• Title/Summary/Keyword: 이차분석

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Mineralogical Changes Caused by the Weathering of Tailings Deposited on the Riverside of the Nakdong River, Bonghwa, Korea (봉화군 일대 낙동강변에 퇴적된 광미의 풍화에 따른 광물학적 변화)

  • Kim, Min-Jung;Kim, Yeong-Kyoo;Park, Hyoung-Sim;Jeon, Sang-Ho
    • Journal of the Mineralogical Society of Korea
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    • v.21 no.4
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    • pp.331-339
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    • 2008
  • In the upstream of Nakdong river in Bonghwa-gun, Gyeongsangbuk-do, certain areas of riverside were found to be covered by weathered mine tailings which were assumed to be migrated and deposited by flood. This study was conducted to investigate the formation and characteristics of the secondary minerals from tailings and related leaching behavior of heavy metals in the severely weathered tailing deposits by river waters. Quartz, feldspar, micas, chlorite, hornblende, talc, pyroxene (johannsenite), pyrite, and calcite were identified as primary minerals by XRD. Kaolinite can be formed by the weathering of tailings, but considering the short period of weathering time, kaolinite in the deposits is considered to be from unweathered tailings or moved from soils. The secondary minerals such as goethite, gypsum, basanite, and jarosite were also identified. The formation of the secondary minerals was affected by the species of primary minerals and pH conditions. The weathering of pyrite produced sulfate minerals such as gypsum, basanite, jarosite, and also goethite. Mn oxide was also identified by SEM, coated on the primary minerals such as quartz. This Mn oxide was poorly crystalline and thought to be the weathering product of johannsenite (Mn-pyroxene). The Fe and Mn oxides are the main minerals determining the brown/red and black colors of weathered tailings. EDS results showed that those oxides contain high concentrations of Pb, Zn, and As, indicating that, in the river, the formation of Fe and Mn oxides can control the behavior and leaching of heavy metals by co-precipitation or adsorption.

Structure and Dynamics of Pinus densiflora Community in Mt. Kaya (가야산(伽倻山) 소나무(Pinus densiflora)군락(群落)의 구조(構造) 및 동태(動態))

  • Bae, Kwan Ho;Hong, Sung Cheon
    • Journal of Korean Society of Forest Science
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    • v.85 no.2
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    • pp.260-270
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    • 1996
  • Structure and dynamics of Pinus densiflora community in Mt. Kaya were studied to provide the information needed for management of Pinus densiflora forest in the southern inland of Korea. Stratification structure of Pinus densiflora community in the lower and middle slope consisted of tree layer(10~15m), subtree layer(4~10m), shrub layer(1~4m), and herb layer(below 1m), while in the rock zone of ridge and top area consisted of tree layer(7~10m), subtree layer(2~7m), shrub layer(1~2m), and herb layer(below 1m). According to the diameter distribution of tree species in Pinus densiflora community, secondary Pinus densiflora forest will gradually decline. Its forest may be replaced by Quercus mongolica, Quercus serrata, Carpinus laxiflora, C. cordata, and Fraxinus rhychophylla in the lower slope, and by Quercus mongolica in the middle slope. Pinus densiflora forest has its seedlings and saplings in ridge and top area, so it may be sustained. By taking cores from Pinus densiflora trees in research area, it could be obtained that in the lower and middle slope, age of Pinus densiflora forest was about 80~90 years old. When the age of its trees was about 72~80 years old, withering trees of standing dead occurred. Disturbance regime of Pinus densiflora community in Mt. Kaya consisted of standing dead, uprooting and limbfall, these were 70.6%, 17.6% and 11.8% respectively. It takes about 100~110 years for advance growth of Pinus densiflora in ridge and top area to reach tree layer. During the period, it has twice chances of disturbance in standing dead. Annual diameter growth of Pinus densiflora was 2.45~2.9mm in the lower and middle slope, while it was 1.75mm in ridge and top region, by measuring cores.

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Effect of Joint Orientation Distribution on Hydraulic Behavior of the 2-D DFN System (절리의 방향분포가 이차원 DFN 시스템의 수리적 특성에 미치는 영향)

