• Bulletin of the Korean Chemical Society
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• 제14권6호
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• pp.713-717
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• 1993

The crystal structure of the potassium salt of penicillin V has been studied by the X-ray crystallographic methods. Crystal data are as follows; potassium 3,3-dimethyl-7-oxo-6-phenoxyacetoamido-4-thia-1- azabicyclo[3.2.0]-heptane-2${\alpha}$-carboxylate, $K^+{\cdot}C_{16}H_{18}N_2O_5S^-$, $M_r$= 388.5, triclinic, Pl, a= 9.371 (1), b= 12.497 (2), c= 15.313 (2) ${\AA},\;{\alpha}= 93.74\;(2),\;{\beta}=99.32\;(1),\;{\gamma}=90.17\;(1)^{\circ},\;V=1765.7\;(2)\;{\AA}^3$, Z=4, $D_m=1.461\;gcm^{-1},\;{\lambda}(Cu\;K{\alpha})=1.5418\;{\AA},\;{\mu}=40.1\;cm^{-1}$, F(000)=808, T=296 K. The structure was solved by the heavy atom and difference Fourier methods with intensity data measured on an automated four-circle diffractometer. The structure was refined by the full-matrix least-squares method to a final R= 0.081 for 3563 observed $[I_0{\geq}2{\sigam}(I_0)]$ reflections. The four independent molecules assume different overall conformations with systematically different orientations of the phenyl groups although the penam moieties have the same closed conformations. There are intramolecular hydrogen bonds between the exocyclic amide nitrogen and phenoxy oxygen atoms. The penam moiety is conformationally very restricted although the carboxyl and exocyclic amide groups apparently have certain rotational degrees of freedom but the phenyl group is flexible about the ether bond despite the presence of the intramolecular N-H${\cdots}$O hydrogen bond. There are complicated pseudo symmetric relationships in the crystal lattice. The penam moieties are related by pseudo 20.5 screw axes and the phenyl groups by pseudo centers of symmetry. The potassium ions, related by both pseudo symmetries, form an infinite zigzag planar chain parallel to the b axis. Each potassium ion is coordinated to seven oxygen atoms in a severely distorted pentagonal bipyramid configuration, forming the infinite hydrophilic channels which in turn form the molecular stacks. Between these stacks, there are only lipophilic interactions involving the phenyl groups.

• 한국전기전자재료학회논문지
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• 제32권5호
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• pp.418-425
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• 2019

A piezoelectric ceramic fiber composite (PCFC) was successfully fabricated using $0.69Pb(Zr_{0.47}Ti_{0.53})O_3-0.31[Pb(Zn_{0.4}Ni_{0.6})_{1/3}Nb_{2/3}]O_3$ (PZT-PZNN) for use in small-scale wind energy harvesters. The PCFC was formed using an epoxy matrix material and an array of Ag/Pd-coated PZT-PZNN piezo-ceramic fibers sandwiched by Cu interdigitated electrode patterned polyethylene terephthalate film. The energy harvesting performance was evaluated in a custom-made wind tunnel while varying the wind speed and resistive load with two types of flutter wind energy harvesters. One had a five-PCFC array vertically clamped with a supporting acrylic rod while the other used the same structure but with a five-PCFC cantilever array. Stainless steel (thickness: $50{\mu}m$) was attached onto one side of the PCFC to form the PZT-PZNN cantilever. The output power, in general, increased with an increase in the wind speed from 2 m/s to 10 m/s for both energy harvesters. The highest output power of $15.1{\mu}W$ at $14k{\Omega}$ was obtained at a wind speed of 10 m/s for the flutter wind energy harvester with the PZT-PZNN cantilever array. The results presented here reveal the strong potential for wind energy harvester applications to supply sustainable power to various IoT micro-devices.

