• 제목/요약/키워드: Silver complex

검색결과 159건 처리시간 0.026초

의복용 메타물질 흡수체 (Metamaterial Based Absorber for Wearable Applications)

  • 이동주;임성준
    • 한국전자파학회논문지
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    • 제28권1호
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    • pp.19-24
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    • 2017
  • 본 논문에서는 스크린 인쇄 방식으로 제작된 의복용 메타물질 흡수체를 제안한다. 제안된 흡수체의 단위구조의 도체 패턴 모양은 의류 브랜드인 샤넬 로고를 차용하였으며, FEM 방식의 시뮬레이션 툴을 사용하여 성능을 검증하였다. 또한, 성능을 검증하기 위해 일반적인 직물 원단 위에 전도성 잉크를 스크린 프린팅 방식으로 인쇄하여 시제품을 제작한 뒤, 벡터 회로망 분석기와 두 개의 도파관을 이용하여 반사계수를 측정하였다. 그 결과, 제안된 흡수체는 10.8 GHz에서 약 93 %에 가까운 흡수율을 갖는 것을 확인하였다.

Baroque직물에 나타난 floral 패턴의 조형성 (A Study on the Figuration of Floral Pattern of Baroque Textiles)

  • 이선화;권영숙
    • 복식
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    • 제52권7호
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    • pp.1-11
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    • 2002
  • The shape of floral Pattern in the Period of Baroque could be divided single. bunch and vine. The style of representation was stylized, abstract and realistic. the most of style was stylized. The type of composition was fullness, independent and scattered. Floral patterns were shaped simple and complex and components of design could be classified into flower and leaf. flower and fruit. flower and band. bunch of flower, flower and geometry. flower and pot, flower and animal. flower and crest. Kinds of flower were tulip. common marigold, lily, carnation, small bel]flower. lotus, acandus leaf, pomegranate, strawberry. pine cone and abstract anonymous flower which were unfolded by repeat. Characters of floral Pattern were classical elegance, taste of royalty and lively and damask, velvet, brocade which made with gold and silver so, those were a very brilliant and gorgeous. Characters of design were illustrated plane style and stylization where developed arranged on front by repeat or repeat symmetric of vertical. Art, costumes and textiles in this era were a very rich and colorful. The result of study on Baroque's floral pattern will be used to develope a various textile design and chance to be adopted classical pattern into aesthetic value in our time.

영화(映畵) "벨벳 골드마인(Velvet Goldmine)"에 나타난 글램 스타일(Glam Style) (The Glam Style Expressed in the Movie "Velvet Goldmine")

  • 김은아;염혜정
    • 패션비즈니스
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    • 제5권1호
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    • pp.73-85
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    • 2001
  • The purpose of this study is to understand what the Glam Style is, focus on the movie "Velvet Goldmine". The Glam Style is refered early 1970s Glam rockers' costume, typified by silver lurex, corksoled platform, men in make-up, personified, for example, by David Bowie, Marc Bolan, New York Dolls, Roxy Music and Iggy Pop. To approach the Glam Style comprehensively, I have divided the formative background of Glam Style into the improvement technology, the advent of the young generation and the diffusion of mass media, the rock music fever and influence on Pop art. Following is the result of analyzing of the character in the movie. First, Brian Slade has the flamboyant transsexual image by skin-tight space suit, glitter pants, lurex, satin and sequined stretch fabrics, vivid color, gauze make-up, feather boa. Second, Curt Wild expresses the outrageous sexual image by black leather jacket, emphasized black eyes make-up. Third, Mandy Slade appears the exaggerated and frivolous image by gold leopard patterned one piece, fur coat, ornamented with beads, tropical make-up, spangles and the costume jewelry. Forth, Auther Stuart has the complex image by black leather jacket, velvet jacket, skin-tight bold shirt, glitter pants, glitter make-up, silk scarf, cherry-red sunglasses. The characteristics meaning of Glam Style implied in this formative characteristic could be presented as the experimental expression of androgynous, the hordes of outrageous alien and kitsch parody.

