• 한국환경농학회지
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• 제23권2호
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• pp.92-98
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• 2004

본 연구에서는 생물흡착제인 미역을 사용하여 인공폐액내의 중금속의 흡착 특성을 조사하였으며, 다음과 같은 결론을 얻었다. 미역 폐기물을 이용하여 제조된 생물흡착제의 단일 중금속 흡착효율은 각 중금속 100 mg/L인 용액에 biosorbent 3g을 처리했을 때 Pb는 거의 100%였고, Cu와 Cd가 약 $85{\sim}86%$, Zn과 Cr은 약 $60{\sim}64%$, Co와 Ni은 약 57%, Mn은 약 48%였다. 복합중금속 흡착효율은 단일중금속 흡착효율에 비하여 Pb를 제외한 다른 중금속들은 크게 감소되었으나 biosorbent g당 전체 중금속 흡착량은 더 증가되었다. 온도, pH에 따른 중금속 흡착효율은 별 차이가 없었으며 전반적으로 pH는 pH $5{\sim}6$ 범위, 온도는 $20{\sim}30^{\circ}C$ 범위의 실온이 적당한 것으로 나타났다. 생물흡착제의 흡착평형은 모든 중금속이 1시간 이내에 이루어졌다. Freundlich과 Langmuir 등온흡착식을 구하여 실제폐수처리에 적용여부를 검토한 결과 Pb, Cu, Cr, Cd, Co 순으로 비교적 친화도가 큰 것으로 나타났고, Freundlich 등온 흡착식에 가장 잘 일치하였다. 모든 중금속의 Freundlich 지수 1/n값이 $0.1{\sim}0.5$ 범위에 포함되어 흡착이 용이하고, Pb, Cr, Cu, Cd 순으로 비교적 평형 흡착량이 큰 것으로 나타났으며, 이 결과는 Langmuir 흡착등온식의 결과와 거의 유사하였다. 따라서, 중금속 농도범위에 따른 한계범위를 설정하여 등온흡착식을 적용시키면 매우 높은 중금속 처리효율을 나타낼 것으로 판단된다. 생물흡착제가 중금속 흡착 후의 구조적인 특성을 조사하기 위하여 FT-IR분석 결과, 중금속 이온과 치환될 것으로 생각되는 functional group을 확인할 수 있었으며, 3,400/cm에서의 -OH group, 1,648/cm에서의 C=O bond,1,426/cm에서의 C-O bond그리고 850/cm에서의 S=O등이 전반적으로 중금속 흡착 후에 peak가 커지는 것이 관찰되었다. 생물흡착제의 재사용 가능성을 검토하기 위하여 최적의 중금속 탈착조건 검토하였는데, 탈착제 종류에 따른 중금속 탈착효율은 탈착제 종류와 중금속 종류에 따라 차이가 있었고, 전반적으로 NTA>$H_2SO_4$>HCl>EDTA 순으로 우수하였으며, 전체적으로 특정 중금속의 탈착효율이 떨어지지 않는 NTA가 탈착제로 가장 적합하였다. NTA농도에 따른 중금속 탈착효율은 NTA $0.1{\sim}0.3%$ 농도범위에서는 농도 증가에 따라 탈착 효율도 약간 증가되었으나 그 이상의 농도에서는 별 차이 없었다. 온도와 pH 변화에 따른 중금속 탈착효율은 Cr을 제외한 다른 중금속들은 크게 영향을 받지 않는 것으로 나타났으며 전반적으로 온도는 $30^{\circ}C$, pH는 2에서 높았다. 탈착제 접촉 반응시간에 따른 탈착효율은 10분 이내에 전체 탈착량의 80%이상이 탈착 되었으며 1시간 이후에는 거의 변화가 없었다.

• The Korean Journal of Ceramics
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• 제1권4호
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• pp.191-196
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• 1995

Using sol-gel processing method, thin films of lathanum modified lead titanate(PLT) on Corning 7059 glass were prepared. A differential thermal analysis (DTA/TG) curve of gel powder and infrared spectra (FT-IR) of the films were measured to estimate residual organices in them. The heat-treated films were characterized by X-ray diffraction(XRD). Microstructures of the films were observed by a scanning electron microscope (SEM). Optical properties of the films were determined by a UV-VIS spectrophotometer. The waveguiding properties and optical attenuation were measured with the end coupling method and the cut back method. Effects of the drying conditions on the transmittance and the propagation loss of the films were investigated. Experimemtal results showed that the content of residual organics in the film decreased as the drying temperature of the film increased. As the La content of the film increased, the grain size decreased and the transmittance increased. The transmittances of the films increased with the increasing of the drying temperature. The propagation losses in the film decreased as the drying temperature increased.

