• 제목/요약/키워드: LaAlO3/SrTiO3

검색결과 43건 처리시간 0.034초

금강하구 표층퇴적물의 지화학적 특성에 관한 연구 (Geochemical Characteristics of Surface Sediments in the Keum River Estuary Adjacent to Coastal Area)

  • 서만석;박영석
    • 수산해양교육연구
    • /
    • 제19권1호
    • /
    • pp.1-7
    • /
    • 2007
  • The purpose of this study was to investigate geochemical characteristics of surface sediments in the Keum river estuary adjacent to coastal area. For this study we collected the 21 surface sediments samples. Mean size of surface samples was $3.24{\sim}6.65{\phi}$ on inner estuary and was $2.15{\sim}3.42{\phi}$ on outside estuary. Surface samples were composed of silt on inner estuary and were composed of sand which was more larger than $4{\phi}$ on outside estuary. Most major elements except CaO, $Na_2O$ showed good relationships between variation of contents and grain size. Contents of $Al_2O_3$, $Fe_2O_3$, MgO, $K_2O$, $TiO_2$, $P_2O_5$ and $M_nO$ were increased predominately owing to the variation of mean size of surface samples. Contents of Co, Cr, Cu, Li, Sr, Zn, La, Ce, Pb, Rb, Nd have a good relationships with grain size but Ba, Th, Sm have not. All of major and minor elements contents except $K_2O$ and Ba were less than world mean contents of shallow surface sediments but apprehend a high pollution possibility on silt sediments in the estuaries.

Oxygen Vacancy Effects of Two-Dimensional Electron Gas in SrTiO3/KNbO3 Hetero Structure

  • Choi, Woo-Sung;Kang, Min-Gyu;Do, Young-Ho;Jung, Woo-Suk;Ju, Byeong-Kwon;Yoon, Seok-Jin;Yoo, Kwang-Soo;Kang, Chong-Yun
    • 센서학회지
    • /
    • 제22권4호
    • /
    • pp.244-248
    • /
    • 2013
  • The discovery of a two-dimensional electron gas (2DEG) in $LaAlO_3$ (LAO)/$SrTiO_3$ (STO) heterostructure has stimulated intense research activity. We suggest a new structure model based on $KNbO_3$ (KNO) material. The KNO thin films were grown on $TiO_2$-terminated STO substrates as a p-type structure ($NbO_2/KO/TiO_2$) to form a two-dimensional hole gas (2DHG). The STO thin films were grown on KNO/$TiO_2$-terminated STO substrates as an n-type structure to form a 2DEG. Oxygen pressure during the deposition of the KNO and STO thin films was changed so as to determine the effect of oxygen vacancies on 2DEGs. Our results showed conducting behavior in the n-type structure and insulating properties in the p-type structure. When both the KNO and STO thin films were deposited on a $TiO_2$-terminated STO substrate at a low oxygen pressure, the conductivity was found to be higher than that at higher oxygen pressures. Furthermore, the heterostructure formed at various oxygen pressures resulted in structures with different current values. An STO/KNO heterostructure was also grown on the STO substrate, without using the buffered oxide etchant (BOE) treatment, so as to confirm the effects of the polar catastrophe mechanism. An STO/KNO heterostructure grown on an STO substrate without BOE treatment did not exhibit conductivity. Therefore, we expect that the mechanics of 2DEGs in the STO/KNO heterostructures are governed by the oxygen vacancy mechanism and the polar catastrophe mechanism.

