• Title/Summary/Keyword: 백금족 원소

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RF Magnetron Sputtering을 이용하여 제작한 불용성 촉매전극의 해수전해 특성

  • Lee, Hyeon-Seok;Kim, Se-Gi;Seok, Hye-Won;Choe, Heon-Jin
    • Proceedings of the Materials Research Society of Korea Conference
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    • 2011.10a
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    • pp.29.2-29.2
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    • 2011
  • 수용액 상에서 유기물이나 무기물의 전해산화에는 높은 산소과전압과 그 화학종에 대한 화학적, 물리적 안정성이 요구되며, 이러한 요구 조건을 만족하는 소재로써 백금족의 원소가 통상 사용되고 있으나, 가격이 매우 비싸다는 단점을 가지고 있다. 특히 고전류밀도 폐수처리 불용성 전극은 수용액을 전기분해할 때 높은 전류밀도를 낼 수 있으며, 폐수에 혼합되어 있는 각종 화학적 성분에 대한 화학적, 물리적 내구성이 있는 전극으로서, 현재 기존의 수처리용 전극은 금속 Ti을 기판으로 하여 그 위에 불용성 촉매로써 전도성 금속염을 도포, 열처리를 반복하여 산화물의 형태로 수 ${\mu}m$의 두께로 코팅하는 이른바, DSA (Dimensionally Stable Anodes) 전극을 사용하고 있는데, 이는 제조 단가의 상승과 금속 Ti 기판 상에 코팅된 전도성 금속산화물의 미약한 접착력으로 인한 탈리로 전극 전체의 성능 저하 및 수명 단축을 초래하는 문제점이 있다. 본 연구에서는 상기의 문제점을 개선하고자 대표적 불용성 촉매 물질인 백금을 RF magnetron 스퍼터링방식으로 100~300 nm 두께로 성막하여 Ti 기판에 대한 불용성 촉매 물질의 부착력과 내구성 및 모의 해수에 대한 해수전해 특성 등을 평가하였다.

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Simultaneous Determination of Traces of Platinum and Rhodium by Differential Pulse Polarograpy (펄스 차이 폴라로그래피법에 의한 미량 백금과 로듐의 동시 정량)

  • Czae, Myoung-Zoon;Lee, Chul;Hong, Tae-Kee;Kwon, Young-Soon;Hong, Mi-Jeong
    • Journal of the Korean Chemical Society
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    • v.39 no.1
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    • pp.35-39
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    • 1995
  • Simultaneous measurements of trace platinum and rhodium, based on catalytic reduction of protons by the adsorbed Pt-formazone and Rh-formaldehyde complexes formed in formaldehyde-hydrazine-sulfuric acid medium, were demonstrated. The conditions for the measurements of Pt and Rh both present at trace levels (>10-10 M) were 0.004% (w/v) formaldehyde-0.0012% (w/v) hydrazine-0.75 M sulfuric acid. In this medium method detection limits are 7.3${\times}$10-11 M Pt and 3.2${\times}$10-11 M Rh. And dynamic ranges are 5${\times}$10-10~6${\times}$10-8 M and 1${\times}$10-10∼2${\times}$10-8 M for platinum and rhodium respectively. In the linear dynamic ranges, Rh and Ir interfere platinum in the presence of only 10 and 100 times that of Pt respectively. There are no interferences from other platinum group metal ions for rhodium even in the presence of a 500-fold excess of Ir(IV), a hundredfold excess of platinum.

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수소 발생 반응 촉매 개발: 원소 치환을 통한 MoS2 표면 최적화