• 자원환경지질
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• 제31권4호
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• pp.277-290
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• 1998

The purpose of this research is to investigate the dispersion pattern of gold during skarnization and genesis of gold mineralization in the Sangdong skarn deposits. The Sangdong scheelite orebodies are embedded in the Cambrian Pungchon Limestone and limestone interbedded in the Myobong Slate of the Cambrian age. The tungsten deposits are classified as the Hangingwall Orebody, the Main Orebody and the Footwall Orebody as their stratigraphic locations. Recently, the Sangdong granite of the Cretaceous age (85 Ma) were found by underground exploratory drillings below the orebodies. In geochemisty, the W, Mo, Bi and F concentrations in the granite are significantly higher than those in the Cretaceous granitoids in southern Korea. Highest gold contents are associated with quartz-hornblende skarn in the Main Orebody and pyroxene-hornblende skarn in the Hangingwall Orebody. Also Au contents are closely related to Bi contents. This could be inferred that Au skarns formed from solutions under reduced environment at a temperature of $270^{\circ}C$. According to the multiple regression analysis, the variation of Au contents in the Main Orebody can be explained (87.5%) by Ag, As, Bi, Sb, Pb, Cu. Judging from the mineralogical, chemical and isotope studies, the genetic model of the deposits can be suggested as follows. The primitive Sangdong magma was enriched in W, Mo, Au, Bi and volatiles (metal-carriers such as $H_2O$, $CO_2$ and F). During the upward movement of hydrothermal ore solution, the temperature was decreased, and W deposits were formed at limestone (in the Myobong Slate and Pungchon Limestone). In addition, meteoric water influx gave rise to the retrogressive alterations and maximum solubility of gold, and consequently higher grade of Au mineralization was deposited.

• 한국초전도ㆍ저온공학회논문지
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• 제14권3호
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• pp.1-4
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• 2012

Effects of artificial holes on the cooling efficiency of single grain YBCO bulk superconductors were studied. Single grain YBCO bulk superconductors without artificial holes, with six 2.4 mm holes and six holes filled with Bi-Pb-Cd-Sn metal solder were fabricated by a top-seeded melt growth process for powder compacts with/without holes. Simulation for the cooling rate to a liquid nitrogen temperature (77 K) of YBCO samples was carried out using a finite element method (FEM) and the results are compared with the actual cooling rates of samples in liquid nitrogen. The simulated cooling times for the YBCO sample without holes, with six holes and with six holes filled with the metal solder were 80, 47 and 75 sec. respectively, which are similar to the actual cooling times of 84, 52 and 78 sec. estimated for the same samples cooled in liquid nitrogen. The shorter cooling time of the sample with artificial holes are attributed to the increased surface areas associated with the presence of artificial holes. The metal filling into the holes did not give any remarkable effect on the cooling efficiency.

• Journal of Plant Biology
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• 제19권1호
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• pp.1-6
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• 1976

This study was carried out to investigate the formation of precipitates between lead ion and the essential anions of plants, the effects of lead concentration on seed germination and plant growth in water and soil culture, and the germinating and growing recovery of inhibited seed germination and plant growth by lead. Four kinds of the seeds (Glycine max M., Triticum vulgare V., Setaria viridis (L) P. De Beauvois, and Digitoria sanguinalis (L) Scopoli var) were germinated and growth in water and soil culture included the different concentrations of lead for five days. The seeds and plants inhibited germination and growth by lead were transferred to lead free Hoagland solution and the growing recovery was observed. The precipitates of lead ion were observed in the solution of both acidity and alkalinity included each anion of $H_2PO_4^-, HPO_4^{2-}, PO_4^{3-}, SO_4^{2-} and MoO_4^{2-}$ in a room temperature, whereas the precipitates between lead ion and other anions were observed largely in the solution of alkalinity, so that it seemed that lead could be remained in the state of non-soluble in plant and soil. The inhibition of germination and growth in the water culture was observed in 100ppm of lead, whereas the inhibition in the case of the soil culture was observed in 10000ppm of lead. The difference of the effected concentration between water and soil culture in germination and the growth was 100 times. When the seed and plant inhibited the growth in 5000ppm or 10000ppm of lead for five days were transferred to lead free Hoagland solution, the recovery of germination and growth was observed in three days. This growing recovery was different according to the kinds of plant and concentrations of lead. It seemed that plant growth could be inhibited by the inhibition of the metabolism concerned with the precipitates between lead iion and other anions.