Temporal variation of magma chemistry in association with extinction of spreading, the fossil Antarctic-Phoenix Ridge, Drake Passage, Antarctica

  • Choe, Won-Hie;Lee, Jong-Ik;Lee, Mi-Jung;Hur, Soon-Do;Jin, Young-Keun
    • 한국지구과학회:학술대회논문집
    • /
    • 한국지구과학회 2005년도 추계학술발표회 논문집
    • /
    • pp.136-141
    • /
    • 2005
  • The K Ar ages, whole rock geochemistry and Sr Nd Pb isotopes have been determined for the submarine basalts dredged from the P2 and P3 segments of the Antarctic-Phoenix Ridge (APR), Drake Passage, Antarctica, for better understanding on temporal variation of magma chemistry in association with extinction of seafloor spreading. The fossilized APR is distant from the known hot spots, and consists of older N-MORB prior to extinction of spreading and younger E-MORB after extinction. The older N-MORB (3.5-6.4 Ma) occur in the southeast flank of the P3 segment (PR3) and the younger E-MORB (1.4-3.1 Ma) comprise a huge seamount at the P3 segment (SPR) and a big volcanic edifice at the P2 segment (PR2). The N-type PR3 basalts have higher Mg#, K/Ba, and CaO/Al2O3 and lower Zr/Y, Sr, and Na8.0 with slight enrichment in incompatible elements and almost flat REE patterns. The E-type SPR and PR2 basalts are highly enriched in incompatible elements and LREE. The extinction of spreading occurring at 3.3 Ma seems to have led to a temporal magma oversupply with E-MORB signatures. Geochemical signatures such as Ba/TiO2, Ba/La, and Sm/La suggest heterogeneity of upper mantle and formation of E-MORB by higher contribution of enriched materials to mantle melting, compared to N-MORB environment. E-MORB magmas beneath the APR seem to have been produced by low melting degree (up to 1% or more) at deeper low-temperature regime, where metasomatized veins consisting of pyroxenites have preferentially participated in the melting. The occurrence of E-MORB at the APR is a good example to better understand what kinds of magmatism would occur in association with extinction of spreading.

  • PDF

New fabrication methods of step-edge Josephson junctions on SrTiO$_3$, MgO, LaAlO$_3$ single crystal substrates for YBa$_2$Cu$_3$O$_7$ thin films by using ion milling technique

  • Moon, Sunk-Yung;Ahn, Jong-Rok;Hwang, Yun-Seok;Lee, Soon-Gul;Choi, Hee-Seok;Kim, Jin-Tae
    • 한국초전도학회:학술대회논문집
    • /
    • 한국초전도학회 2000년도 High Temperature Superconductivity Vol.X
    • /
    • pp.146-150
    • /
    • 2000
  • Two methods have been investigated to fabricate good quality step-edge Josephson junctions on STO, MgO, and LAO single crystal substrates. One is the annealing of substrates at 1050$^{\circ}$C in 1 atmospheric oxygen after Ar-ion milling. The other is the cleaning of step-edge by using Ar ion milling. The step-edge is characterized with atomic force microscope (AFM) images. And YBCO thin films are deposited by using pulsed laser. The I-V properties of step-edge junctions are characterized. The yield rate of step-edge junction is increased by new fabrication methods.

  • PDF

THIN FILM TECHNOLOGIES RELATED TO THE HIGH T$_{c}$ SUPERCONDUCTORS

  • Ri, Eui-Jae
    • 한국표면공학회지
    • /
    • 제29권5호
    • /
    • pp.415-423
    • /
    • 1996
  • Thin film technologies for fabricating SQUIDs involve etching and deposition procedures with the proper substrate materials and $YBa_2Cu_3O_{7-d}$ (YBCO) as the high $T_c$ superconductor. YBCO were prepared on various substrates of MgO, $SrTiO_3$, and $LaAlO_3$ by using off-axis magnetron sputtering methods and annealing in-situ. The parameters of film fabrication processes had been optimized to yield good quality films in terms of the critical temperature $T_c$ and the critical current density $J_c$. The optimized processes yielded $T_C$>90K along with $J_c$>$10_6A$$extrm{cm}^2$ at 77K and>$2\times10_7A/Cm^2$ at 5K. We fabricated step-edge type dc-SQUIDs and directly coupled magnetometers, producing step edges on MgO(100) substrates by etching with Ar-ion beam, depositing YBCO material on them, then patterning them by using ion-milling technique. Circuitizing washer-shape SQUIDs to possess a pair of step-edge junctions of 2-5$\mu$ line width with a high angle>$50^{\circ}C$ , we examined their I-V characteristics thoroughly and Shapiro steps clearly as we irradiate microwaves of 8-20 GHz frequency.