  • Lee, Gyeong-Pung;Yu, Dong-Seon
    • Proceeding of EDISON Challenge
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    • 2016.03a
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    • pp.330-332
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    • 2016
  • 수소 발생 반응 촉매는 주로 백금(Pt)족 물질로 만들어져왔으나, 그 높은 가격과 희귀성으로 인해 이를 대체할 촉매의 개발이 요구되고 있다. 그중에서 주목받는 물질이 판상 $MoS_2$인데, 순물질로써의 $MoS_2$는 오직 모서리 부분만이 촉매로 기능하며 표면은 안정하여 촉매로써 기능을 하지 못한다는 한계가 있었다. 따라서 $MoS_2$의 표면도 촉매로 기능하여 보다 효율적인 촉매가 될 수 있도록, 자연계에 비교적 풍부한 원소들로 Mo원자를 치환해 보고 평면 스트레인을 줌으로써 표면이 촉매로 기능할 수 있는 조건을 밀도 범함수 이론에 근거해 계산해 보았다. 그 결과, Ge로 치환되고 -10% 스트레인이 걸린 $MoS_2$의 표면이 촉매로 기능할 수 있는 조건을 만족시켰다. 한편 Ge로 치환된 샘플에 수소를 흡착시켰을 때, 치환된 원자와 수소 원자가 반발력을 나타내는 듯한 현상이 관찰되었다.

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Determination of Rhodium by Differential Pulse Polarography (펄스차이 폴라로그래피를 이용한 로듐의 정량)

  • Kwon, Young-Soon;Hong, Mi-Jeong;Czae, Myung-Zoon
    • Analytical Science and Technology
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    • v.13 no.1
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    • pp.1-4
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    • 2000
  • Determination of trace rhodium, based on catalytic reduction of protons by the adsorbed Rhformaldehyde complexes formed in formaldehyde-hydrochloric acid medium, was demonstrated. The condition for the measurements of Rh at trace levels was 0.004%(w/v) formaldehyde-0.75M hydrochloric acid. In this medium detection limit was $7.0{\times}10^{-12}M$ and the linear dynamic range was $1.0{\times}10^{-11}{\sim}1.0{\times}10^{-8}M$ Rh. There were no interferences from other platinum group metal ions even in the presence of a 500-fold excess.

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장수명핵종군 분리공정 평가

  • 이일희;김광욱;홍두성;양한범;임재관;권선길;김영환;정동용;김응호
    • Proceedings of the Korean Nuclear Society Conference
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    • 1998.05b
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    • pp.521-526
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    • 1998
  • 군분리공정의 관심대상 핵종인 잔존 U, MA인 Am, Np 및 백금족원소의 장수명핵종인 Tc을 방사성모의용액으로부터 효과적으로 분리할 수 있었다. 각 단위공정에 주입되는 용액의 농도를 기준으로 하여 볼 때 잔존 U 제거 공정에서 U, Np, 및 Tc의 회수율은 각각 99.1%. 31.9%, 및 99.5%였다. 개미산 탈질 공정에서는 탈질 용액의 총 산도를 0.4M 이하까지 감소시켰으며, 부수적으로 후속용매추출 공정 전반에 걸쳐 문제 핵종으로 작용하는 Zr, Mo, Fe 등을 각각 99.8%, 94.2%, 22.4% 침전 제거시킬 수 있었다. 마지막으로 DEHPA에 의한 AM/RE 상호분리 공정에서는 연속적인 선택적역추출에 의해 Am 및 Np 의 회수율은 각각 99.8% 및 98.2% 정도였고, Am의 경우 7.6%읜 Fe및 81.6% 의 Mo가, Np의 경우 5.8%의 Fe이 불순물로서 여전히 존재하고 있다. 한편 RE 생성물에서는 97~99.9%의 RE가 회수 제거되었다.

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Determination of Fission Products in Simulated Nuclear Spent Fuels by Cation.Anion Exchange Chromatography and Inductively Coupled Plasma Atomic Emission Spectrometry (양.음이온교환 크로마토그래피와 유도결합플라스마 원자방출분광법을 이용한 모의 사용후핵연료 중 핵분열생성물 분석)

