에 따라 복토층, jarosite zone, Fe-sulfate zone, Fe-oxyhydroxide zone, gypsum-bearing pyrite zone, calcite-bearing pyrite zone, soil zone(광미층 집적 이전 토양층), weathered zone 등 7개분대로 구분할 수 있으며, 새로 생성된 이차광물상의 특성을 고려할 때 지하수면을 기준으로 상부층을 산화대(oxidation zone)로, 하부층을 비산화대(unoxidation zone), 혹은 carbonate-rich primary zone으로 크게 대분할 수 있다. 본 연구결과를 기초로 구룡광산 광미층의 물리 화학적 및 광물학적 변화를 지하수면 상부층에서의 황화광물, 특히 황철석의 산화반응이 핵심요소가 되어, 이로 인한 pH 값의 감소, 일차광물의 용해반응 및 원소 용출, 이차광물상 생성, 그리고 생성된 산의 탄산염 및 규산염광물에 의한 산-중화반응 등 일련의 지화학적 반응으로 설명할 수 있다. This study is focused on characterization of the physio-chemical and mineralogical properties, investigation of their vertical changes in the tailing profile of the Guryoung mining area, classification of the profile into distinct zones, and condition conceptual model of physio-chemical conditions and phases-water relationships controlling the element behaviors in the tailings. The upper part of the groundwater is characterized by the high contents of $Fe_2O_3$ and $SO_3$ for whole rock analysis, low pH, and the occurrence of jarosite, schwertmannite and Fe-oxyhydroxide as the secondary mineral phases. The tailing profile can be divided into the covering soil, jarosite zone, Fe-sulfate zone, Fe-oxyhydroxide and gypsum-bearing pyrite zone, calcite-bearing pyrite zone, soil zone, and weathered zone on the based of the geochemical and mineralogical characteristics. The profile can be sampled into the oxidized zone and the carbonate-rich primary zone with the dramatic changes in pH and the secondary mineral phases. The conceptual model proposed for the tailing profile can be summarized that the oxidation of pyrite is the most important reaction controlling the changes in pH, the dissolution of the primary silicates and carbonates, the precipitation of secondary mineral phases, acid-neutralizing, and heavy metal behaviors through the profile.
MCDM 기법을 이용한 도심지 토사재해 예방을 위한 도시계획적 대책 위치 결정방법 제안
문용희,이상은,김소윤,김명수,Moon, Yonghee,Lee, Sangeun,Kim, Soyoon,Kim, Myoungsoo 한국안전학회 2017 한국안전학회지 Vol.32 No.5
The landslide disaster damage has been increased by mountain development, leading to construction of educational facilities, medical facilities, petty industrial facilities, and large housing complexes. Therefore, effective regulation is required as an effort in urban planning solutions. For suggesting specific mitigation strategies on urban landslide, this study aims to define evaluation criteria for urban planning management of debris-flow disaster. AHP (Analytic Hierarchy Process), one of the multiple criterion decision making methods, was utilized in this study. This study makes use of 16 sub-criteria under the framework of hazard, exposure, and vulnerability, and well-planned expert survey measures their weights. The weights are also applied to evaluate each grid in urban space (min $10{\times}10m$) and classify it with red, orange, yellow, or green grade so that areas at higher risk are clearly identified. This study concludes that the suggested method is useful to support a strategies for urban planning management of debris-flow disaster, particularly in a GIS base.
문용희(Yonghee Moon),송윤구(Yungoo Song),문희수(Hi-Soo Moon),장용선(Yong-Seon Zhang) 한국토양비료학회 2010 한국토양비료학회지 Vol.43 No.3
The laboratory column experiments were used to transport of metal elements by infiltration-related dispersion and/or diffusion in mine tailing of the Guryong gold mine. The mine tailing shows the neutral pH (for a pore water) and contains quartz, chlorite, pyrite and calcite. Both a non-reactive solute (Cl<SUP>-</SUP> of 100 mg L<SUP>-1</SUP>) and a reactive solute (1N HCl), were injected continuously through columns. The breakthrough curve in the non-reactive experiment reached at a maximum under 1.5 pore volumes (PV). The longitudinal dispersion (0.607 cm) and hydrodynamic dispersion coefficient (1.96×10<SUP>-7</SUP> cm² sec<SUP>-1</SUP>) were calculated by the slope. In the reactive experiment, the plateau curve was appeared in the pH values of 5.3, 4.5 and 1.7. The releases of metal elements such as Fe, Mn, Al, Cu, Zn, Pb, and Cd were observed to be related to the pH buffering. High concentrations of Mn, Cd and Zn were observed at the first pH plateau (4 PV and pH 5.3), whereas Fe, Cu, Al and Pb were released as the pH decreased to 4.0 or less. The resulting order of metals mobility, based on the effluent water, is Mn=Cd>Zn>Cu>Fe>Al>Pb.