  • PDF

High-$I_c$ single-coat YBCO films prepared by the MOD process

  • Lee, J.W.;Shin, G.M.;Yoo, S.I.
    • 한국초전도ㆍ저온공학회논문지
    • /
    • 제13권4호
    • /
    • pp.22-25
    • /
    • 2011
  • A single-coat $YBa_2Cu_3O_{7-{\delta}}$ (YBCO) film of high critical currents ($I_c$) could be successfully fabricated by optimizing the viscosity of the coating solution in the metal-organic deposition (MOD) process. From a Ba-deficient coating solution (Y: Ba: Cu = 1: 1.5: 3) having the viscosity of 212 $mPa{\cdot}sec$, 0.9 ${\mu}m$-thick single coat YBCO film with the $I_c$ value of 289 A/cm-width ($J_c$ = 3.2 MA/$cm^2$) at 77 K was achievable on the $SrTiO_3$ (STO) substrate, which was superior to that of our previous report for 0.8 ${\mu}m$-thick single coat YBCO film from a stoichiometric coating solution (Y: Ba: Cu = 1: 2: 3) on the $LaAlO_3$ (LAO) substrate. This result might be attributed to denser and more homogeneous microstrcuture in the case of the YBCO film from the Ba-deficient coating solution.

거제도 화산암의 암석학적 연구 (Petrology of the Volcanic Rocks in Geoje Island, South Korea)

  • 윤성효;이준동;이상원;고정선;서윤지
    • 암석학회지
    • /
    • 제6권1호
    • /
    • pp.1-18
    • /
    • 1997
  • 이 연구에서는 한반도 남해안 도서지역중 거제도 일대의 화산암류를 대상으로 암석 기재, 암석화학적 특성을 알아보고, 화산암류의 조구적 위치 및 성인에 대하여 고찰하고자 한다. 본 역의 화산암류는 백악기의 퇴적암층을 기반으로 피복하여 주로 안산암질 화성쇄설암과 용암류가 교호로 누적된 산상 즉, 최하부는 두터운 화산각력암, 응회각력암 및 라필리응회암 누층으로 구성되고, 상부로 감에 따라 상대적으로 안산암 용암류가 라필리응회암과 응회암을 협재하며 빈번하게 노출되고 최상부에는 데사이트-유문암질 용결회류응회암류가 분포한다. 본 역의 화산암류는 주성분 화학조성으로 볼 때, 현무암에서 현무암질안산암, 안산암, 데사이트 그리고 유문암에 이르는 넓은 성분 조성을 하며 전형적인 BAR조합을 나타낸다. 본 역의 화산암류는 칼크-알칼리암계열에 속하며, SiO2에 대한 K2O 성분에서 medium-K의 조성을 나타내고, La, Th 및 Nb 상관도에서 조산대안산암(orogenic andesite)의 영역에 도시된다. 미량원소 함량을 MORB값으로 표준화한 spider diagram에서 Sr, K, Rb, Ba, Th 등이 다른 원소에 비하여 상대적으로 높은 값을 가지는 반면, Nb, P, Ti, Cr의 함량이 낮은, 지판의 침강 섭입에 관련된 대륙연번부/도호의 조구적환경에 관련된 암석들에 나타나는 특징을 잘 나타낸다. 희토류원소를 chondrite로 표준화한 그림에서는 전체적으로 LREEs가 HREEs에 비하여 부화되어 있으며, 현무암에서 현무암질안산암, 안산암, 데사이트 및 유문암으로 감에따라 Eu의 '-'이상이 점진적으로 커지며, 변화패튼이 대체로 평행한 배영을 보여주므로 본 역의 암석들은 동원마그마에서 유래하였음을 알 수 있다. 지구조위치 판별도에서 본 역의 화산암류는 지판이 침강 섭입하는 지판경계부에서 생성된 마그마로부터 유래한 화산암의 조구적 위치 즉 정상적인 대륙연변호(normal continental margin arc)의 영역에 해당한다. 거제도지역의 화산암류는 약 10% 정도의 맨틀물질의 부분용융으로 형성된 현무암질 시원마그마가 생성되어 지각으로 상승하는 과정에서 분별되어 칼크-알칼리 안산암질 마그마가 형성되었으며, 이 마그마로부터 계속 분별결정작용, 동화작용 및 마그마 혼합 등의 과정을 거치면서 다양한 화산암류를 형성한 것으로 해석된다.