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광양금광상(光陽金鑛床), 고흥동광상(高興銅鑛床)의 광상생성(鑛床生成)과 암석학적(岩石學的) 연구(硏究) (Metallogenesis and Petrology of the Gwangyang Gold Deposits and Goheung Copper Deposits)

  • 박영석;신병우
    • 자원환경지질
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    • 제17권2호
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    • pp.91-100
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    • 1984
  • The Gwangyang gold deposits geologically consist of granitic gneiss, metatectic gneiss and porphyroblastic gneiss which correspond to Jirisan gneiss complex. The formations of Gyeongsang system lies unconformably on these gneisses and are intruded by diorite, porphyritic andesite and Bulgugsa granites. Goheung districts are composed of quartz schist, andesitic rock, tuff and granite. The Gwangyang gold deposits are gold bearing fissure filling veins. The vein thickness varies from 15cm to 40cm and they consist of 7-10 layers in parallel. The Goheung copper deposits are sulphide bearing quartz veln which filled the fracture in andesitic rock and biotite granite. The contact zone of these rocks is partially altered. The mineral paragenesis of the Gwangyang and Goheung districts is pyrite, arsenopyrite, pyrrhotite, chalcopyrite, sphalerite, galena, sericite, quartz and calcite. The variation trends of FMA and A'KF triangular diagrams and the differentiation index (norm, Q + Or + Ab) versus oxides diagrams is similar to the Gyeonsang basin igneous rocks. From the trace element analysis of 10 samples of country rocks, wall rocks and veins, the distribution of copper and lead contents display a correlative distribution pattern in relation to gold and silver. Homogenization temperature of fluid inclusions range from $200^{\circ}C$ to $270^{\circ}C$ in quartz from the Gwangyang gold vein and the size of fluid inclusion range from 0.01mm to 0.04mm. The fluid inclusions are mainly one or two phase and the filling degree of the inclusions varies from 85 to 95.

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Rehabilitation of an Amur Leopard Cat (Prionailurus bengalensis) with Complex Injury by a Road Accident

  • Sungryong Kim;Sungin Lee;Ok-Joo Lim;Ki-Jeong Na;Dong-Hyuk Jeong
    • 한국임상수의학회지
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    • 제39권6호
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    • pp.411-416
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    • 2022
  • A 2.2 kg adult female Amur leopard cat (Prionailurus bengalensis) injured in a road accident was rescued. Severe abrasions on the left chin were washed daily with an antiseptic and silver sulfadiazine ointment was applied. Corneal edema of the oculus sinister (OS) was treated with ofloxacin and 5% sodium chloride eye drops. The skin wounds gradually improved, but the eye condition did not improve and the lens was also found to be detached. In addition, on the 6th day of hospitalization, melena was observed. On radiographic examination, foreign bodies in the stomach and a fracture of the sternum were confirmed. Subsequently, endoscopic removal of foreign bodies and enucleation of the OS using an electrothermal vessel sealer were performed sequentially over several days. However, corrective surgery of the fractured sternum was not carried out because a natural union of the fracture had occurred, which was found to be fairly stable. The patient completely recovered on the 83rd day and was successfully released into the wild on the 97th day, after two weeks of adaptation training in a natural environment. This report describes the rehabilitation of a wild Amur leopard cat injured in a road accident through a series of diagnostic and treatment steps until its eventual return to the wild and highlights some improvements needed in the process.