• 자원환경지질
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• 제23권4호
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• pp.369-381
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• 1990

우리나라에서 중요한 금속광상인 상동 중석, 연화 연-아연, 거도의 동-철 광상은 모두 태백분지내 함백향사 남익부에 위치하고 있다. 이들 광화작용은 대체로 동서 주향에 25-30도 북향한 경사로 놓여진 캠브리아기의 묘봉층내 석회암 협층과 풍촌 석회암에서 일어났다. 함백향사의 북익부에는 동일한 지질내에 동일형의 광상이 노출되어 있지 않아, 이 지역에서의 잠두광체를 찾기위한 수단으로 알려진 상동광산 지역에서 암석지화학적, 특별히 Si, Ca, Fe 및 탄소 안정동위원소를 이용한 탐사연구를 시도하였다. 광화대와 비광화대의 석회암 사이의 CaO와 $AL_2O_3$ 함량은 큰 차이를 보이고, 탄소동위 원소 분석결과 역시 ${\delta}^{13}C$ 값이 광화대에서 더 낮은 값을 보이는 바 그 내용은 아래와 같다. 비광화대 광화대 CaO 51.3% 43.5% $Al_2O_3$ 0.6% 2.4% ${\delta}^{13}C$ -0.39 permil -0.56 permil $Fe_2O_3$ 0.9% 1.4% $SiO_2$ 3.0% 2.4% 광화대내의 풍촌석회암의 Si 함량이 감소한 것은 앞선 연구(Moon. 1987) 결과와 상치되는 바, 광화대내의 석회암중 Al 함량이 증가한 사실을 확인한 사실을 근거로 생각해 볼때, Si의 감소는 열극, 균열, 또는 소규모의 단층올 따라 주로 발달된 변질물의 증가에 따른 결과로 유추되기도 한다. 따라서 광화대내의 Si 와 Al 함량이 보여주는 현상은 화강암류로부터 전달된 열의 영향으로부터 기인된 것으로 상위 지표부의 석회암에 이로부터 광화활동이 이어진 것으로 여겨진다. 만약 함백향사의 북익부에서 풍촌석회암의 Fe, Al의 함량이 평균 함량치 보다 높을 뿐만 아니라, Ca와 Si는 낮고 Ca 함량과 ${\delta}^{13}C$의 값이 평균치보다 낮은 값을 보이는 경우는 잠두광체 탐사에 이용될 가치가 있다고 본다.

• 한국터널지하공간학회 논문집
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• 제9권4호
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• pp.403-413
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• 2007

터널과 같은 지하공간 구조물에 있어서 록볼트는 숏크리트와 함께 주요 지보재 중의 하나이며, 그러므로 록볼트 시공품질 정도에 따라 이러한 지중구조물의 안정성에 큰 영향을 미치게 된다. 본 연구의 목적은 록볼트를 따라 전파되는 유도파에 대하여 푸리에 및 웨이브렛 변환을 이용하여 록볼트의 건전도를 평가하는데 있다. 각기 다른 결함비율을 가진 다섯 개의 록볼트 시험체를 제작하여 콘크리트 블록에 매설한 후, PZT($Pb[Zr_xTi_{1-x}]O_3$: lead zirconate titanate) 엘리먼트로 유도파를 발생시키고 AE(acoustic emission) 센서를 이용하여 신호를 측정하였다. 수집된 신호는 푸리에 변환을 이용하여 주파수 영역에서 분석하였고, 가버 웨이브렛을 사용한 웨이브렛 변환을 이용하여 시간-주파수영역에서 분석하였다. 푸리에 변환을 이용하여 얻은 스펙트럼을 분석하면 록볼트의 결함비율이 증가함에 따라 고주파 대역 에너지의 비율이 증가하는 것을 알 수 있다. 또한, 시간-주파수 영역에서의 각 파군별 최대 에너지가 나타나는 지점의 시간차는 각 반사파군 간의 이동 시간차를 나타내며, 이를 통해 계산된 유도파의 에너지 속도는 록볼트의 공동결함비율이 증가함에 따라 증가하는 것으로 나타났다. 본 연구는 스펙트럼 비와 에너지 속도가 록볼트의 건전도 평가에 있어서 하나의 지표가 될 수 있음을 보여준다.

