• 제목/요약/키워드: crystallographic group

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cis,fac-Dibromooxotris(2,6- dimethylphenyl isocyanide)molybdenum (IV), cis,fac-$[Mo(O)Br_2(CN-C_6H_3-2,6-Me_2)_3]$의 분리 및 구조 (Isolation and Structure of cis,fac -Dibromooxotris(2,6-dimethylphenyl isocyanide)molybdenum(IV), cis,fac-$[Mo(O)Br_2(CN-C_6H_3-2,6-Me_2)_3]$)

  • 이범준;한원석;이순원
    • 한국결정학회지
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    • 제13권2호
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    • pp.82-85
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    • 2002
  • cis,cis,trans-[MoBr/sub 2/(CO)/sub 2/(PPh/sub 3/)/sub 2/]와 2,6-dimethylphenyl isocyanide의 반응으로부터 화합물cis,fac-[Mo(O)Br/sub 2/,(CN-C/sub 6/H/sub 3/,-2,6-Me/sub 2/)sub 3/] (1)이 분리되었다. 화합물 1의 구조가 분광학적 방법(/sup 1/H-NMR, /sup 13/C{/sup 1/H}-NMR, IR) 및 X-ray 회절법으로 규명되었다. 화합물 1의 결정학 자료: 삼사정계 공 간군 P(equation omitted), a=9.172(2) (equation omitted), b = 11.550(3) (equation omitted), c = 15.106(3) (equation omitted), α = 100.44(2)°, β= 107.12(2)°, γ= 107.83(1)°, Z = 2, R(wR/sub 2/) = 0.0529(0.1344).

Single-Crystal Structure of |Li50Na25|[Si117Al75O384]-FAU

  • Kim, Hu Sik;Suh, Jeong Min;Kang, Jum Soon;Lim, Woo Taik
    • 대한화학회지
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    • 제57권1호
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    • pp.12-19
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    • 2013
  • The single-crystal structure of fully dehydrated partially $Li^+$-exchanged zeolite Y, ${\mid}Li_{50}Na_{25}{\mid}[Si_{117}Al_{75}O_{384}]$-FAU, was determined by single-crystal synchrotron X-ray diffraction techniques in the cubic space group $Fd\bar{3}m$ at 100(1) K. Ion exchange was accomplished by flowing stream of 0.1 M aqueous $LiNO_3$ for 2 days at 293 K, followed by vacuum dehydration at 623 K and $1{\times}10^{-6}$ Torr for 2 days. The structure was refined using all intensities to the final error indices (using only the 801 reflections with ($F_o$ > $4{\sigma}(F_o)$) $R_1/R_2=0.043/0.140$. The 50 $Li^+$ ions per unit cell are found at three different crystallographic sites. The 19 $Li^+$ ions occupy at site I' in the sodalite cavity: the $Li^+$ ions are recessed 0.30 ${\AA}$ into the sodalite cavity from their 3-oxygens plane (Li-O = 1.926(5) ${\AA}$ and $O-Li-O=117.7(3)^{\circ}$). The 20 $Li^+$ ions are found at site II in the supercage, being recessed 0.23 ${\AA}$ into the supercage (Li-O = 2.038(5) ${\AA}$ and $O-Li-O=118.7(3)^{\circ}$). Site III' positions are occupied by 11 $Li^+$ ions: these $Li^+$ ions bind strongly to one oxygen atom (Li-O = 2.00(8) ${\AA}$). About 25 $Na^+$ ions per unit cell are found at four different crystallographic sites: 4 $Na^+$ ions are at site I, 5 at site I', 12 at site II, and the remaining 4 at site III'.

Crystallographic Analysis of Ar Encapsulate within Cs3-A Zeolite

  • Lim, Woo Taik;Kim, Bok Jo;Park, Jong Sam;Chang, Chang Hwan;Jung, Sung Wook;Heo, Nam Ho
    • 분석과학
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    • 제15권6호
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    • pp.540-549
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    • 2002
  • The arrangement of encapsulated Ar atoms in the molecular-dimensioned cavities of fully dehydrated zeolite A of unit-cell composition $Cs_3Na_8HSi_{12}Al_{12}O_{48}$ ($Cs_3$-A) has been studied crystallographically to probe the confinement effect of guest species in microporous environment. Atoms of Ar were encapsulated in the cavities of $Cs_3$-A by treatment with 410 atm of Ar at $400^{\circ}C$ for two days, followed by cooling at room temperature. The crystal structure of $Cs_3Na_8H$-A(4Ar) ($P_e$ = 410 atm, $a=12.245(2){\AA}$, $R_1=0.0543$, and $R_2=0.0552$) has been determined by single crystal X-ray diffraction technique in the cubic space group $Pm\bar{3}m$ at 21 (1) $^{\circ}C$ and 1 atm. Encapsulated Ar atoms are distributed in three crystallographic distinct positions: 1.5 Ar atoms per unit cell opposite 6-rings, 1.5 opposite four-rings in the large cavity, and finally 1.0 in the sodalite-unit. The possible structures of argon clusters, such as $Ar_2$, $Ar_3$, and $Ar_4$, are proposed.