한국 중부와 동남부지역 금·은광화작용의 성인적 특성 (Contrasting Styles of Gold and Silver Mineralization in the Central and Southeastern Korea)

  • 최선규;최상훈
    • 자원환경지질
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    • 제28권6호
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    • pp.587-597
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    • 1995
  • 한반도 중부지역과 동남부지역에 분포하는 금-은 광상들의 광화작용은 쥐라기 중기로부터 백악기 말기에 걸쳐서 진행되었으며, 이들 광상은 유행별로 산출지역 및 산출시기에 연관된 지질학적 지화학적 생성환경의 차이를 나타내고 있다. 중부지역 금-은 광상은 북동-남서의 방향성을 갖고 산출분포하는 중생대 화강암류 및 주변 선캠브리아기 변성암류내에 분포하지만, 동남부지역 금-은 광상은 백악기 퇴적암 및 화산암류내에 주로 배태되고 있다. 이는 한반도 대표적인 화성활동인 쥐라지 대보화성활동 및 백악기 불국사 화성활동과 각각 밀접한 성인적 연관성을 시사하고 있다. 이러한 각 광상들의 광화작용 특성(광물공생관계, 조직, 구조 등)과 연대측정결과 및 지질학적 분포특성은 쥐라가 중기로부터 백악기 말기에 이르기까지 광상형성과 연관된 열수유체의 성인적 차이를 의미하고 있다. 즉, 쥐라기로부터 초기 백악기에는 금광단일형 광상의 광화작용이 우세하게 진행되었으나, 후기 백악기에 이르면서 금-은혼합형광상 및 은광단일형 광상의 광화작용이 우세하게 야기되었음을 알 수 있다. 쥐라기 금광단일형 광상들은 괴상의 맥상 산출특성 및 단순한 광석 광불 공생관계를 보여주는 단성광맥으로 높은 fineness 값을 나타내지만, 백악기 금-은혼합형 광상과 은광단일형 광상은 다양하고 복잡한 구조 및 조치특성 갖는 복성 광맥내에 함은황인 및 황화광물과 함은tellurides 및 자연은 등을 포함하는 등 상대적으로 복잡한 광석광물 공생과계를 보여준다. 한편 황화광물의 지질온도계와 유체포유물 연구의 결과등에 의하면 백악기 금-은혼합형 광상과 은광단일형 광상은 천부(<0.5 kb)에서 천수가 우세한 광화유체로부터 $200^{\circ}{\sim}350^{\circ}C$ 온도조건하에서 주된 광화작용이 진행되었지만, 쥐라기 금광단일형 광상은 마그마기원의 열수용액으로부터 고온$(300^{\circ}{\sim}500^{\circ}C)$ 및 고압$({\approx}4-5kb)$의 생성환경하에서 광화작용이 진행되었음을 시사한다.

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한국 금-은광화작용과 천열수 광상의 성인모텔 : 탐사에의 적용

