Lithium-ion batteries have been considered the most important devices to power mobile or small-sized devices due to their high energy density. LixCoO2 has been studied as a cathode material for the Li-ion battery. However, the limitation of its capacity impedes the development of high capacity cathode materials with Ni, Mn, etc. in them. The substitution of Mn and Ni for Co leads to the formation of solid solution phase LiNixMnyCo1-x-yO2 (NMC, both x and y < 1), which shows better battery performance than unsubstituted LiCoO2. However, despite a high discharge capacity in the Ni-rich compound (Ni > 0.8 in the metal site), poor cycle retention capability still remains to be overcome. In this study, aiming to improve the stability of the physical and chemical bonding, we investigate the stabilization effect of Ca in the Ni-rich layered compound Li(Ni0.83Co0.12Mn0.05)O2, and then Ca is added to the modified secondary particles to lower the degree of cationic mixing of the final particles. For the optimization of the final grains added with Ca, the Ca content (x = 0, 2.5, 5.0, 10.0 at.%) versus Li is analyzed.

이 논문에서는 철근콘크리트 쉘구조의 동적해석을 위한 비선형 유한요소 해법을 제시하였다. 사용된 프로그램은 철근콘크리트 구조물의 해석을 위한 RCAHEST이다. 유한요소로서는 면내회전강성도를 갖는 4절점 평면 쉘요소가 사용되었다. 두께방향에 대한 철근과 콘크리트의 재료성질을 고려하기 위하여 층상화기법이 도입되었다. 재료적 비선형성에 대해서는 균열콘크리트에 대한 인장, 압축, 전단모델과 콘크리트 속에 있는 철근모델을 조합하여 고려하였다. 이에 대한 콘크리트의 균열모델로서는 분산균열모델을 사용하였다. 동적 평형방정식의 해는 HHT법에 의한 수치적분으로 구하였다. 신뢰성 있는 해석결과와 비교를 통하여 이 논문의 제안방법이 철근 콘트리트 쉘구조의 비선형 동적해석에 적합한 방법임을 입증하고자 한다.

This paper is concerned with the vibration control of multi-layer structure for ultra-tall buildings and main tower of large bridge etc. We have modeled the multi-layer structure with the distributed mass system as the lumped mass system of two-degree-of-freedom structure and made experimental equipment. The LQ optimal control theory is applied to the design of the control system. The designed control system is simulated by computer. As a result, the LQ regulator showed good vibration control performance with impact excitation.

리튬2차전지용 양극소재 개발을 위해 Li[L ixM n1-x-yC ry ] O2를 공침법(co-p.ecipitation method)을 적용하여 각각 650℃(CR650)와 850℃(CR850)에서 합성하였다. 리트벨트 구조분석 결과 계산의 정밀도를 나타내는 R 지수값을 보면 Rexp에 대한 Rwp값( Rwp/ Rexp)은 CR650과 CR850의 각각에 대해 19.2%/10.1%과 15.9%/9.76%를 보여주며, Rb값은 각각 10.9%와 8.54%, 그리고 S(GofF)값은 각각 1.9와 1.6으로 계산되었다. 합성된 양극소재는 공간군 R3m의 층상구조(LiMn O2)가 존재하였으며, 전이금속 층 내의 Mn이 Li로 치환되면서(Li[L i13/M n23/] O2) 단사구조(C2/c)의 거대격자(Superlattice) 구조현상도 관찰되었다. 계산된 단위포는 공간군 R3m, CR650이 a=2.8520(2)a, c=14.248(2)a, V=100.40(1)a3이며, CR850은 a=2.8504(1)a, c=14.2371(7)a, V=100.179(8)a3으로 각각 계산되었다. 또한 최종 결정된 화학식은 CR650은 Li[L i0.35M n0.56C r0.09] O2, CR850은 Li[L i0.27M n0.61C r0.13] O2으로 각각 구해졌다.다...다..구해졌다.다...다..