Crystal Structure of Dehydrated $Rb^{+}$-Exchanged Zeolite X, $Rb_{71}Na_{21}Si_{100}Al_{92}O_{384}$

  • 이석희;김양;김덕수;Karl Seff
    • Bulletin of the Korean Chemical Society
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    • 제19권1호
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    • pp.98-103
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    • 1998
  • The crystal structure of dehydrated $Rb^+$-exchanged zeolite X, stoichiometry $Rb_{71}Na_{21}-X\; (Rb_{71}Na_{21}Si_{100}Al_{92}O_{384})$ per unit cell, has been determined from single-crystal X-ray diffraction date gathered by counter methods. The structure was solved and refined in the cubic space group Fd3, a=25.007(3) Å at 21(1) ℃. The crystal was prepared by ion exchange in a flowing stream using a 0.05 M aqueous RbOH solution (pH=12.7). The crystal was then dehydrated at 360 ℃ and $2{\times}10^{-6}$ torr for two days. The structure was refined to the final error indices, $R_1=0.047$ and $R_2=0.040$ with 239 reflections for which I> 3σ(I). In this structure, 71 $Rb^+$ ions per unit cell are found at six different crystallographic sites and 21 $Na^+$ ions per unit cell are found at two different crystallographic sites. Four and a half $Rb^+$ ions are located at site Ⅰ, the center of the hexagonal prism. Nine $Rb^+$ ions are found at site Ⅰ' in the sodalite cavity (Rb-O=2.910(15) Å and O-Rb-O=78.1(4)°). Eighteen $Rb^+$ ions are found at site Ⅱ in the supercage (Rb-O=2.789(9) Å and O-Rb-O=92.1(4)°). Two and a half $Rb^+$ ions, which lie at site Ⅱ', are recessed ca. 2.07 Å into the sodalite cavity from their three O(2) oxygen planes (Rb-O=3.105(37) Å and O-Rb-O=80.6(5)°). Thirty-two $Rb^+$ ions are found at site Ⅲ deep in the supercage (Rb-O=2.918(12) Å and O-Rb-O=71.9(4)°), and five $Rb^+$ ions are found at site Ⅲ'. Seven $Na^+$ ions also lie at site Ⅰ. Fourteen $Na^+$ ions are found at site Ⅱ in the supercage (Na-O=2.350(19) Å and O-Na-O=117.5(6)°).

Chemistry and Crystallographic Studies of Metal Ion Exchanged Zeolite X. Ⅰ. The Crystal Structure of Fully Dehydrated and Fully $K^+$-Exchanged Zeolite X, $K_{92}$-X

  • 장세복;김양
    • Bulletin of the Korean Chemical Society
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    • 제16권6호
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    • pp.539-542
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    • 1995
  • The crystal structure of K92-X (K92Al92Si100O384), a=25.128(1) Å, dehydrated at 360 ℃ and 2X 10-6 Torr, has been determined by single-crystal X-ray diffraction techniques in the cubic space group Fd&bar{3} at 21(1) ℃. The structure was refined to the final error indices R1=0.044 and Rw=0.039 with 242 reflections for which I<3σ(I). In this structure, ninety-two K+ ions are located at the five different crystallographic sites. Sixteen K+ ions are located at the centers of the double six rings (site I; K(1)-O(3)=2.65(2) Å and O(3)-K(1)-O(3)=92.0(6)°). About twelve K+ ions lie at site I' in the sodalite cavity opposite double six rings (D6R's) and these K+ ions are recessed ca. 1.62 Å into the sodalite cavity from their O(3) plane (K(2)-O(3)=2.74(2) Å, O(3)-K(2)-O(3)=88.5(8)°). About thirty-two K+ ions are located at the site II in the supercage and these K+ ions are recessed ca. 1.20 Å into the supercage from their O(2) plane (K(3)-O(2)=2.64(2) Å, and O(2)-K(3)-O(2)=101(1)°). About twenty-two K+ ions lie at the site III in the supercage opposite 4-ring ladder and the remaining ten K+ ions lie at the site III' near the 4-ring ladder in the supercage (K(4)-O(4)=2.88(3) Å, O(4)-K(4)-O(4)=79.8(9)°, K(5)-O(4)=2.8(2) Å, and O(4)-K(5)-O(4)=68(5)°).