• 자원환경지질
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• 제15권3호
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• pp.123-154
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• 1982

Petrochemical, K-Ar dating, Sand Rb/Sr isotopes, metallogenic zoning, paleomagnetic and geotectonic studies of the Gyongsang basin were carried out to examine applicability of plate tectonics to the post-late Cretaceous igneous activity and metallogeny in the southeastern part of Korean Peninsula. The results obtained are as follows: 1. Bulgugsa granitic rocks range from granite to adamellite, whose Q-Ab-Or triangular diagram indicates that the depth and pressure at which the magma consolidated increase from coast to inland varying from 6 km, 0.5-3.3 kb in the coastal area to 17 km, 0.5-10 kb in the inland area. 2. The volcanic rocks in Gyongsang basin range from andesitic to basaltic rocks, and the basaltic rocks are generally tholeiitic in the coastal area and alkali basalt in the inland area. 3. The volcanic rocks of the area have the initial ratio of Sr^{87}/Sr^{86} varying from 0.706 to 0.707 which suggests a continental origin; the ratio of Rb/Sr changing from 0.079-0.157 in the coastal area to 0.021-0.034 in the inland area suggests that the volcanism is getting younger toward coastal side, which may indicate a retreat in stage of differentiation if they were derived from a same magma. The K_2O/SiO_2 (60%) increases from about 1.0 in the coastal area to about 3.0 in the inland area, which may suggest an increase indepth of the Benioff zone, if existed, toward inland side. 4. The K-Ar ages of volcanic rocks were measured to be 79.4 m.y. near Daegu, and 61.7 m.y. near Busan indicating a southeastward decrease in age. The ages of plutonic rocks also decrease toward the same direction with 73 m.y. near Daegu, and 58 m.y. near Busan, so that the volcanism predated the plutonism by 6 m.y. in the continental interior and 4 m.y. along the coast. Such igneous activities provide a positive evidence for an applicability of plate tectonics to this area. 5. Sulfur isotope analyses of sulfide minerals from 8 mines revealed that these deposits were genetically connected with the spacially associated ingeous rocks showing relatively narrow range of ${\delta}^{34}S$ values (-0.9‰ to +7.5‰ except for +13.3 from Mulgum Mine). A sequence of metallogenic zones from the coast to the inland is delineated to be in the order of Fe-Cu zone, Cu-Pb-Zn zone, and W-Mo zone. A few porphyry type copper deposits are found in the Fe-Cu zone. These two facts enable the sequence to be comparable with that of Andean type in South America. 6. The VGP's of Cretaceous and post Cretaceous rocks from Korea are located near the ones($71^{\circ}N$, $180^{\circ}E$ and $90^{\circ}N$, $110^{\circ}E$) obtained from continents of northern hemisphere. This suggests that the Korean peninsula has been stable tectonically since Cretaceous, belonging to the Eurasian continent. 7. Different polar wandering path between Korean peninsula and Japanese islands delineates that there has been some relative movement between them. 8. The variational feature of declination of NRM toward northwestern inland side from southeastern extremity of Korean peninsula suggests that the age of rocks becomes older toward inland side. 9. The geological structure(mainly faults) and trends of lineaments interpreted from the Landsat imagery reveal that NNE-, NWW- and NEE-trends are predominant in the decreasing order of intensity. 10. The NNE-trending structures were originated by tensional and/or compressional forces, the directions of which were parallel and perpendicular respectively to the subduction boundary of the Kula plate during about 90 m.y. B.P. The NWW-trending structures were originated as shear fractures by the same compressional forces. The NEE-trending structures are considered to be priginated as tension fractures parallel to the subduction boundary of the Kula plate during about 70 m.y. B.P. when Japanese islands had drifted toward southeast leaving the Sea of Japan behind. It was clearly demonstrated by many authors that the drifting of Japanese islands was accompanied with a rotational movement of a clock-wise direction, so that it is inferred that subduction boundary had changed from NNE- to NEE-direction. A number of facts and features mentioned above provide a suite of positive evidences enabling application of plate tectonics to the late Cretaceous-early Tertiary igneous activity and metallogeny in the area. Synthesizing these facts, an arc-trench system of continental margin-type is adopted by reconstructing paleogeographic models for the evolution of Korean peninsula and Japan islands. The models involve an extention mechanism behind the are(proto-Japan), by which proto-Japan as of northeastern continuation of Gyongsang zone has been drifted rotationally toward southeast. The zone of igneous activity has also been migrated from the inland in late-Cretaceous to the peninsula margin and southwestern Japan in Tertiary.