• 자원환경지질
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• 제33권5호
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• pp.391-404
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• 2000

This study investigated the geochemical characteristics of mine drainage discharged from an abandoned coal mine in the Hwasoon area. Surface water samples were collected from 23 locations along the Hancheon creek. The concentration of Zn and Cu in stream waters was highest at low pH (3.53), whereas the content of TDS and TDI was highest at high pH (7.78) due to the concentration of Ca, $HCO_3$ and $SO_4$. At the upstream site, the Ba, Fe, Mn, Zn, and $SO_4$ contents were relatively high but decreased significantly with the distance from the coal mine. On the contrary, the Na and $NO_3$ contents were low at the upstream site but increased downstream. Yellow precipitate material collected in the Hancheon consisted mainly of iron and LOI. This yellow precipitate was heated from 100 to $900^{\circ}C$ for 1 hour. With increasing temperature, the intensity of hematite peaks were sharply produced in X-ray pattern and the absorption band Fe-O of hematite increased in IR due to dehydration and melting. The yellow to brown precipitate and evaporite materials were collected by a air-dry from the acid mine water at the laboratory. After drying, the concentration of ions in the acid water samples increased progressively in oversaturation with respect to either gypsum, ferrohexahydrite or quenstedetite. The X-ray powder diffraction studies identified that the precipitated and evaporated materials after drying were well crystallized gypsum, ferrohexahydrite and quenstedetite. Diagnostic peaks used for identification of gypsum were the 7.65, 4.28, 3.03, 2.87 and 2.48$\AA$ peaks and those for ferrohexahydrite were the 5.46, 5.12, 4.89, 4.44, 4.05, 3.62, 3.46, 3.40, 3.20, 3.03, 2.94, 2.53, 2.28, 2.07, 1.88 and 1.86${\AA} peaks. The IR spectra with OH-stretching, deformation of $H_2O$and ${SO_4}^{2-}$stretching vibration include the existence of gypsum, ferrohexahydrite and quenstedetite in the precipitated and evaporite materials. In the SEM and EDS analysis for the evaporite material, gypsum with well-crystallized, acicular, and columnar form was distinctly observed.

• 한국자기학회지
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• 제7권1호
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• pp.13-18
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• 1997

기본 조성 N $i_{0.18}$Z $n_{0.68}$C $u_{0.14}$F $e_{2}$ $O_{4}$와 N $i_{0.14}$Z $n_{0.64}$C $u_{0.22}$F $e_{2}$ $O_{4}$ 및 N $i_{0.24}$Z $n_{0.64}$C $u_{0.12}$F $e_{2}$ $O_{4}$에 입계의 고저항층을 형성하고 소결을 촉진시키기 위해서 0.1 mol %의 Ca $Co_{3}$와 입자의 성장을 촉진시키고 높은 투자율을 얻을 목적으로 $V_{2}$ $O_{5}$를 0.04 mol% 첨가하였다. 이들 원료들을 혼합한 후 950 .deg. C에서 3시간 하소 과정을 거친후 ball mill해서 toroid 시편을 만들고 1030 .deg. C, 1050 .deg. C 및 1070 .deg. C 에서 2시간 동안 공기중에서 소결 시켰다. Raw material의 조성비 변화 및 소결 온도 변화에 따른 여러 가지 물리적 특성들을 조사하였다. X-선 회절 분석 결과 이들 시편들이 spinel 구조를 이루고 있음을 확인하였고 금속현미경으로 측정한 결정 입자의 크기는 6 .mu. m ~ 16 .mu. m 이었다. 초투자율, 자기 유도는 소결 온도가 1030 .deg. C에서 1050 .deg. C로 증가함에 따라 증가하였고 Q factor와 보자력은 감소하였다. 보자력과 큐리온도는 각각 0.17 Oe 및 220 .deg. C 근처로 모든 시편들에서 거의 비슷하였다. 본 시편의 사용 주파수 범위는 0.4 ~ 20 MHz로 확인되었으며, 소결 온도 1050 .deg.C와 기본 조성 N $i_{0.14}$Z $n_{0.64}$C $u_{0.22}$F $e_{2}$ $O_{4}$ 에서 다른 사람들 보다 더욱 더 우수한 자기유도값(B, $B_{m}$ )을 얻을 수 있었다.

