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The crystal structure of chalcoaiumite: mechanisms of Jahn-Teller-driven distortion in ~[6]Cu~(2+)-containing oxysalts

机译:硫铝矾石的晶体结构:含〜[6] Cu〜(2+)的含氧盐的Jahn-Teller驱动变形的机理

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The crystal structure of chalcoaiumite, ideally Cu~(2+)Al_4(S0_4)(OH)_(12)(H_2O)_3, monoclinic, P2_1 ,Z= 4: a 10.228(3), b 8.929(3), c 17.098(6) A, β 95.800(11)°, V 1553.6(1.5) A~3, has been refined to R_1= 3.08% for 4,022 unique observed (4σ) reflections collected on a Bruker D8 three-circle diffractometer equipped with a rotating-anode generator, multilayer optics and an APEX-II CCD.detector. In the structure of chalcoaiumite, there is one S site, tetrahedrally coordinated by four O anions, with = 1.472 A. There are four Al sites with site-scattering values in accord with occupancy by Al and distances of 1.898—1.919 A. There is one Cu site occupied by Cu~(2+) and coordinated by six anions in the [4 + 2] arrangement typical for octahedrally coordinated Cu~(2+). The short distance of 2.086 A is in accord with the low degree of bond-length distortion of the Cu octahedron. There are 19 anion sites: 4 sites are occupied by O atoms that are bonded to the S cation, 12 sites are occupied by (OH) groups that bond to all octahedrally coordinated cations, and 3 sites are occupied by (H_2O) groups that are held in the structure solely by hydrogen bonding. The structure of chalcoaiumite consists of interrupted sheets of edge-sharing Al and Cu octahedra of the form [Cu~(2+)Al_4(OH)_(12)]~(2+) that intercalate layers of (SO_4) tetrahedra and (H_2O) groups. Chalcoaiumite is a member of the nickelalumite group.Cu~(2+)ψ6 (ψ = O~(2-), (OH)-, (H_2O)~0) octahedra show a wide range of bond-length distortion away from the holosymmetric arrangement, driven by spontaneous symmetry-breaking of the degenerate electronic ground-state in holosymmetric octahedral coordination. Here, we examine the structural mechanisms that allow large octahedron distortions of this type. There are two mechanisms: (1) coupling of (usually parallel) octahedron distortions to a vibrational phonoh, inducing a (often ferroelastic) phase transition in M~(2+)-Cu~(2+) solid-solutions; (2) cooperative orientational disorder, where bond topology (polyhedron linkage) allows large differences in bond lengths within polyhedra to accord with the valence-sum rule of bond-valence theory.
机译:铝矾土的晶体结构,理想的是Cu〜(2+)Al_4(S0_4)(OH)_(12)(H_2O)_3,单斜晶,P2_1 / n,Z = 4:a 10.228(3),b 8.929(3) ,c 17.098(6)A,β95.800(11)°,V 1553.6(1.5)A〜3,已对配备有Bruker D8三圆衍射仪的4,022个独特观察到的(4σ)反射进行了精修,使R_1 = 3.08%带有旋转阳极发生器,多层光学器件和APEX-II CCD检测器。在硫铝矾石的结构中,有一个S位点,由四个O阴离子四面体配位, = 1.472A。有四个Al位点的位点散射值与Al和距离1.898-1.919A。在典型的八面体配位Cu〜(2+)的[4 + 2]排列中,有一个Cu位被Cu〜(2+)占据,并由六个阴离子配位。较短的距离为2.086 A,这与Cu八面体的键长畸变程度低相符。有19个阴离子位点:与S阳离子键合的O原子占据4个位点,与所有八面体配位阳离子键合的(OH)基团占据12个位点,由(H_2O)基团占据3个位点仅通过氢键保持在结构中。硫矾铝石的结构由边缘共享的Al和Cu八面体的断续片组成,形式为[Cu〜(2+)Al_4(OH)_(12)]〜(2+),插层了(SO_4)四面体和( H_2O)组。铝矾土是镍铝矾土族的成员.Cu〜(2+)ψ6(ψ= O〜(2-),(OH)-,(H_2O)〜0)八面体的键长畸变范围较宽整体对称的排列,由简并八面体配位的简并电子基态的自发对称破坏驱动。在这里,我们研究了允许这种类型的大八面体变形的结构机制。有两种机理:(1)将(通常是平行的)八面体畸变耦合到振动声子上,从而在M〜(2 +)-Cu〜(2+)固溶体中引起(通常是铁弹性)相变; (2)合作取向障碍,其中键拓扑(多面体链接)允许多面体中键长的较大差异符合键价理论的价和规则。

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