  • PDF

Process Characteristics for $YB_{2}Cu_{3}O_{7-d}$ Films Fabricated by Single Target Sputter and Surface Modification Technique

  • Lee, Eue-Jae
    • 한국재료학회지
    • /
    • 제5권5호
    • /
    • pp.598-605
    • /
    • 1995
  • Thin films of $YB_{2}Cu_{3}O_{7-d}$ were prepared on various substrated of MgO(100), $SrTiO_{3}$, and $LaAlO_{3}$ by using off-axis magentron sputtering methods and annealing in-situ. The prarameters of film fabrication processes had been optimized through a "follow the lcoal maxima" strategy to yield good quality films in therms of the critical temperature $T_{c}$ and the critical current density $J_{c}$. Optimizedproecsses employing a plane magndtron and an cylindrical magnetron yielded $T_{c}$>90K along with $J_{c}$$10^{6}$A/$\textrm{cm}^2$ at 77K and > 2${\times}$$10^{7}$A/$\textrm{cm}^2$ at 5K. The sampels, however, showed degradationinthe properties, after chemical etching for fabrication of microbridges with the line width of 2-10 mocrons. In particular, the value of $T_{c}$ for the microbridges of 2microns was as small as 80%. The degradation was strongly dependent on the line width through a formula : $T_{c}$(e)=$T_{c}$)b) [1-a exp(-1000 bL)} where $T_{c}$(e) and $T_{c}$ (b) are the values of $T_{c}$ in the absolute scale measured after and before chemical etching, respectively and L is the line width in mm. By utilizing a best fitting technique, the proper constant values of a and to b were found as exp(-1.2) and 0.22, respectively. This formula was very useful in estimatiing the upper limit of the device operationtemperature.

  • PDF

In Situ Spectroscopy in Condensed Matter Physics

  • Noh, Tae Won
    • 한국진공학회:학술대회논문집
    • /
    • 한국진공학회 2014년도 제46회 동계 정기학술대회 초록집
    • /
    • pp.92-92
    • /
    • 2014
  • Recently, many state-of-art spectroscopy techniques are used to unravel the mysteries of condensed matters. And numerous heterostructures have provided a new avenue to search for new emergent phenomena. Especially, near the interface, various forms of symmetry-breaking can appear, which induces many novel phenomena. Although these intriguing phenomena can be emerged at the interface, by using conventional measurement techniques, the experimental investigations have been limited due to the buried nature of interface. One of the ways to overcome this limitation is in situ investigation of the layer-by-layer evolution of the electronic structure with increasing of the thickness. Namely, with very thin layer, we can measure the electronic structure strongly affected by the interface effect, but with thick layer, the bulk property becomes strong. Angle-resolved photoemission spectroscopy (ARPES) is powerful tool to directly obtain electronic structure, and it is very surface sensitive. Thus, the layer-by-layer evolution of the electronic structure in oxide heterostructure can be investigated by using in situ ARPES. LaNiO3 (LNO) heterostructures have recently attracted much attention due to theoretical predictions for many intriguing quantum phenomena. The theories suggest that, by tuning external parameters such as misfit strain and dimensionality in LNO heterostructure, the latent orders, which is absent in bulk, including charge disproportionation, spin-density-wave order and Mott insulator, could be emerged in LNO heterostructure. Here, we performed in situ ARPES studies on LNO films with varying the misfit strain and thickness. (1) By using LaAlO3 (-1.3%), NdGaO3 (+0.3%), and SrTiO3 (+1.7%) substrates, we could obtain LNO films under compressive strain, nearly strain-free, and tensile strain, respectively. As strain state changes from compressive to tensile, the Ni eg bands are rearranged and cross the Fermi level, which induces a change of Fermi surface (FS) topology. Additionally, two different FS superstructures are observed depending on strain states, which are attributed to signatures of latent charge and spin orderings in LNO films. (2) We also deposited LNO ultrathin films under tensile strain with thickness between 1 and 10 unit-cells. We found that the Fermi surface nesting effect becomes strong in two-dimensions and significantly enhances spin-density-wave order. The further details are discussed more in presentation. This work was collaborated with Hyang Keun Yoo, Seung Ill Hyun, Eli Rotenberg, Ji Hoon Shim, Young Jun Chang and Hyeong-Do Kim.