  • Han, Jisu;Um, Jeong-Gi
    • Economic and Environmental Geology
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    • v.49 no.1
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    • pp.31-41
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    • 2016
  • A program code was developed to calculate block hydraulic conductivity of the 2-D DFN(discrete fracture network) system based on equivalent pipe network, and implemented to examine the effect of joint orientation distribution on the hydraulic characteristics of fractured rock masses through numerical experiments. A rock block of size $32m{\times}32m$ was used to generate the DFN systems using two joint sets with fixed input parameters of joint frequency and gamma distributed joint size, and various normal distributed joint trend. DFN blocks of size $20m{\times}20m$ were selected from center of the $32m{\times}32m$ blocks to avoid boundary effect. Twelve fluid flow directions were chosen every $30^{\circ}$ starting at $0^{\circ}$. The directional block conductivity including the theoretical block conductivity, principal conductivity tensor and average block conductivity were estimated for generated 180 2-D DFN blocks. The effect of joint orientation distribution on block hydraulic conductivity and chance for the equivalent continuum behavior of the 2-D DFN system were found to increase with the decrease of mean intersection angle of the two joint sets. The effect of variability of joint orientation on block hydraulic conductivity could not be ignored for the DFN having low intersection angle between two joint sets.

Molten-Salt-Assisted Chemical Vapor Deposition for Growth of Atomically Thin High-Quality MoS2 Monolayer (용융염 기반의 화학기상증착법을 이용한 원자층 두께의 고품질 MoS2 합성)

  • Ko, Jae Kwon;Yuk, Yeon Ji;Lim, Si Heon;Ju, Hyeon-Gyu;Kim, Hyun Ho
    • Journal of Adhesion and Interface
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    • v.22 no.2
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    • pp.57-62
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    • 2021
  • Recently, the atomically thin two-dimensional transition-metal dichalcogenides (TMDs) have received considerable attention for the application to next-generation semiconducting devices, owing to their remarkable properties including high carrier mobility. However, while a technique for growing graphene is well matured enough to achieve a wafer-scale single crystalline monolayer film, the large-area growth of high quality TMD monolayer is still a challenging issue for industrial application. In order to enlarge the size of single crystalline MoS2 monolayer, here, we systematically investigated the effect of process parameters in molten-salt-assisted chemical vapor deposition method. As a result, with optimized process parameters, we found that single crystalline monolayer MoS2 can be grown as large as 420 ㎛.

Enhanced Performance in a Lithium-ion Battery via the Crystal-aligned LiNi0.6Mn0.2Co0.2O2 and the Relevant Electrochemical Interpretation (결정배향 LiNi0.6Mn0.2Co0.2O2 전극활물질을 통한 리튬이차전지 성능 향상 및 이의 전기화학적 해석)

  • Cham, Kim
    • Journal of the Korean Chemical Society
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    • v.66 no.6
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    • pp.451-458
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    • 2022
  • Through the crystal alignment research based on the magnetic properties of LiNixMnyCo1-(x+y)O2 such as magnetic susceptibility and related anisotropy, a crystal aligned LiNi0.6Mn0.2Co0.2O2 electrode is obtained, in which the (00l) plane is frequently oriented perpendicular to the surface of a current collector. The crystal aligned LiNi0.6Mn0.2Co0.2O2 electrode steadily exhibits low electrode polarization properties during the charge/discharge process in a lithium-ion battery, thus affording an improved capacity compared to a pristine LiNi0.6Mn0.2Co0.2O2 electrode. The aligned LiNi0.6Mn0.2Co0.2O2 electrode may have an appropriate structural nature for fast lithium-ion transport due to the oriented (00l) plane, and thus it contributes to enhancing the battery performance. This enhancement is analyzed in terms of various electrochemical theories and experiment results; thus, it is verified to occur because of the considerably fast lithium-ion transport in the aligned LiNi0.6Mn0.2Co0.2O2 electrode.

Estimation of 3-D Hydraulic Conductivity Tensor for a Cretaceous Granitic Rock Mass: A Case Study of the Gyeongsang Basin, Korea (경상분지 백악기 화강암 암반에 대한 삼차원 수리전도텐서 추정사례)

  • Um, Jeong-Gi;Lee, Dahye
    • The Journal of Engineering Geology
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    • v.32 no.1
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    • pp.41-57
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    • 2022
  • A workflow is presented to estimate the size of a representative elementary volume and 3-D hydraulic conductivity tensor based on fluid flow analysis for a discrete fracture network (DFN). A case study is considered for a Cretaceous granitic rock mass at Gijang in Busan, Korea. The intensity and size of joints were calibrated using the first invariant of the fracture tensor for the 2-D DFN of the study area. Effective hydraulic apertures were obtained by analyzing the results of field packer tests. The representative elementary volume of the 2-D DFN was determined to be 20 m square by investigating the variations in the directional hydraulic conductivity for blocks of different sizes. The directional hydraulic conductivities calculated from the 2-D DFN exhibited strong anisotropy related to the hydraulic behavior of the study area. The 3-D hydraulic conductivity tensor for the fractured rock mass of the study area was estimated from the directional block conductivities of the 2-D DFN blocks generated for various directions in 3-D. The orientations of the principal components of the 3-D hydraulic conductivity tensor were found to be identical to those of delineated joint sets in the study area.