  • Choi, Kwang Soon;Sohn, Se Chul;Pyo, Hyung Yeol;Suh, Moo Yul;Kim, Do Yang;Park, Yang Soon;Jee, Kwang Yong
    • Analytical Science and Technology
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    • v.13 no.4
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    • pp.446-452
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    • 2000
  • The simulated nuclear spent fuel (SIMFUEL) containing the platinum group elements which will not be dissolved in a nitric acid was completely dissolved with a acid digestion bomb. The metallic elements separated in the SIMFUEL were measured by inductively coupled plasma atomic emission spectrometry (ICP-AES). Because the peaks of metallic elements were spectrally interfered by uranium spectrum, uranium and metallic elements were separated by cation exchange resin for Mo, Pd, Rh and Ru and by anion exchange resin for Ba, Ce, La, Nd, Rh, Sr, Y and Zr, respectively. The recovery of Mo, Pd, Rh and Ru after separation by cation exchange chromatography found to be 99-103% and anion exchange separation showed 96.5-107% of recovery except Y with the simulated solution whose concentration was similar to the spent nuclear fuel. The relative standard deviation of this method showed 1.3-6.7% in the SIMFUEL whose concentrations of metallic elements were between several $10^2-10^3$ppm.

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Geochemical Characteristics of Black Slate and Coaly Slate from the Uranium Deposit in Deokpyeong Area (덕평리 지역 우라늄광상의 흑색점판암과 탄질점판암의 지구화학적 특성)

  • Shin, Dong-Bok;Kim, Su-Jeong
    • Economic and Environmental Geology
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    • v.44 no.5
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    • pp.373-386
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    • 2011
  • Geochemical study was performed on black slates and interbedded U-bearing coaly slates in Deokpyeongri area, the representative uranium mineralized district of the Ogcheon Metamorphic Belt, to discuss the genetic environments of the uranium deposit. REE concentration (254 ppm) of the black slates is higher than that (169 ppm) of the coaly slates and NASC-normalized REE patterns of the coaly slates show remarkable positive Eu anomaly. l11e redox-sensitive trace elements such as V, Cr, Co, Ni, Mo and U in the coaly slates are highly enriched compared to the black slates, especially for V of 24 times, Mo of 62 times, and U of 60 times. In additions, Pd and Pt are also enriched in the coaly slates. Positive Eu anomaly and the noticeable enrichment of the elements listed above compared to those of NASC indicate that those elements were not derived from common seawater but deposited under high temperature and reducing environment of submarine hydrothermal activities. Wide compositional ranges of major elements ($SiO_2/Al_2O_3$: 3.98~11.88, $Al_2O_3/Na_2O$: 25.6~139.06, $K_2O/Na_2O$: 6.80~46.85) also suggest that the source rocks of the sediments are mixtures of sedimentary rocks and igneous rocks. Higher sulfur contents in the coaly slates, 2.6 wt.%, than those in the black slates, 0.6 wt.% also indicates that the former was influenced by hydrothermal activities containing much sulfur. These geochemical characteristics are similar to the genetic environments of South China type PGE deposits (Mo-Ni-Zn-PGE) which is geotectonically correlated with the Ogcheon Metamorphic Belt and is known as sedimentary-exhalative deposits. In conclusions, the uranium and other metallic elements mineralization seems to have occurred in the sedimentary basin that was affected by submarine hydrothermal activities and rich in organic materials under oxygen-poor environments as well.

Electrodeposition of some Alpha-Emitting Nuclides and its Isotope Determination by Alpha Spectrometry (몇가지 알파입자 방출 핵종의 전해석출 및 알파 스펙트럼 측정에 의한 그의 동위원소 정량)

  • Key-Suck Jung;In-Suck Suh
    • Journal of the Korean Chemical Society
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    • v.27 no.4
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    • pp.279-286
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    • 1983
  • An apparatus was made for the electrodeposition of alpha emitting actinide nuclides, $^{207}Bi$ and $^{210}Po$. The electrodeposition was made on a polished stainless steel plate cathode. The anode was made of platinum wire and to stir the solution. With the ammonium chloride as electrolyte initial pH = 4, chloride concentration = 0.6M and solution volume = 15ml, a current of 1.5 ampere(current density = 0.59A/$cm^2$) was flowed for 100 minutes for the quantitative recovery of electrodeposition and on average recovery of 98.3% was obtained within ${\pm}$0.7% uncertainty. Alpha spectrometry of the electrodeposited sample showed alpha peaks from $^{210}Po, ^{234}U$ and $^{239}Pu$ having energy resolution (FWHM) of 18.3, 21.8 and 36.0 keV respectively. The electrodeposition and alpha spectrometry for a natural uranium sample of domestic origin gave $^{238}U : ^{234}U = 1 : 6.1{\times}10^{-5}$ and for a neutron-irradiated uranium sample did $^{238}U : ^{239}Pu : ^{241}Am = 100 : 0.0263 : 5.20{times}10^{-5}$. The result of $^{238}U$ determination in the irradiated sample by electrodeposition-alpha spectrometry was in accord within ${\pm}1.6%$ of relative error with the results of solid fluorimetry and mass spectrometry. For $^{239}Pu$ the result of electrodeposition-alpha spectrometry was in accord within ${\pm}$4.0% of relative error with the results of anion exchange separation and the thenoyltrifluoroacetone(TTA) extraction both followed by alpha spectrometries.