• 한국균학회지
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• 제14권2호
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• pp.101-107
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• 1986

The properties of carboxyl proteinase which was contained in Poria cocos (Schw.) Wolf were investigated by means of the purification with 0.65 ammonium sulfate saturation, DEAE cellulose and Sephadex G-75 gel filtration. This enzyme was found to hydrolyze only peptide bond between glutamyl-L-tyrosine of carbobenzoxy-L-glutamyl-L-tyrosine among the synthetic substrates of carbobenzoxy-L-glutamyl-L-tyrosine, hippuryl- L-phenylalanine and hippuryl-L-arginine. This enzyme was inhibited by $Zn^{+2},\;Fe^{+2},\;Ca^{+2},\;CN^{-1},\;P_2O_7^{-4}$ ions, but stimulated by $Hg^{+2}$ ion. Also, this enzyme was inhibited by organic compounds such as L-lysine, L-phenylalanine, hippuryl-L-phenylalanine, diazoacetyl-DL-norleucine methyl ester (DAN) and 1,2-epoxy-3-(P-nitrophenoxy)propane(EPNP). In particular, the activity was inhibited by L-lysine till 20 minutes of preincubation time rapidly, and by DAN in the presence of $Cu^{+2}$ ion more rapidly after 30 minutes than DAN in the absence of $Cu^{+2}$ ion. L-Lysine was found to be a competitive inhibitor and its $K_i$ value was determined to be 0.12 mmole by Dixon plot.

• 자원환경지질
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• 제46권2호
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• pp.179-198
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• 2013

신장 위구르 자치구 바이청현 보즈구얼 지역의 A형 화강암체는 타림지대의 북쪽 끝과 동서쪽 방향의 알칼리 관입암대에 접하여 위치해 있다. 이 화강암체는 추휘석(aegrine)이나 아페소나이트(arfvedsonite)-석영-알칼리장석 섬장암, 또는 아페소나이트-알칼리장석 화강암, 흑운모-알칼리장석 섬장암으로 구성되며, 주요광물로는 알바이트(albite), K-장석, 석영, 아페소나이트(arfvedsonite), 추휘석, 시데로필라이트(siderophyllite) 등이 있으며 부성분 광물로는 지르콘(zircon), 파이로클로르(pyrochlore), 토라이트(thorite), 형석, 모나자이트(monazite), 바스네사이트(bastnaesite), 제노타임(xenotime), 아스트로필라이트(astrophyllite) 등이 있다. 이 알칼리 화강암체는 67.32%의 평균값을 갖는 $SiO_2$를 포함하고 평균 11.14%의 높은 $Na_2O+K_2O$(9.85~11.87%) 조성을 보이며 이 중 $K_2O$는 평균 4.73%의 조성을 보인다. $K_2O/Na_2O$의 비는 0.31~0.96 사이이며 $Al_2O_3$는12.58%부터 15.44%사이로 포함되고 총 $FeO^T$함량은 2.35~5.65%이내이다. CaO, MgO, MnO, $TiO_2$의 함량은 낮은 것으로 관찰된다. 희토류원소의 총량은 평균 $77{\times}10^{-6}$으로 비교적 높게 나타나고 경희토원소는 농축되어 있지만 중희토원소는 Eu원소의 부(-)의 이상과 함께 상대적으로 결핍되는 특징을 가진다. 또한 알칼리 화강암체의 chondrite-normalized 희토류원소의 패턴은 오른쪽으로 기울어진 갈매기형태를 보인다. Zr는 평균 $594{\times}10^{-6}$의 함량을 보이며 Zr+Nb+Ce+Y는 평균 $1362{\times}10^{-6}$의 함량을 나타낸다. 또한 이 알칼리 화강암체는 높은 HFSE(Ga, Nb, Ta, Zr, Hf)함량과 낮은 LILE(Ba, K, Sr)함량을 보인다. Nb/Ta의 비는 평균 16.5이며 Zr/Hf의 비는 평균 36.80이다. 지르콘은 경희토원소에서 결핍되고 중희토원소에서 농축되어있다. 지르콘의 chondrite-normalized 희토류원소는 Eu원소의 강한 부(-)의 이상과 함께 왼쪽으로 기울어진 갈매기형태를 보인다. 보즈구얼지역의 A타입 화강암체는 A1타입의 화강암과 유사한 특징을 나타낸다. 화강암질 마그마의 평균온도는 $832{\sim}839^{\circ}C$이며 보즈구얼 지역의 A타입 화강암체는 지각과 맨틀의 혼합양상을 보이며 고온, 무수, 낮은 산소의 퓨개시티(fugacity) 환경을 가진 판 내부의 비조산대에서 생성되었을 가능성이 있다.