• 암석학회지
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• 제9권1호
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• pp.13-28
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• 2000

초정-미원지역은 시대미상의 옥천층군과 이를 관입한 쥬라기의 대보화강암류와 백악기의 암맥류로 이루어졌다. 옥천층군은 하부로부터 미동산층, 운교리규암층, 운교리층, 화전리층, 창리층, 황강리층으로, 이루어지며 미동산층과 운교리규암층은 주로 규암으로 구성되며 운교리층은 사질천매암, 화전리층은 석회질 혹은 이질 천매암, 창리층은 이질 내지 탄질 천매암, 황강리층은 역질 천매암으로 구성된다. 대보화강암류는 흑운모화강암, 반상화강암 및 복움모화강암으로 구성되며 맥암류는 석영반암과 소규모의 규장질-고철질 암맥으로 구성된다. 옥천층군의 주요 선형구조는 N25-45E, NS, N30-45W 방향인 바, N25-45E방향은 등사습곡과 1차엽리를 발달시킨 연성변형에 기인하며 NS와 N30W는 단층과 절리를 야기한 취성변형에 기인한다. 화강암지역인 1구역에서의 NS와 N20-45E 방향은 암백의 관입방향과 일치한다. 이 지역의 토양은 양토, 세립 사질 양토, 사질 양토, 역질- 사질 양토, 암괴와 각력이 있는 양토, 암괴와 각력이 있는 사질 양토, 부식토, 자갈과 모래가 있는 하도 퇴적물 및 암석산지 등으로 나누어진다. 이들은 풍화 잔류토양과 충적토로 크게 구분되는 바, 잔류토양에서 Cd, Cr, Cu, Pb 및 Zn 등은 각각 평균 0.2, 50.6, 35.5, 27.9, 93.4 mg/kg 이며 충적토에서는 각각 평균 1.2, 68.2, 9.1, 25.0, 83.8 ppm 이다. 잔류토양에 비하여 충적토양에 Cd와 Cr값이 높으나 Cu, Pb, Zn의 함량은 낮음이 특징이다. 잔류토양이나 충적토 모두 환경오염 기준치를 초과하지 않는 비오염토양이며 부화지수의 경우도 잔류토양의 경우 0.37, 충적토의 경우도 0.38로 오염되지 않은 토양으로 볼 수 있다. 단 부화지수도에서 볼 수 있는 것처럼 남부지역으로 감에 따라 높아지는 경향은 암석분포에 기인하는 것인지 오염인자와 관련된 것인지는 좀 더 연구할 필요가 있다.

• 한국토양비료학회지
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• 제32권4호
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• pp.398-404
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• 1999

토양과 수질에 영향을 주는 주인자를 찾아내기 위하여 한강 수계에서 집약적 농업이 이루어지고 있는 지역을 대상으로 토양과 수질에 대한 요인 분석을 하였다. 화학성 분석을 위한 토양 시료는 고랭지 농업이 이루어지고 있는 평창군 일대에서 그리고 수질 시료는 한강의 소유역인 구리, 춘천, 둔내 및 대관령에서 1996년과 1997년에 채취하여 분석하였다. 분석된 토양의 질 11요소에 대한 상호 상관분석에서 55개 상관쌍 중 29개 상관쌍의 유의성이 인정되었다. 시료채취 적정성을 위한 전체 Kaiser값은 0.6이었다. 토양의 질 요소 중 부하가 큰값을 보이는 제1요인은 pH, Ca 및 Mg이었다. 제2요인은 인산과 미량요소이었으며, 제2요인은 인산과 미량요소이었으며, 제3요인은 유기물과 EC, 그리고 제4요인은 칼리와 철이었다. 수질 요소 20개의 190개 상관쌍 중 86개 상관쌍의 유의성이 인정되었다. 전체 Kaiser값은 0.74이었다. 수질요소 중 제1요인은 EC로 전체 변이의 27.1%를 차지하였으며 Na, Ca, SO4, Mg, K, Cl, NO3 그리고 T-N이 높은 부하를 보였다. 제2요인은 중금속 중 Zn, Fe, Mn 그리고 Cd이었다. 제3요인에서 제7요인은 각각 PO4, TSS, 무기질소, pH 와 T-P 그리고 Cu이었다. EC 요인 스코어는 구리에서 가장 높았고, 춘천, 둔내 및 대관령의 순이었다. 이 연구 결과는 요인 분석이 농업 소유역에서 토양과 수질에 영향을 주는 주요인 분석 선정에 유용함을 의미하였다.