전황함량과 순산발생능력의 상관관계를 통한 잠재특이산성토양 기준 설정
문용희(Yonghee Moon),장용선(Yong-Seon Zhang),현병근(Byung-Keun Hyun),손연규(Yeon-Kyu Sonn),박찬원(Chan-Won Park),송관철(Kwan-Cheol Song) 한국토양비료학회 2012 한국토양비료학회지 Vol.45 No.6
황철석 (Pyrite, FeS<sub>2</sub>)을 함유한 잠재특이산성토는 강하류 삼각지 토양, 간척지 등의 해성토뿐만 아니라, 영일만과 같은 융기해성토 지대, 내륙의 선상지하단 유기물이 많은 암흑색 토층이 있을 때에 존재하는 수가 있다. 또한 안산암지역의 열수작용에 의해 생성되어 암맥을 따라 형성된 황철석이 광산개발이나 도로건설로 절취사면에서 노출되어 산화되면 매우 강한 산성을 띠는 특이산성토층을 형성하여 주변농경지에 피해를 주고 있다. 현재 잠재특이산성토양의 판정은 현장에서는 과산화수소로 반응 시 수증기발생 정도로 판단하거나 실내실험에서는 전황 (Total-S)성분의 함량으로 판단한다. 하지만 이들 방법은 시군농업기술센터 및 현장 진단 시 적용이 용이하지 않다. 산발생 능력평가 중 순산발생능력실험 (Net Acid Generation, NAG pH)은 대상지역의 산성발생 가능성에 대한 예측을 정량적 계산으로 가능하다. 순산발생능력실험을 이용하여 전황함량과 NAG pH와의 상호관계를 통해 특이산성토양 판정을 제안하기 위해 화산기원의 잠재특이산성 토양과 사양질 토양을 일정비율로 혼합된 토양과 특이산성토양인 김해통과 해척통 토양에 대해 실험을 수행하였다 전황의 함량이 0.75% 이상인 시료의 NAG pH가 2.5이며 0.75-0.50%의 중간 특이산성토양은 NAG pH 3.0으로 측정되었다. 그리고 전황 함량이 0.5-15% 약한 특이산성 토양은 NAG pH 3.8로 측정되었다. 따라서 순산발생량은 NAG pH를 이용하여 토양 내 황철석을 모두 산화시키고 pH를 측정하여 pH 3.8이하인 토양은 특이산성토양으로 구분하는 것이 타당할 것으로 판단되었다. Acid sulfate soil (ASS) and potential acid sulfate soil (PASS) are distribution in worldwide and originate from sedimentary process, volcanic activity, or metamorphism and are problematic in agriculture and environmental due to their present and potential acidity developed by the oxidation. The PASS was defined as soil materials that had sulfidic layer more than 20 cm thick within 4 m of the soil profile and contained more than 0.15% of total-sulfur (T-S). A tentative interpretative soil classification system was proposed weak potential acid sulfate (T-S, 0.15-0.5%), moderate potential acid sulfate (T-S, 0.5-0.75%) and strong potential acid sulfate (T-S, more than 0.75%). PASS due to excess of pyrite over soil neutralizing capacity are formed. It provides no information on the kinetic rates of acid generation or neutralization; therefore, the test procedures used in acid base account (ABA) are referred to as static procedures. The net acid generation (NAG) test is a direct method to measure the ability of the sample to produce acid through sulfide oxidation and also provides and indication. The NAG test can evaluated easily whether the soils is PASS. The samples are mixed sandy loam and the PAS from the hydrothermal altered andesite (1:3, 1:8, 1:16, 1:20, 1:40, 1:80 and 1:200 ratios) in this study. We could find out that the NAG pH of the soil containing 0.75% of T-S was 2.5, and that of the soil has 0.15% of T-S was 3.8. NAG pH test can be proposed as soil classification criteria for the potential acid sulfate soils. The strong type has NAG pH of 2.5, the moderate one has NAG pH of 3.0, and the weak one has NAG pH of 3.5.