• 한국지반공학회논문집
• /
• 제26권12호
• /
• pp.61-70
• /
• 2010

해안매립지와 같은 연약한 점토지반에 시공된 쇄석말뚝의 내진성능 평가를 위해 1g 진동대 실험을 수행하였다. 개량전 후 지반의 동적응답특성을 비교하기 위해 가속도 증폭 및 시간에 따른 전단변형, 전단파 속도 등을 평가하였다. 실험 결과, 쇄석말뚝으로 개량된 지반의 전단변형은 개량되지 않은 지반에 비해 감소되는 경향을 보이나, 단주기 지진파에는 더 높은 수준의 지반 가속도 증폭이 발생되는 것으로 나타났다. 따라서 쇄석말뚝으로 개량된 지반의 내진성능 향상여부는 모형실험과 함께 지반응답해석 등의 수행하여 평가되어야 한다고 판단된다.

• 자원환경지질
• /
• 제24권1호
• /
• pp.63-69
• /
• 1991

Gravity study was carried out to investigate the structure and total mass of the Bupyeong silver deposits closely related to formation of the Bupyeong caldera. Survey region covers $3.3{\times}6.6km^2$ over silver deposits and is comprised of 334 gravity measurement stations. An apparent regional gravity trend parallel to the west coast line is mainly attributed to isostasy. A least square isostasy model was used for the regional correction. A Fortan subroutine was coded to calculate 3-dimensional subsurface model. The calculated gravity values from the 3-dimensional model of the caldera with silver deposits agree with observed anomalies relatively well. Gravity anomaly due to Bupyeong silver deposits reaches to +3.5 mgal from the background value and anomaly due to the caldera reaches to -4 mgal. But the maximum negative anomaly of the caldera would be much greater at its center. The total mass of silver deposits calculated from the subsurface model is $4.19{\times}10^9$ tons. Although the economic part of silver deposits depends on the grade of orebody, we expect that there are still large amount of silver reserves in Bupyeong area.

• 자원환경지질
• /
• 제31권5호
• /
• pp.431-446
• /
• 1998

The calcretes from the Cretaceous Gyeongsang Supergroup in the vicinity of Ulsan city have been examined at five sites (Daedong, Seodong, Ansachon, Deogha, and Mangyangri). In these calcretes, evidences indicating pedogenic origin are recognized. Included are calcite aureoles around detrital grains, pedotubular pores, microstromatactis, circumgranular cracks, fitted structure of adjacent peloids, calcrete ooids, rhizocretions, and calcrete intraclasts. On the basis of calcrete development together with lithofacies, the depositional environments of those deposits are interpreted as lake margin (Daedong deposits), braided to low-sinuosity river (Seodong deposits), braid plain (Ansachon deposits), and meandering river (Deogha and Mangyangri). Stratigraphically, the fluvial deposits of study area show paleoenvironmental change from braided to low-sinuosity river plain under arid climatic condition to meandering river plain under seasonally wet an dry climatic condition. The stratigraphic successions of the Gyeongsang Supergroup of the study area Qacustrine-fluvial-Iacustrine) together with paleoenvironmental change of fluvial deposits suggest that those deposits can be correlated with the Banyaweol-Songnaedong-Geoncheonri formations of the Gyeongsang Supergroup in the western part of the Yangsan Fault.