• 자원환경지질
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• 제30권1호
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• pp.35-49
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• 1997

The coal formation of the Deokpyeong area are interbedded along metapelites of the Ogcheon Supergroup, which are composed mainly of graphite, quartz, muscovite and associated with small amounts of biotite, chlorite, pyrite and barite. The ratios of $SiO_2/Al_2O_3$, $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ of the coaly metapelite are variable and wide range from 1.80 to 10.21, from 27.8 to 388.8 and from 7.6 to 61.8, respectively. These coal formation were deposited in basin of marine environments, and the REE of these rocks are not influenced with metamorphism and hydrothermal alterations on the basis of $Al_2O_3$ versus La, La against Ce, the ratios of La/Ce (0.19 to 0.99) and Th/U (0.02 to 4.75). These rocks also show much variation in $La_N/Yb_N$ (1.19 to 22.89), Th/Yb (0.14 to 21.43) and La/Th (0.44 to 13.67), and their origin is explained by derivation from a mixture of sedimentary and igneous rocks. The wide range in trace and REE element characteristics as Co/Th (0.12 to 2.78), La/Sc (0.33 to 10.18), Sc/Th (0.57 to 5.73), V/Ni (8 to 2347), Cr/V (0.02 to 0.67) and Ni/Co (1.56 to 32.95) of these coaly metapelites argues for inefficient mixing of the various source lithologies during sedimentation. Deep to pale green barium-vanadium muscovites (vanadium-oellacherite) have been found in this coal formations. Modes of occurrence and grain size of muscovite are heterogeneous, but most of the barium and vanadium-bearing muscovites occur along the boundaries between graphite and quartz grains, ranging from 200 to $350{\mu}m$ in length and from 40 to $60{\mu}m$ in width. Results of X-ray diffraction data of the minerals characterized to be monoclinic system with $a=5.249{\AA}$, $b=8.939{\AA}$, $c=20.924{\AA}$ and ${\beta}=95.894^{\circ}$. Representative chemical formula of the muscovite was $(Na_{0.09}K_{1.44}Ba_{0.46})(Al_{2.75}Ti_{0.07}V_{0.56}Fe_{0.08}Mg_{0.50})(Si_{6.12}Al_{1.88})O_{22}$. The V possibly substitute octahedral Al, and the Ba is coupled substitution of $K^+Si^{4+}=Ba^{2+}Na^+Ca^{2+}$, which compositional ranges of V and Ba are from 0.42 to 0.69 and from 0.34 to 0.56 based on $O_{22}$, respectively. Formation mechanism of the barium-vanadium muscovites in the coaly metapelite is shown that the formed by high pressure and temperature from regional metamorphism origanated during diagenesis at the interface between a basinal brine and organic matter.

• Ocean and Polar Research
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• 제36권4호
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• pp.407-421
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• 2014

The benthic environmental impact experiment addresses environmental impacts at a specific site related to deep-sea mineral resource development. We have acquired several tens of multi- or box core samples at 31 sites within the Benthic environmental Impact Site (BIS) since 2010, aiming to examine the basic properties of surficial deep-sea sediment as a potential source for deep-water plumes. In this study, we present the geochemical properties such as major elements, rare earth elements (REEs), and heavy metal contents at the BIS. Such proxies vary distinctly according to the Facies association. The lithology of all core sediments in the BIS corresponds to both Association Ib and Association IIIb. The vertical profiles of some major elements ($SiO_2$, $Fe_2O_3$, CaO, $P_2O_5$, MgO, MnO) show noticeable differences between Association Ib and IIIb, while others ($Al_2O_3$, $TiO_2$, $Na_2O$, and $K_2O$) do not vary between Association Ib and IIIb. REEs are also distinctly different for Associations Ib and IIIb; in Association Ib, REY and HREE/LREE are uniform through the sediment section, while they increase downward in Association IIIb like the major elements; below a depth of 8 cm, REY is over 500 ppm. The metal enrichment factor (EF) evaluates the anthropogenic influences of some metals (Cu, Ni, Pb, Zn, and Cd) in marine sediments. In both Associations, the EF for Cu is over 1.5, the EF for Ni and Pb ranges from 0.5 to 1.5, and the EF for Zn and Cd are less than 0.5, indicating Cu is enriched but Zn and Cd are relatively depleted in the BIS. The vertical variations of geochemical properties between Association Ib and IIIb are shown to be clearly different, which seems to be related to the global climate changes such as the shift of Intertropical convergence zone (ITCZ).