  • 최선규;박상준;김창성
    • 한국광물학회:학술대회논문집
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    • 한국광물학회.대한자원환경지질학회.대한광업진흥공사 2002년도 추계 공동 심포지엄 논문집: 국내 자원의 현황과 전망
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    • pp.119-136
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    • 2002
  • Contrasts in the style of the gold-silver mineralization in geologic and tectonic settings in Korea, together with radiometric age data, reflect the genetically different nature of hydrothermal activities, coinciding with the emplacement age and depth of Mesozoic magmatic activities. It represents a clear distinction between the plutonic settings of the Jurassic Daebo orogeny and the subvolcanic environments of the Cretaceous Bulgugsa igneous activities. During the Daebo igneous activities (c.a. 200-150 (?) Ma) coincident with orogenic time, gold mineralization took place between c.a. 195 and 135 (127 ?) Ma. The Jurassic Au deposits commonly show several characteristics; prominent association with pegmatites, low Ag/hu ratios in the ore-concentrating parts, massive vein morphology and a distinctively simple mineralogy including Fe-rich sphalerite, galena, chalcopyrite, arsenopyrite, Au-rich electrum, pyrrhotite and/or pyrite. During the Bulgugsa igneous activities $(110\~50Ma)$, the precious-metal deposits are generally characterized by such features as complex vein morphology, medium to high AE/AU ratios in the ore concentrates, and diversity of ore minerals including base-metal sulfides, pyrite, arsenopyrite, Ag-rich electrum and native silver nth Ag sulfides, Ag-Sb-As sulfosalts and Ag tellurides. Vein morphology, mineralogical, fluid inclusion and stable isotope results indicate the diverse genetic natures of hydrothermal systems in Korea. The Jurassic Au-dominant deposits (orogenic type) were formed at the relatively high temperature $(about\;300^{\circ}\;to\;450^{\circ}C)$ and deep-crustal level $(4.0{\pm}1.5\;kb)$ from the hydrothermal fluids containing more amounts of magmatic waters $(\delta\;^{18}O_{H2O}\;5\~10\%_{\circ})$. It can. It can be explained by the dominant ore-depositing mechanisms as $CO_2$ boiling and sulfidation, suggestive of hypo- to mesothermal environments. In contrast, the Cretaceous Au-dominant $(l13\~68\;Ma),\;Au-Ag \;(108\~47\;Ma)$ and Ag-dominant $(103\~45\;Ma)$ deposits, which correspond to volcanic-plutonic-related type, occurred at relatively low temperature $(about\;200^{\circ}\;to\;350^{\circ}C)$ and shallow-crustal level $(1.0\{pm}0.5\;kb)$ from the ore-forming fluids containing more amounts of less-evolved meteoric waters$(\delta\;^{18}O_{H2O}\;-10\~5\%_{\circ})$. These characteristics of the Cretaceous precious-metal deposits can be attributed to the complexities in the ore-precipitating mechanisms (mixing, boiling, cooling), suggestive of epi- to mesothermal environments. Therefore, the differences of the emplacement depth between the Daebo and the Bulgugsa igneous activities directly influence the unique temporal and spatial association of the deposit styles.

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L-Sparteine 수식전극을 사용한 Hg (II) 이온의 정량 (Determination of Hg (II) Ion at a Chemically Modified Carbon Paste Electrode Containing L-Sparteine)

  • 정의덕;원미숙;심윤보
    • 대한화학회지
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    • 제35권5호
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    • pp.545-552
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    • 1991
  • 수은 이온의 정량을 위해 l-sparteine으로 처리한 carbon paste 전극(CPE)을 제작하였다. 수용액중의 수은 이온을 CPE에 수식 시킨 l-sparteine과 반응시켜 착화합물 상태로 전극표면에 석출시킨 후 이 착물을 벗김 전압-전류곡선법을 사용하여 정량하였다. 또한 수식된 CPE의 전극반응을 순환 전압 전류 곡선법을 사용하여 초산/초산염 완충용액에서 조사하였다. 한번 사용한 전극은 산 용액으로 처리하여 5회 이상 재사용할 수 있었다. 선형주사 전압전류법을 사용하였을 경우 $2.0{\times}10^{-6}$ M 농도까지 정량이 가능하였다. 시차펄스 전압전류법으로 실험할 경우 $7.0 {\times}10^{-7}$ M 농도까지 직선적으로 감응함을 알 수 있었으며 그 때의 상대 표준편차는 ${\pm}$5.1% 이었다. 이 경우 검출 한계는 $5.O{\times} 10^{-7}$ M이었다. 리간드와 착물을 형성할 것으로 예상되는 여러 금속이온에 대한 방해 작용을 조사하였다. 그 결과 은(I) 이온이 방해를 하지만 염화칼륨으로 사전 처리하여 방해작용을 제거할 수 있었다.