티타늄과 산소의 함량이 서로 다른 4가지의 합성 페롭스카이트형(perovskite-type) 광물((K2La2Tin/O2n+4, n=3, 4, 5, 6; 14/mcm, 14/mmm, I42 m)을 대상으로 리트벨트(Rietveld)구조분석법을 실시하여 결정구조를 밝히고 티타늄함량에 따른 층상형 구조를 연구하였다. 4가지 합성시료에 대하여 구조분석을 실시한결과 대표적인 페롭스카이트형 광물인 토소나이트(taustonite, La1-x //Kx /TiO3, x〈0.4)가 주성분으로 나타났으며 토스나이트내에 12개의 산소를 배위하는 A자리 양이온은 자리점유율에 의해 La3+ 와 K+ /의 치환관계를 보여준다 공간군은 14/mcm, 단위포는 a=5.505(1)~5.510(1)a, c=7.793(1)~7.796(1)a V=236.25~236.66 a3 범위의 값을 갖는다. 구조의 정밀도를 나타내는 R지수를 살펴보면 RB 값은 5.31~9.10 S(GofF)값은 0.86~1.24로 각각 계산되었다. 12배위를 하는 A자리 양이온인 란탄과 산소의 평균거리는 2.755a이고 6배위를 하는 B자리 양이온인 티타늄과 산소의 평균거리는 1.948 a의 결과를 얻었다. 합성된페롭스카이트형 광물의 층상구조가 알려져 있지 않아 시뮬레이션을 통해 구조모델을 결정하였으며 그결과 n=3인 R-38시료에서만 두 종류의 층상 페롭스카이트(La2K2Ti3O10 ) 구조 (A-type: 14/mmm, a=3.8178 a, c=29.9189 a, V=436.04 a3, B-type: 142 m, a =3.8376 a, c=28.023 a, V=412.6 a3)가 존재함을 확인하였으나 다른 시료에서는 토소나이트, 금홍석 외에 새로운 합성광물로 제파이트의 존재를 확인하였다.

FORTRAN program PHYLS was developed to model the structures of 2:1 1M and 2M1 phyllosilicates on the basis of geometrical analyses. Input to PHYLS requires the chemical composition and d(001) spacing of the mineral. The output from PHYLS consists of the coordinates of the crystallographically independent sites in the unit cell, and such structural parameters as the cell dimensions, interaxial angle, cell volume, interatomic distances, and deformation angles of the polyhedra. PHYLS can generate these structural details according to the user's choice of space group and cation configuration. User can choose one of such space groups as C2/m, C2,and C2/c and such cation configurations as random and ordered tetrachedral/octahedral cation configurations. PHYLS simulated the structures of dioctahedral and trioctahedral phyllosilicates having random tetrahedral cation configuration fairly close to the reported experimentally determined structures. In contrast, the simulated structures for ordered tetrahedral cation configurations showed greater deviation from the experimentally determined structures than those for random configurations. However, if the cations were partially ordered and the sizes of the tetrahedra became similar, the simulated PHYLS may be helpful in various investigations on the relationships between structures and physicochemical properties of the phyllosilicates.

Buserties are known to have layer structures with variable C dimension which depended on the nature interlayer catious and contents of water molecular between edge-sharing [MnO6] octabedral layers. Na-, Ca-, Mg-, and Zn-buserties were synthesized in the laboratory and studied for to know the structural states of water molecules and the role of catious in the buserite structures. With lowering the relative humidity(RH), Ca-buserite begins to dehydrate at 27% RH and proceeds further very slowly. Mg- and Zn- buserite also slow dehydration above 2% RH. With gradual ineveasing temperature Ca- and Zn-buserite show abrupt shifting of 10a peak (10a-phare) toward 7a peak. All of 7a-phare are further dehydrated to 5a-phare by further increasing temperature. It suggests that interlayer catious play a crucial role in the dehydration behavious of buserites. Simulation of one-dimensional X-ray diffraction patterns of buserties show that buserites have three layers of water molecules of different types: the very loosely bound and tightly bend waters, instead of two layers that was regarded by previous authers. The very loosely bound water is sited I open space of the interlayer, the loosely bound water is bound on the tightly bound water by hydrogen bond, and the tightly bond water in coodinately bound on the interlayer catious.