• Asian Journal of Atmospheric Environment
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• 제8권3호
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• pp.126-139
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• 2014

In order to estimate the influence of sources on $PM_{2.5}$ in the industrial area of Japan, we carried out a source analysis using chemical component data of $PM_{2.5}$. $PM_{2.5}$ samples were collected intermittently at an industrial area in Japan from July 2010 to November 2012. Water soluble ions ($Cl^-$, $NO_3{^-}$, $SO{_4}^{2-}$, $Na^+$,$NH_4{^+}$, $K^+$, $Mg^{2+}$, $Ca^{2+}$), elements (Al, K, Ca, Ti, V, Cr, Mn, Fe, Ni, Cu, Zn, As, Cd, Sb, Pb), and carbonaceous species (OC, EC) of the $PM_{2.5}$ (a total of 198 samples) were analyzed. Positive Matrix Factorization (PMF) model was applied to the data of those chemical components to identify the source of $PM_{2.5}$. At this observation site, nine factors were extracted. The major contributors of $PM_{2.5}$ were secondary sulfate 1, in which loading factors of $SO{_4}^{2-}$ and $NH_4{^+}$ were large (percentage source contribution: 20.9%), traffic, in which loading factors of OC (organic carbon) and EC (elemental carbon) were large (20.8%), secondary sulfate 2, in which loading factors of K and $SO{_4}^{2-}$ were large (8.0%), steel mills (7.8%), secondary chloride and nitrate (7.0%), soil (5.0%), heavy oil combustion (3.8%), sea salt (3.8%), and coal combustion (2.3%). The conditional probability function (CPF) and the potential source contribution function (PSCF) were carried out to examine the influence of a regional source and a broad-based source, respectively. CPF results supported local source influences such as steel mills, sea salt, traffic, coal combustion, and heavy oil combustion. PSCF results suggested that ships in the East China Sea, an industrial area of the east coastal region of China, and an active volcano in the Kyushu region of Japan were potential regional sources of secondary sulfate 1. Secondary sulfate 2 was affected by the burning of biomass fields and by coal combustion in Chinese urban areas such as Beijing, Hebei, and western Inner Mongolia. Source characterization using continuous data from one site showed a potential source representing fossil fuel combustion is affected both by regional and broad-based sources.

• 한국대기환경학회지
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• 제24권4호
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• pp.439-454
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• 2008

The purpose of this study was to extensively identify $PM_{10}$ sources and to estimate their contributions to the study area, based on the analysis of the $PM_{10}$ mass concentration and the associated inorganic elements, ions, and total carbon. The contribution of $PM_{10}$ sources was estimated by applying a receptor method because identifying air emission sources were effective way to control the ambient air quality. $PM_{10}$ particles were collected from May to November 2007 in the Yongin-Suwon bordering area. $PM_{10}$ samples were collected on quartz filters by a $PM_{10}$ high-volume air sampler. The inorganic elements (Al, Mn, V, Cr, Fe, Ni, Cu, Zn, Cd, Pb, Si, Ba, Ti and Ag) were analyzed by an ICP-AES after proper pre-treatments of each sample. The ionic components of these $PM_{10}$ samples ($Cl^_$, $NO_3^-$, $SO_4^{2-}$, $Na^+$, $NH_4^+$, $K^+$, $Ca^{2+}$, and $Mg^{2+}$) were analyzed by an IC. The carbon components (OC1, OC2, OC3, OC4, OP, EC1, EC2 and EC3) were also analyzed by DRI/OGC analyzer. Source apportionment of $PM_{10}$ was performed using a positive matrix factorization (PMF) model. After performing PMF modeling, a total of 8 sources were identified and their contribution were estimated. Contributions from each emission source were as follows: 13.8% from oil combustion and industrial related source, 25.4% from soil source, 22.1% from secondary sulfate, 12.3% from secondary nitrate, 17.7% from auto emission including diesel (12.1%) and gasoline (5.6%), 3.1% from waste incineration and 5.6% from Na-rich source. This study provides information on the major sources affecting air quality in the receptor site, and therefore it will help us maintain and manage the ambient air quality in the Yongin-Suwon bordering area by establishing reliable control strategies for the related sources.