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페놀이 첨가된 생태계에서 세균 군집구조 변화의 분석 (Characterization of Bacterial Community in the Ecosystem Amended with Phenol)

  • 김진복;김치경;안태석;송홍규;이동훈
    • 미생물학회지
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    • 제37권1호
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    • pp.72-79
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    • 2001
  • 폐수 처리장의 방류수에 페놀을 첨가한 후 terminal restriction fragment length polymorphism (T-RFLP) 방법을 이용하여 세균군집의 구조와 변화를 조사하였다. 시료로부터 얻은 16S rRNA gene은 eubacterial primer로 증폭하였으며, 한 primer는 5'말단에 biotin을 부착하였다. 증폭된 product는 HaeIII와 AluI으로 각각 절단하였고, 절단된 단편 중에서 terminal restriction fragment (T-RF)를 streptavidin paramagnetic particle을 이용하여 분리하였다. 분리된 T-RF는 전기영동과 silver staining을 통하여 확인하였다. 본 실험의 유용성을 검증하기 위하여 표준 균주 10 균주를 대상으로 실험하였고, 균주마다 특징적인 T-RF를 가지는 것과 그 크기가 Ribosomal database project (RDP) 자료로부터 계산된 결과와 일치하는 것을 확인할 수 있었다. 한편, 대조군으로 사용된 페놀을 첨가하지 않은 방류수 시료에서는 Acinetobacter, Bacillus, Pseudomonas 속 등이 우점종을 차지하고 있었고, 페놀 (최종농도 250mg.$l^{-1}$)을 첨가한 방류수 시료에서는 Acinetobacter, Comamonas, Cytophaga, Pseudomonas 속 등이 우점종을 차지함을 알 수 있었다. Gel에서 분리한 Acinetobacter와 Cytophaga에 해당되는 T-RF는 재증폭 및 염기 서열 분석이 가능하였는데, database의 염기서열과 비교한 결과 Acinetobacter junii와 유연관계가 가깝다는 것을 확인하였다.

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광양-승주지역 금은광상의 광화작용 (Gold-Silver Mineralization in the Kwangyang-Seungju Area)

  • 이창신;김용준;박천영;고진석
    • 자원환경지질
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    • 제26권2호
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    • pp.145-154
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    • 1993
  • Gold-silver deposits in the Kwangyang-Seungju area are emplaced along $N4^{\circ}{\sim}10^{\circ}W$ to $N40^{\circ}{\sim}60^{\circ}W$ trending fissures and fault in Pre-cambrian Jirisan gneiss complex or Cretaceous diorite. Mineral constituents of the ore from above deposits are composed mainly of pyrite, arsenopyrite, pyrrhotite, magnetite, sphalerite, chalcopyrite, galena and minor amount of electrum, tetrahedrite, miargyrite, stannite, covellite and goethite. The gangue minerals are predominantly quartz and calcite. Gold minerals consist mostly of electrum with a 56.19~79.24 wt% Au and closely associated with pyrite, chalcopyrite, miargyrite and galena. K-Ar analysis of the altered sericite from the Beonjeong mine yielded a date of $94.2{\pm}2.4\;Ma$ (Lee, 1992). This indicates a likely genetic tie between ore mineralization and intrusion of the middle Cretaceous diorite ($108{\pm}4\;Ma$). The ${\delta}^{34}S$ values ranged from +1.0 to 8.3‰ with an average of +4.4‰ suggest that the sulfur in the sulfides may be magmatic origin. The temperatures of mineralization by the sulfur isotopic composition with coexisting pyrite-galena and pyrite-chalcopyrite from Beonjeong and Jeungheung mines were $343^{\circ}C$ and $375^{\circ}C$ respectively. This temperature is in reasonable agreement with the homogenization temperature of primary fluid inclusion quartz ($330^{\circ}C$ to $390^{\circ}C$; Park.1989). Four samples of quartz from ore veins have ${\delta}^{18}O$ values of +6.9~+10.6‰ (mean=8.9‰) and three whole rock samples have ${\delta}^{18}O$ values of +7.4~+10.2‰ with an average of 7.4‰. These values are similar with those of the Cretaceous Bulgugsa granite in South Korea (mean=8.3‰; Kim et al. 1991). The calculated ${\delta}^{18}O_{water}$ in the ore-forming fluid using fractionation factors of Bulgugsa et al. (1973) range from -1.3 to -2.3‰. These values suggest that the fluid was dominated by progressive meteoric water inundation through mineralization.

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