X-ray Crystallographic Study of Archaerhodopsin

  • Enami, Nobuo;Okumura, Hideo;Kouyama, Tsutomu
    • Journal of Photoscience
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    • 제9권2호
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    • pp.320-322
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    • 2002
  • Archaerhodopsin (aR), a light-driven proton pump found in HaIonubrum sp. aus-l, was crystallized into an octahedral crystal belonging to the space group P4$_3$2$_1$2. It is shown that aR is composed of7 helical segments and an anti-para1leI ${\beta}$ sheet. The main-chain sIrudure of aR is nearly identical to that of bacteriorhodopsin, but a significant structural difference is observed in the protein surface, especially at lipid binding sites.

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Mineral Carbonation 원료용 수활석 전처리에 대한 연구 (A Study on Pretreatment of Brucite for Mineral Carbonation)

  • 최원경;문승현;조태환;이재근
    • 한국수소및신에너지학회논문집
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    • 제16권3호
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    • pp.277-283
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    • 2005
  • Pretreatment procedure was investigated into brucite powders for mineral carbonation materials. Higher magnesium content was found from brucite powders and weight loss due to hydroxy group(-OH) elimination, explained by FT-IR spectra, was found after pretreatment. X-ray diffraction results showed that the crystallographic changing of brucite into magnesium oxides during pretreatment. XPS core spectra also showed chemical transformation of magnesium ingredient from hydroxides to oxide.

Preliminary X-ray Studies of a New Crystal form of 28 kDa Clonorchis sinensis Glutathione S-Transferase

  • Cho, Youn-Hye;Kim, Young-Kwan;Kim, Seung-Joon;Hong, Seong-Jong;Chung, Yong-Je
    • 한국결정학회지
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    • 제16권2호
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    • pp.138-140
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    • 2005
  • A new crystal of helminth glutathione S-transferase, 28 kDa isozyme from Clonorchis sinensis has been grown from a 20% PEG MME 550 solution containing 50 mM $CaCl_{2}$ in 0.1 M bis-Tris buffer (pH 6.5) in $2{\sim}3$ days. The crystals diffract to $3.0{\AA}$ resolution and belong to the orthorhombic space group $P2_{1}2_{1}2_{1}$ with cell parameters $a=62.58{\AA},\;b=69.92{\AA},\;and\;c=339.67{\AA}$.

Vanadium Haloperoxidase의 구조와 작용 메커니즘과 해양천연물질 (Reaction Mechanism of Vanadium Haloperoxidase and Marine Natural Products)

  • 한재홍
    • 한국결정학회지
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    • 제16권2호
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    • pp.66-74
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    • 2005
  • 다양한 생리활성을 가지는 marine natural products는 일반적인 secondary metabolites와 유사한 구조를 가지는데, 염소, 브롬, 요오드의 할로겐 원소에 의해 수식이 되어있는 것이 일반적이다. Vanadium haloperoxidase는 이러한 marine natural products의 생산에 중요한 효소로 vanadate를 조효소로 하는 금속효소이다. 본 리뷰에서는 vanadium haloperoxidase의 분리와 단백질 구조를 살펴보고, 이 금속효소의 작용기작에 대해서 설명할 것이다. 마지막으로, vanadium haloperoxidase의 반응성과 secondary metabolites 중 indole, terpenoids, acetogenins의 생합성 예를 살펴볼 것이다.

INFRA-NILMANIFOLDS AND THEIR FUNDAMENTAL GROUPS

  • Dekimpe, Karel;Igodt, Paul;Malfait, Wim
    • 대한수학회지
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    • 제38권5호
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    • pp.883-914
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    • 2001
  • We present a survey of research results obtained for infra-nilmanifolds, their fundamental groups and some of their generalizations. This is presented from two different approaches and covers achievements obtained during the past four decades and showing a remarkable amount of mathematical interdisciplinarity. We go more in depth concerning the existence and construction of polynomial structures for these manifolds and groups, a direction where significant progress was made in the past few years. The bounded-degree polynomial structures developed by the authors triggered a number of challenging open problems. Also, their study already has lead to some interesting results concerning e.g. Anosov diffeomorphisms and expanding maps.

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