for the discovery of quasicrystals

We report herein the existence of a metallic solid which diffracts electrons like a single crystal but has point group symmetry $m \bar{35}$ (icosahedral) which is inconsistent with lattice translations.(2)
A crystal is a substance in which the constituent atoms, molecules, or ions are packed in a regularly ordered, repeating three-dimensional pattern.So the discover of Shechtman and collegues was very important: they introduce a new class of crystals, named quasicrystals by Levine and Steinhardt some weeks later(3), and a new way to view crystals.
In particular Shechtman, studying Al with 10–14% Mn, and collegues observed that
The symmetries of the crystals dictate that several icosahedra in a unit cell havedifferent orientations and allow them to be distorted (...)(2)And when they observe crystal using lattice translations:
crystals cannot and do not exhibit the icosahedral point group symmetry.(2)They also oserve that the formation of the icosahedral phase is a transition phase of the first order, because the two phases (the other is translational) coexist for a while during translation(2).
Indeed we can define the coordinate system of the solid in the following way(4): \[(\pm u, \pm v, 0); \; (0, \pm u, \pm v); \; (\pm v, 0, \pm u)\] where \[\frac{v}{u} = \tau - 1\] with $\tau$ golden ratio.
So the elements of the icosahedral point groups are the symmetry transformations that permutate icosahedral vertices. With this definition, we can distinguish between two different icosahedral gruop, $235 [I]$ that contains all rotations which leave the icosahedron invariant, and $2/M \bar{35} [I_h]$, the group of Al with 10–14% Mn, that contains 120 elements.
This group is the direct product of the icosahedral group $235 [I]$ and the group consisting of the identity and spatial inversion.(4)The four generators of the group can be represented with the following matrices: \[D [2 (12)] = \begin{pmatrix} -1 & 0 & 0 \\ 0 & -1 & 0 \\ 0 & 0 & 1 \end{pmatrix}\] \[D [3 (143)] = \begin{pmatrix} 0 & 0 & 1 \\ 1 & 0 & 0 \\ 0 & 1 & 0 \end{pmatrix}\] \[D [5 (1-12)] = \begin{pmatrix} 0.5 & -0.5 \tau & \frac{0.5}{\tau} \\ 0.5 \tau & \frac{0.5}{\tau} & -0.5 \\ \frac{0.5}{\tau} & 0.5 & 0.5 \tau \end{pmatrix}\] \[D [\bar{1}] = \begin{pmatrix} -1 & 0 & 0 \\ 0 & -1 & 0 \\ 0 & 0 & -1 \end{pmatrix}\]
Facts about quasicrystals and icosahedrons:
Disorderly quasicrystals
Icosahedral group
Easter Is a Quasicrystal
Nobel Prize in Chemistry: Further readings
(1) de Bruijn, N. (1981). "Algebraic theory of Penrose's non-periodic tilings of the plane". Nederl. Akad. Wetensch. Proc A84: 39.
(2) Shechtman, D., Blech, I., Gratias, D., & Cahn, J. (1984). Metallic Phase with Long-Range Orientational Order and No Translational Symmetry Physical Review Letters, 53 (20), 1951-1953 DOI: 10.1103/PhysRevLett.53.1951
(3) D. Levine, R. Steinhardt (1984) ―Quasicrystals: a new class of ordered structures‖, Physical Review Letters 53(26), pp 2477-2480.
(4) Litvin, D. (1991). The icosahedral point groups Acta Crystallographica Section A Foundations of Crystallography, 47 (2), 70-73 DOI: 10.1107/S0108767390010054
No comments:
Post a Comment
Markup Key:
- <b>bold</b> = bold
- <i>italic</i> = italic
- <a href="http://www.fieldofscience.com/">FoS</a> = FoS