  • PDF

충주(忠州)-월악산(月岳山)-제천(提川) 화강암류(花崗岩類)의 암석화학적(岩石化學的) 연구(硏究) (Petrochemistry of the Granitic Rocks in the Chungju, Wolaksan and Jecheon Granite Batholiths)

  • 김규한;신윤수
    • 자원환경지질
    • /
    • 제23권2호
    • /
    • pp.245-259
    • /
    • 1990
  • Petrochemical analyses of granitic rocks including trace element, REE and oxygen isotope were carried out to understand petrogenesis of plutonic rocks from the Chungju, Wolaksan and Jecheon granite batholiths, which might be related with tungsten-base metal-fluorite mineralization in the Hwanggangri metallogenic province. Different geochemical characteristics such as major and trace elements were found between Jurassic Daebo granitic rocks (Chungju, Jecheon, Wonju, and Boeun granitic rocks) and Cretaceous Bulgugsa granitic rocks (Wolaksan, Muamsa and Sokrisan granitic rocks). Cretaceous granitoids are characterized by high $SiO_2$and $K_2O$ contents and low $TiO_2$, $Al_2O_3$, MgO and CaO contents. They also have relatively high contents of trace elements(Zn, V, Co, Cr, Sr, and Ba) in comparison with the Jurassic granitoids. (Eu)/($Eu^*$) and $(La/Lu)_{CN}$ ratios of Jurassic plutons vary from 0.78 to 1.13 and from 26.02 to 30.5, respectively, while the ratios of Cretaceous ones range from 0.22 to 0.28 and from 4.42 to 14.2, respectively. The REE patterns of the Cretaceous and Jurassic granitic rocks have quite different Eu anomalies: large negative Eu anomaly in the former, and mild or absent Eu anomaly in the latter. The large Eu negative of Cretaceous granitic rocks are interpreted as a differentiated product of fractional crystallization of granitic magma deduced by Rayleigh fractionation model(Tsusue et al., 1987). Oxygen isotopic compositions of quartz for Daebo and Bulgugsa granitic rocks range from 9.98 to 10.51‰ and from 8.26 to 9.56‰, respectively. The Daebo granitic rocks enriched in $^{18}0$ suggest that the magma be undergone different partial melting processes from the Bulgugsa ones. Of the Bulgugsa granitoids, Wolaksan and Sokrisan mass have different contents of trace elements and ${\delta}\;^{18}0$ values of the silicate minerals, which indicate that they are not from the identical source of magma. Many mineral deposits are distributed in and/or near the Wolaksan and Muamsa granitic rocks, but a few mineral deposits are found in and near the Chungju and Jecheon granite batholiths. It might be depend on geochemisty of the related igneous rocks which have low contents of Ba, Sr, Co, V, Cr, Ni, Zn and high contents of Nb and Y, and on lithology of country rocks such as cabonate and noncarbonate rocks.

  • PDF