• 한국환경과학회지
• /
• 제7권2호
• /
• pp.149-156
• /
• 1998

Enoronmental problems caused by certain geologic conditions Include pollution of soil by heavy metal, acidization of souls , acid mine drainage, Pound-water pollution, and natural radioactivity, as well as zoo-logical hazards such as landslide and subsidence. The acrid mine drainage contains large amount of heavy metals nO, therefore. cause serious pollution onto the nearby drainage systems and soils. In spite of this prospective environmental danger, few studies have been done on the acid mine drainage derived from non-metallic ore deposits such as pyrophyllitefNapseok) deposits. The sudo-bearing pyrophyllite ores, alteration zones, and mine talllngs of pyrophylllte deposits produce acrid mine drainage by the okidation of weathering. Compared to the fresh host rocks, the ores and altered rocks of pyrophyllite deposits produce acidic solution which contain higher amount of heavy metals because of OeP lower buffering capacity to acrid solution. The pus of urine water and nearby stream water of pyrophyllite deposits are 2.1~3.7, which are strong- ly acidic and much lower than that (6.2~7.2) of upstream water and than that (6.8~7.6) of the stream water derived from the non-mineralized area. This study reveals that this acrid mine drainage can affect the downstream area which is 8km far from the pyrophyllite deposits, even though the drain Is diluted with abundant non-contaminated river water This suggmists that not only acid mine drainage but also the sulfide-bearing sediments originated from the pyrophyllite deposits move downstream and form acidic water through continuous oxidation reaction. The heavy metals such as Pb, Zn, Cu, Cd, Nl, Mn and Fe are enriched In the mine water of low pH, and their contents decrease as the pH of mine water Increases because of the Influx of fresh stream wainer. SoUs of the Pyrophyulte deposits are characterized by high contents of heavy metals. The stream sediments containing the yellowish brown precipitates formed by neutralization of acid mine drainage occur in all parts of the stream derived from the pyrophyllite deposits, and the sediments also contain high amounts of heavy metals. In summary, the acid mine drainage of the pyrophyllite deposits is located in the upstream part of Hoidong water reservoir in Pusan contains large amounts of heavy metals and flows into the Holdong water reservoir without any purification process. To protect the water of Holdong reservoir, the acid mine drainage should be treated with a proper purification process.

• 대한치과의사협회지
• /
• 제57권4호
• /
• pp.213-220
• /
• 2019

Purpose: The aim of this study was to evaluate the red fluorescence characteristics of bacterial dental deposits assessed by quantitative light-induced fluorescence (QLF) technology and confirm whether the red fluorescence can distinguish and evaluate quantitatively accumulation of bacterial dental deposits. Methods: This retrospective cross-sectional study used QLF images captured at a dental clinic from January to December 2016. In each QLF image, a skilled examiner selected one region where the presence of deposits was suspected. Then, the regions were classified into three groups of not detectable deposits(ND), half detectable deposits (HD), and full detectable deposits (FD) by two examiners according to classification criteria. Only those images where the regions of bacterial dental deposits were classified identically by all examiners were used for analysis. The mean red fluorescence intensity (RFI) was defined as the mean value of R/G for all pixels in the regions. The RFI was compared between groups using Welch's ANOVA test, and the Spearman correlation was calculated to assess the association between RFI and accumulation of deposits. Results: In this study, 351 images among the collected images of 605 subjects were finally selected. The mean age of subjects was about 44 years. The R/G values of the ND, HD and FD were 0.73, 1.26 and 1.83 respectively. There were significant differences between all groups (p<0.001), and strong positive correlation was identified between the R/G value and the accumulation of deposits (r = 0.90, p<0.001). Conclusion: The intensity of red fluorescence as observed in the QLF images correlated well with the accumulation maturation of the deposits, which indicates that the QLF technology can be used to evaluate the status of oral hygiene.

• 한국지반공학회:학술대회논문집
• /
• 한국지반공학회 2009년도 세계 도시지반공학 심포지엄
• /
• pp.755-760
• /
• 2009

It is essential to carry out site investigations such as SPT, CPT sampling etc. to understand the characteristics of soil deposits. However, the results deduced only from the engineering standpoint have limited information to fully understand ground characteristics. In this study, it is discussed site investigation results on Youngjong deposits obtained from not only the geotechnical standpoint, but also geotechnical and geological mixed standpoint to understand correct characteristics of Youngjong soil deposit.