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Phase Equilibria of the System Pd-Sb-Te and Its Geological Implications (팔라듐-안티몬-테루르 계(系)의 상평형(相平衡)과 지질학적(地質學的) 의의(意義))

  • Kim, Won-Sa;Chao, George Y.
    • Economic and Environmental Geology
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    • v.26 no.3
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    • pp.327-335
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    • 1993
  • Phase relations in the system Pd-Sb-Te were investigated at $1000^{\circ}$, $800^{\circ}$, and $600^{\circ}C$, using the sealed-capsule technique; the quenched products were studied by reflected light microscopy, X-ray diffraction, and electron microprobe analysis. At $1000^{\circ}C$, the solid phases Pd, $Pd_{20}Sb_7$, $Pd_8Sb_3$, $Pd_{31}Sb_{12}$, and $Pd_5Sb_2$ are stable with a liquid phase that occupies most of the isothermal diagram. Additional solid phases at $800^{\circ}C$ are $Pd_5Sb_3$, PdSb, $Pd_8Te_3$, $Pd_7Te_3$, and a continuous $Pd_{20}Te_7-Pd_{20}Sb_7$ solid solution becomes stable. At $600^{\circ}$, $PdSb_2$, $Pd_{17}Te_4$, $Pd_9Te_4$, PdTe, $PdTe_2$, $Sb_2Te_3$, and Sb and continuous PdSb-PdTe and $PdTe-PdTe_2$ solid solutions are stable. All the solid phases exhibit solid solution, mainly by substitution between Sb and Te to an extent that varies with temperature of formation. The maximum substitution (at.%) of Te for Sb in the Pd-Sb phases is: 44.3 in $Pd_8Sb_3$, 52.0 in $Pd_{31}Sb_{12}$, 46.2 in $Pd_5Sb_2$ at $800^{\circ}C$; 15.3 in $Pd_5Sb_3$, 68.3 in $PdSb_2$ at $600^{\circ}C$. The maximum substitution (at.%) of Sb for Te in the Pd-Te phases is 34.5 in $Pd_5Sb_3$ at $800^{\circ}C$, and 41.6 in $Pd_7Te_3$, 5.2 in $Pd_{17}T_4$, 12.4 in $Pd_9Te_4$, and 19.1 in $PdTe_2$ at $600^{\circ}C$. Physical properties and X-ray data of the synthetic $Pd_9Te_4$, PdTe, $PdTe_2$, $Pd_8Sb_3$, PdSb, and $Sb_2Te_3$ correspond very well with those of telluropalladinite, kotulskite, merenskyite, mertieite II, sudburyite, and tellurantimony, respectively. Because X-ray powder diffraction data consistently reveal a 310 peak ($2.035{\AA}$), the $PdSb_2$ phase is most probably of cubic structure with space group $P2_13$. The X-ray powder pattern of a phase with PdSbTe composition, synthesized at $600^{\circ}C$, compares well with that of testibipalladite. Therefore, testibiopalladite may be a member of the $PdSb_2-Pd(Sb_{0.32}Te_{0.68})$ solid solution series which is cubic and $P2_13$ in symmetry. Thus the ideal fonnula for testibiopalladite, presently PdSbTe, must be revised to PdTe(Sb, Te). Borovskite($pd_3SbTe_4$) has not been found in the synthetic system in the temperature range $1000^{\circ}-600^{\circ}C$.

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