• 한국대기환경학회지
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• 제29권1호
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• pp.74-85
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• 2013

Since the underground transportation system is a closed environment, indoor air quality problems may seriously affect many passengers' health. The purpose of this study was to understand $PM_{10}$ characteristics in the underground air environment and further to quantitatively estimate $PM_{10}$ source contributions in a Seoul Metropolitan subway station. The $PM_{10}$ was intensively collected on various filters with $PM_{10}$ aerosol samplers to obtain sufficient samples for its chemical analysis. Sampling was carried out in the M station on the Line-4 from April 21 to 28, July 13 to 21, and October 11 to 19 in the year of 2010 and January 11 to 17 in the year of 2011. The aerosol filter samples were then analyzed for metals, water soluble ions, and carbon components. The 29 chemical species (OC1, OC2, OC3, OC4, CC, PC, EC, Ag, Al, Ba, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Si, Ti, V, Zn, $Cl^-$, $NO_3{^-}$, $SO_4{^{2-}}$, $Na^+$, $NH_4{^+}$, $K^+$, $Mg^{2+}$, $Ca^{2+}$) were analyzed by using ICP-AES, IC, and TOR after proper pretreatments of each sample filter. Based on the chemical information, positive matrix factorization (PMF) model was applied to identify the $PM_{10}$ sources and then six sources such as biomass burning, outdoor, vehicle, soil and road dust, secondary aerosol, ferrous, and brakewear related source were classified. The contributions rate of their sources in tunnel are 4.0%, 5.8%, 1.6%, 17.9%, 13.8% and 56.9% in order.

• 한국지구과학회지
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• 제24권5호
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• pp.477-490
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• 2003

한국 동해안 영일만 해역에서 퇴적물의 금속 함량과 공간 변화 특성을 연구하기 위해 총 27개의 표층 퇴적물을 채취하여, 입자조직, 유기탄소, 금속 원소들의 함량을 분석하였다. 연구해역애서 표층 퇴적물의 입도는 전반적으로 해안선 부근에서 조립하고 만의 중앙부에서 세립하며, 이러한 공간 변화는 해저지형과 반시계방향의 해류 패턴에 의한 것으로 해석된다. 유기탄소와 금속 원소들의 함량은 대부분 퇴적물의 입도 변화에 수반되어 니질 함량이 높은 만의 중앙부에서 높고 사질 함량이 높은 해안선 쪽으로 갈수록 낮아진다. 그러나 칼슘, 스트론튬, 칼륨의 함량은 조립한 퇴적물이 우세한 해안선 부근 퇴적물에서 높고, 몇몇 중금속(구리, 아연, 카드뮴) 함량 또한 유기물 함량이 매우 높은 구항과 형산강 입구의 퇴적물에서 높은 특징을 보인다. 상관관계 및 요인분석 결과에 의하면, 대부분의 금속 원소들의 함량과 공간 변화는 퇴적물의 입도에 의해 조절되는 것으로 보이나, 카드뮴, 구리 아연, 주석 등은 퇴적층의 무산소 환경에서 일어나는 지화학적 메카니즘이 이들의 함량과 공간 변화를 조절하는 일차적인 요인으로 제시된다. 약산추출 부분(labile fraction)의 함량과 농축비(concentration enrichment ratio) 연구결과에 의하면, 중금속 원소들의 존재 형태가 대부분 "sulfide minerals"와 관련된 것으로써, 이들의 형성과 축적이 일부 연구해역에서 중금속 오염의 주원인으로 제시된다. 한편, 칼슘과 스트론튬 경우에는 퇴적물에 함유된 패각 함량에 의해, 그리고 칼륨은 사질 퇴적물에 우세한 장석(feldspar) 광물에 의해 조절되는 것으로 해석된다.