Numerical Simulations of Cellular Secondary Currents in Open-Channel Flows using Non-linear k-ε Model (비선형 k-ε 모형을 이용한 개수로 흐름에서의 격자형 이차흐름 구조 수치모의)

  • Kang, Hyeongsik;Choi, Sung-Uk;Park, Moonhyeong
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.28 no.6B
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    • pp.643-651
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    • 2008
  • In the present paper, turbulent open-channel flows over longitudinal bedforms are numerically simulated. The Reynolds- averaged Navier-Stokes equations in curvilinear coordinates are solved with the non-linear $k-{\varepsilon}$ model by Speziale( 1987). First, the developed model is applied to rectangular open channel flows for purposes of model validation and parameter sensitivity studies. It is found that the parameters $C_D$ and $C_E$ are important to the intensity of secondary currents and the level of turbulent anisotropy, respectively. It is found that the non-linear $k-{\varepsilon}$ model can hardly reproduce the turbulence anisotropy near the free surface. However, the overall pattern of the secondary currents by the present model is seen to coincide with measured data. Then, numerical simulations of turbulent flows over longitudinal bedforms are performed, and the simulated results are compared with the experimental data in the literature. The simulated secondary currents clearly show upflows and downflows over the ridges and troughs, respectively. The numerical results of secondary currents, streamwise mean velocity, and turbulence structures compare favorably with the measured data. However, it is observed that the secondary currents towards the troughs were significantly weak compared with the measured data.

식품 품질론 <하>

  • 장건형
    • Food Industry
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    • s.24
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    • pp.72-77
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    • 1975
  • 이상 식품의 품질에 관하여 논한바를 다음과 같이 요약하여본다. 가. 식품기업에서 자기가 생산판매한 품목을 결정하는것도 중요하지만 그 품목의 품질을 규정하는 것도 대단히 중요하다. 나. 식품의 품질은 절대적인 것이 아니고 상대적이여서 식품자체의 특성뿐만 아니라 소비자에 따라서 여러가지의 요소가 좌우된다. 다. 식품의 품질요소중에서 가장 중요한 것은 소비자의 기호를 만족시켜주는 색, 맛, 향미, 텍스츄아등의 관능적특성이며 이화학적특성은 관능적특성을 위한 이차적인 요소라고 할수있다. 라. 따라서 품질의 이화학적 분석결과에서 너무 의존하지 말고 항상 관능적인 평가를 병합하여야 할것이다. 마. 최근 과학적으로 발전하여 체계화되고 선진국의 식품업계에서 많이 활용되고 있는 식품의 관능검사방법을 우리나라에서도 도입하여 품질향상에 기여하여야 할 것이다.

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탄소를 도입한 산화타이타늄의 합성과 촉매 활성 연구

  • Kim, Yeong-Yong;Gwon, Gi-Yeong
    • Proceedings of the Korean Vacuum Society Conference
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    • 2016.02a
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    • pp.163.2-163.2
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    • 2016
  • 타이타늄과 탄소의 비율이 서로 다른 조건에서, 탄소가 도입된 산화타이타늄 (TiO2)을 수열합성법을 이용하여 합성하였다. TEM 이미지를 통하여 일정한 형태의 산화타이타늄이 합성된 것과, XRD 패턴 분석을 통하여 Anatase 형태임을 확인하였다. 본 연구에서는 탄소가 도입된 산화타이타늄을 이종상촉매로 사용하여 일차 및 이차 알코올 산화반응과 메틸렌 블루 분해 실험에 응용하였다.

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Evolution and Sediment Facies of the Namdaecheon Spit, Yang-Yan Coast East Sea of korea (강원도 동해안 양양읍 남대천 하고 Spit Beach에 관한 연구)

  • 박용안
    • The Korean Journal of Quaternary Research
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    • v.12 no.1
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    • pp.1-8
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    • 1998
  • 동해안의 강원도 양양읍 남대천 하구에 발달한 spit beach의 지형적변화(1979∼ 1996) 는 outlet의 위치변화와 해안선 모습의 변화로 규명되었는바 일차적인 변화는 해안에 평행한 spit의 성장이며 이차적인 변화는 spit폭의 변화(overwash across sedimentation)라 고 밝혀졌다. 해빈환경의 소환경(subenvironment)으로서 swash zone과 berm crest는 각각 의 특징적 퇴적상(조직매개변수)으로 구분되는바 이에 관한 분석결과가 기술되었다.