• 자원환경지질
• /
• 제25권4호
• /
• pp.397-416
• /
• 1992

본 논문에서는 해남지역의 점토광상인 성산, 옥매산 및 해남광상을 연구대상으로 하였다. 열수변질을 받은 각 점토광상은 중심으로부터 주변부로 감에 따라 변질대를 형성하고 있는데, 성산광상의 경우 카올린대, 카올린-석영대, 견운모대 및 녹니석대의 변질대가, 옥매산광상의 경우 석영대, 명반석대, 카올린대, 견운모대 및 녹니석대의 변질대가, 그리고 해남광상의 경우 석영대, 납석대, 견운모대 및 녹니석대의 변질대가 각각 나타나고 있다. 이같은 변질대들은 두 종류의 변질작용으로 구분될 수 있는데, 하나는 납석대, 명반석대, 석영대, 카올린대 및 카올린-석영대와 같은 산변질작용 (acidic alteration)이고, 다른 하나는 녹니석대와 일부 견운모대와 같은 프로필리틱 (prophylitic alteration) 이다. 모든 점토광상은 high sulfidation (acidic-sulfate) 계에 속한다. 산변질작용의 암석은 납석, 명반석, 카올린광물, 견운모, 석영 및 황철석 등으로 구성되어 있다. 전암화학분석의 결과 $SiO_2$, $TiO_2$, $Fe_2O_3$, MgO, CaO, $K_2O$ 및 $Na_2O$와 같은 원소들은 원암의 조성과 상당한 차이를 보여주고 있는데, 이같은 주원소들의 유동성은 각 변질대의 광물조합과 관련되어 이들에 영향을 주고 있다. 견운모의 폴리타잎(polytype) 은 X-선 회절분석결과, $2M_1$ 및 1M 형으로 밝혀졌다. 성산광상의 경우 $2M_1$ 및 1M 형이 거의 같은 비율로 나타나고, 옥매산광상의 경우 1M 형이 우세한 반면, 해남광상의 경우 $2M_1$ 형이 우세하게 나타나고 있다. 이같은 현상은 견운모의 형성온도를 반영하는 것으로, 해남광상이 가장 고온에서, 성산광상은 중간온도에서, 그리고 옥매산광상이 가장 저온에서 형성되었음을 지시해 준다. 전자현미 분석결과, 면반석의 Na/(K+Na)의 비율이 옥매산광상의 것이 성산광상의 명반석이 성산광상의 것보다 높은 것으로 나타났는데, 이는 옥매산광상의 것보다 상대적으로 고온에서 높은 Na/(K+Na) 값과 낮은 pH 값을 갖는 용액에서 형성되었음을 시사해 준다. 모든 분석결과를 종합하여 볼 때, 명반석은 hypogene 기원이며, steam-heated 환경에서 hydrogen sulfide의 산화작용에 의하여, 그리고 오늘날의 열수계에서 관찰할 수 있는 solfataric alteration의 결과로 형성되었음을 알 수 있다.

• 한국진공학회지
• /
• 제15권4호
• /
• pp.421-426
• /
• 2006

화학증착 시스템의 파이프내 발생하는 오염입자의 진단을 위하여 초음파 및 진동진단법을 각각 비교, 연구하였다. 초음파 진단의 경우 파이프 외벽에 초음파 센서를 부착하여 펄스를 가한 후 에코 분석을 통해 파이프내벽의 오염입자를 관찰하였고 진동 진단의 경우 파이프외벽에 부착된 진통발생기를 통해 파이프에 인위적인 진동을 발생시켜 여기에서 발생되는 주파수 차이를 분석, 파이프내의 오염입자 여부를 관찰하였다. 초음파 진단의 경우, 오염입자가 파이프 내벽에 부착되어 있을 때는 효과가 좋았으나 오염입자가 시간이 지남에 따라 건조되어 파이프 내벽에서 떨어져 나와 파이프 내벽과 오염입자사이에 틈새가 생길 경우 초음파 펄스는 이 공간을 통과하지 못하고 파이프 내벽에서 다시 반사되어 오염입자를 진단하지 못하는 경우가 발생하였다. 따라서 초음파 진단법으로는 진공장비의 오염입자 관찰에 재현성을 보여주지 못하는 것으로 확인되었다. 반면 진동진단법의 경우 위와 같이 일정시간이 지난 동일한 샘플의 경우에서도 오염입자에 의한 차이가 관찰되었다, 즉 파이프내 오염입자가 존재시 새 파이프에 비해 진동음이 저주파대로 떨어짐이 확인되어 추후 화학증착 시스템의 파이프내 오염입자 모니터링 연구에 가장 효과적인 방법으로 기대된다.