• 한국주조공학회지
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• 제11권6호
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• pp.475-481
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• 1991

In this study the fabrication technology and mechanical properties of AC8A/$Al_2O_3$ Composites by squeeze casting process were investigated to develope for application as the piston materials that require good friction, wear resistance, and thermal stability. AC8A/$Al_2O_3$ composistes without a porosity and the break of preform were fabricated at the melt temperature of $740^{\circ}C$, the preform temperature of $500^{\circ}C$, and mold temperature of $400^{\circ}C$ under the applied pressure of $1200kg/cm^2$ as the results of the observation of microstructures. As the results of this study, the tensile strength of AC8A/$Al_2O_3$ composites was not increased linearly with $Al_2O_3$ volume fraction and so it seemed not to agree with the rule of mixture, which had been used often in metal matrix composite. Also the tensile strength after thermal fatigue test was little different from that before the test. Consequently it was thought that AC8A/$Al_2O_3$ composites fabricated under our experimental conditions had a good thermal stability and subsequently a good interface bonding. Wear rate(i.e., volume loss per unit sliding distance) of AC8A/$Al_2O_3$ composites was decreased with $Al_2O_3$ volume fraction and the sliding speed at both room temperature and $250^{\circ}C$ and so there was a good correlation between wear rate and hardness. Also the wear rate of AC/8A20% $Al_2O_3$ composities was obtained the value of $1.65cm^3/cm$ at sliding speed of 1.14m/sec as compared with about $3.0\;{\times}10^{-8}cm^3/cm$ hyereutectie Al-Si alloy(Al-16%Si-2%Cu-1%Fe-1%Ni), which applied presently for piston materials. The wear behavior of $Al_2O_3$ composites was observed to a type of abrasive wear by the SEM view of wear surface.

• 한국진공학회:학술대회논문집
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• 한국진공학회 2000년도 제18회 학술발표회 논문개요집
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• pp.174-174
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• 2000

A strong antiferromagnetic coupling in Fe/Si multilayered films (MLF) had been recently discovered and much consideration has been given to whether the coupling in the Fe/Si MLF system has the same origin as the metal/metal MLF. Nevertheless, the nature of the interfacial ron silicide is still controversial. On one hand, a metal/ semiconductor structure was suggested with a narrow band-gap semiconducting $\varepsilon$-FeSi spacer that mediates the coupling. However, some features show that the nature of coupling can be well understood in terms of the conventional metal/metal multilayered system. It is well known that both magneto-optical (MO) and optical properties of a metal depend strongly on their electronic structure that is also correlated with the atomic and chemical ordering. In this study, the nature of the interfacial regions is the Fe/Si multilayers has been investigated by the experimental and computer-simulated MO and optical spectroscopies. The Fe/Si MLF were prepared by rf-sputtering onto glass substrates at room temperature with the number of repetition N=50. The thickness of Fe sublayer was fixed at 3.0nm while the Si sublayer thickness was varied from 1.0 to 2.0 nm. The topmost layer of all the Fe/Si MLF is Fe. In order to carry out the computer simulations, the information on the MO and optical parameters of the materials that may constitute a real multilayered structure should be known in advance. For this purpose, we also prepared Fe, Si, FeSi2 and FeSi samples. The structural characterization of Fe/Si MLF was performed by low- and high -angle x-ray diffraction with a Cu-K$\alpha$ radiation and by transmission electron microscopy. A bulk $\varepsilon$-FeSi was also investigated. The MO and optical properties were measured at room temperature in the 1.0-4.7 eV energy range. The theoretical simulations of MO and optical properties for the Fe/Si MLF were performed by solving exactly a multireflection problem using the scattering matrix approach assuming various stoichiometries of a nonmagnetic spacer separating the antiferromagnetically coupled Fe layers. The simulated spectra of a model structure of FeSi2 or $\varepsilon$-FeSi as the spacer turned out to fail in explaining the experimental spectra of the Fe/Si MLF in both intensity and shape. Thus, the decisive disagreement between experimental and simulated MO and optical properties ruled out the hypothesis of FeSi2 and $\varepsilon$-FeSi as the nonmagnetic spacer. By supposing the spontaneous formation of a metallic ζ-FeSi, a reasonable agreement between experimental and simulated MO and optical spectra was obtained.