• 한국식물병리학회지
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• 제13권1호
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• pp.46-56
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• 1997

Based on the principal component analysis (PCA) of Richards' parameter estimates, ginseng field soils were grouped as the principal component 1 (PC1) and the principal component 2 (PC2). The microflora and physico-chemical characteristics of each soil group were compared to elucidate soil environmental factors affecting the disease development of root rot of ginseng seedling. Among 3 soil groups by PC1, there were differences in the populations of total fungi (TF) and Cylindrocarpon plus Fusarium (C+F), and the population ratio of Cylindrocarpon plus Fusarium to total fungi or total bacteria (C+F/TF, C+F/TB) in rhizoplane of ginseng seedlings, the population of total actinomycetes (TA) and the population ratio of total Fusarium to total actinomycetes (Fus/TA) in soil, and soil chemical properties (EC, NO3-N, K, Mn, ect.). Among 4 soil groups by PC2, there were differences in TF, C+F, TB, C+F/TF and C+F/TB in the rhizoplane, Trichoderma plus Gliocladium (T+G) in soil, and P2O5 content in soil. Especially, EC, NO3-N, K, K/Mg and Mn were positively correlated to PC1, and TA was negatively to PC1; however, TF, C+F, TB, C+F/TF and C+F/TB in the rhizoplane were significantly correlated to PC2 positively. On the other hand, microbes in the rhizoplane were not significantly correlated to the stand-missing rate (SMR), although TA and Fe/Mn were negatively correlated, and pH and Ca were positively correlated to SMR.

• Current Research on Agriculture and Life Sciences
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• 제4권
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• pp.55-64
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• 1986

배과실(果實)의 PPO를 분리(分離) 정제(精製)한 후(後) 그 특성(特性)을 조사(調査)한 결과(結果)는 다음과 같다. 조효소액(粗酵素液)을 전기영동한 결과 2개의 활성분리대(活性分離帶)가 관찰(觀察)되었으며, 이 조효소액(粗酵素液)을 acetone 심몰(沈沒)과 DEAE-cellulose chromatography로 부분정제(部分精製)한 결과 PPO A 분획(分劃)과 PPO B 분획(分劃)을 얻었다. 각 구분을 전기영동(電氣泳動)한 결과 PPO A, B 각각 Rm치가 0.58, 0.68인 단일 활성분리대(活性分離帶)가 관찰(觀察)되었다. PPO A와 PPO B의 최종 정제도(精製度)는 각각 7.8와 8.7배(倍)였다. PPO A의 최적(最適) pH와 온도(溫度)는 pH 7, $33^{\circ}C$인 반면 PPO B의 최적(最適) pH와 온도(溫度)는 pH 4.2, $30^{\circ}C$로 나타났다. PPO A, B의 열(熱) 안정성(安定性)은 $60^{\circ}C$ 이상(以上)의 온도(溫度)에서는 급격히 활성(活性)이 감소했으며 PPO B보다 PPO A가 더 안전(安定)하였다. 배의 두 PPO는 o-diphenol에 강한 활성을 나타냈으며 특히 PPO A는 catechol에 PPO B는 chlorogenic acid에 활성이 강했다. 또한 PPO A는 pyrogallol에도 활성을 나타냈다. 그러나 두 PPO는 m-diphenol, p-diphenol과 monophenol에는 활성(活性)을 나타내지 않았다. 무기염(無機鹽)의 영향(影響)을 본 결과(結果)는 10mM농도(濃度)에서 $Zn^{{+}{+}}$은 PPO A의 활성(活性)을 증가(增加)시켰으나 $Fe^{{+}{+}}$는 저해(沮害)했고 반면 $Fe^{{+}{+}}$, $Zn^{{+}{+}}$는 PPO B는 활성(活性)을 증가(增加)시켰으나 $K^+$, $Mg^{{+}{+}}$, $Ca^{{+}{+}}$, $Hg^{{+}{+}}$는 저해(沮害)했다. $Cu^{{+}{+}}$는 저농도(低濃度)에서는 효소(酵素)를 활성화(活性化)시켰으나 10mM의 고농도(高濃度)에서는 저해작용(沮害作用)을 했다. 저해제(沮害劑)의 작용(作用)을 조사(調査)한 결과(結果), L-ascorbic acid, L-cysteine, thiourea 등이 저해작용(沮害作用)이 강했다. PPO A와 PPO B의 catechol에 대한 Km치는 각각 20mM과 14.3mM이었다.