• 자원환경지질
• /
• 제41권6호
• /
• pp.773-795
• /
• 2008

우리나라의 주요 수입 광종은 동광, 연-아연광, 철광, 망간광 및 몰리브덴광 등이다. 우리나라의 해외자원개발은 아시아 14개국 92개 사업, 미주 및 유럽지역 10개국 29개 사업 그리고 중동 및 아프리카 9개국 14개 사업이 있으며 주로 호주, 중국, 몽골 및 인도네시아에서 사업수가 높다. 호주, 인도네시아 및 중국의 사업은 대부분이 석탄이고 일부 망간, 철, 연-아연, 니켈, 구리, 금, 몰리브덴, 희유원소 및 우라늄 등이나 몽골은 금과 희유원소가 큰 부분을 차지한다. 금속자원에 대한 광상 유형별 대표적인 광상형은 조산 lode형 광상, VMS형 광상, 반암형 광상, SEDEX형 광상, MVT형 광상, IOCG형 광상 및 마그마성 Ni-Cu-PGE형 광상 등이 있으며 이들 유형별 광상들은 전세계적으로 도처에 분포하며 다른 유형별 광상보다 금속자원의 매장량이 높고 부산물인 미량 금속자원에 대한 품위도 높게 나타난다. 따라서 향후 해외광물자원의 탐사 및 개발에 있어 우선 각 국가별 매장량, 주요 광물자원의 생산량 및 지체구조와 함께 광상 유형별 등을 종합 검토하여 조사 및 탐사를 실시한다면, 해외자원개발의 투자 위험도가 감소될 뿐만 아니라 탐사대상지역에서 품위가 높은 광체를 확보할 수 있을 것이다.

• 자원환경지질
• /
• 제25권1호
• /
• pp.41-50
• /
• 1992

Mineral assemblages, mineral chemistries and stable isotope compositions of altered rocks of the Ogmae, Seongsan, Haenam and Gusi mines near the Haenam volcanic field in the southwestern part of the Korea peninsula were studied. Characteristic hydrothermal alteration zones in these deposits occurring in the Cretaceous volcanics and volcanogenic sediments, acidic tuff, and rhyolite, were outlined. Genetic environment with particular reference to the spatial and temporal relationships for these deposits were considered. The alteration zones defined by a mineral assemblage in the Ogmae and Seongsan deposits can be classified as alunite, pyrophyllite, kaolinite or dickite, quartz, illite or illite/smectite. Alunite was not developed in the Gusi and Haenam deposits. Boundaries between the adjacent zones are always gradational except for vein-type alunite. Alteration zones are superimposed upon each other in some localities. These deposits formed $71.8{\pm}2.8{\sim}76.6{\pm}2.9$ Ma ago, which is the almost same age of later volcanic rocks $79.4{\pm}1.7{\sim}82.8{\pm}1.2$ Ma, the Haenam Group, corresponding to Campanian. It indicates that hydrothermal alteration of these deposits appeared to be related to felsic volcanism in the area. Consideration of the stability between kaolinite, alunite, pyrite and pyrophyllite, and the geothermometry based on the mineral chemistry of illite and chlorite suggests that the maximum formation temperature for alunite and pyrophyllite can be estimated at about $250^{\circ}C$ and $240{\sim}290^{\circ}C$, respectively. It also suggests that these deposits were formed by acidic sulfate solution with high aqueous silica and potassium activity in a shallow depth environment. Compositional variation of alunite also suggests that the physico-chemical conditions fluctulated considerably during alteration processes, indicating shallow depth environment. The Haenam deposit was formed at a relatively greater depth than the others. The sulfur isotope composition of alunite and pyrite indicates that sulfur probably had a magmatic source, and the oxygen isotope composition for kaolinite indicates that the magmatic hydrothermal solution was diluted by circulating meteoric water.