• 한국재료학회:학술대회논문집
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• 한국재료학회 2011년도 춘계학술발표대회
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• pp.53.2-53.2
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• 2011

Ti metal has superior mechanical properties along with biocompatibility, but it still has the problem of bio-inertness thus forming weaker bond in bone/implant interface and long term clinical performance as orthopaedic and dental devices are restricted for stress shielding effect. On the other hand, despite the excellent biodegradable behavior as being an integral constituent of the natural bone, the mechanical properties of ${\beta}$-tricalcium phosphate $(Ca_3(PO_4)_2;\;{\beta}-TCP)$ ceramics are not reliable enough for post operative load bearing application in human hard tissue defect site. One reasonable approach would be to mediate the features of the two by making a composite. In this study, ${\beta}$-TCP/Ti ceramic-metal composites were fabricated by spark plasma sintering in inert atmosphere to inhibit the formation of $TiO_2$. Composites of 30 vol%, 50 vol% and 70 vol% ${\beta}$-TCP with Ti were fabricated. Detailed microstructural and phase characteristics were investigated by FE-SEM, EDS and XRD. Material properties like relative density, hardness, compressive strength, elastic modulus etc. were characterized. Cell viability and biocompatibility were investigated using the MTT assay and by examining cell proliferation behavior.

• 한국환경보건학회지
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• 제49권5호
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• pp.251-261
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• 2023

Background: This paper deals with the study of natural radioactivity in rocks from Ogun State in Southwestern Nigeria. The aim is to determine radiation emissions from rocks in order to estimate radiation hazard indices. Objectives: The following objectives were targeted: 1. To determine radiation emissions from each type of rocks; 2. To estimate radiation hazard indices based on the rocks; 3. To correlate the activity concentrations of radionuclides with major oxides. Methods: The samples were analyzed using a NaI (Tl) gamma ray spectrometric detector and PerkinElmer AAnalyst 400 AAS spectrometer. Results: The activity of ⁴⁰K, ²²⁶Ra, and ²³²Th were found in order of decreasing magnitude from pegmatite>granite>migmatite. In contrast, lower concentrations were found in shale, phosphate, clay stone, sandstone and limestone. The mean absorbed doses were 125±23 nGyh^-1 (migmatite), 74±13 nGy/h (granite), 72±13 nGyh^-1 (pegmatite), 64±09 nGyh^-1 (quartzite), 45±16 nGyh^-1 (shale), 41±09 nGyh^-1 (limestone), 41±11 nGyh^-1 (clay stone), 24±03 nGyh^-1 (phosphate), and 21±10 nGyh^-1 (sandstone). The outdoor effective dose rates in all rock samples were slightly higher than the world average dose value of 0.34 mSvy^-1. The percentage composition of SiO₂ in the rock samples was above 50 wt% except for in the limestone, shale and phosphate. Al₂O₃ ranged from 4.10~21.24 wt%, Fe₂O₃ from 0.39~7.5 wt%, and CaO from 0.09-46.6 wt%. In addition, Na₂O and K₂O were present in at least 5 wt%. Other major oxides, including TiO₂, P₂O₅, K₂O, MnO, MgO and Na₂O were depleted. Conclusions: The findings suggest that Ogun State may be described as a region with elevated background radiation. It is recommended that houses should be constructed with good cross ventilation and residences should use home radiation monitoring instruments to monitor radon emanating from walls.