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17plane groups

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Title: 17plane groups


1
17-plane groups
  • When the three symmetry elements, mirrors,
    rotation axis and glide planes are shown on the
    five nets, 17-plane groups are derived.

2
17-plane groups
3
17-plane groups
4
17-plane groups
5
17-plane groups
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17-plane groups
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17-plane groups
8
17-plane groups
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17-plane groups
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17-plane groups
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17-plane groups
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17-plane groups
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17-plane groups
14
17-plane groups
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17-plane groups
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17-plane groups
17
17-plane groups
18
17-plane groups
19
The 14 Bravavis Lattices.
  • There are 14 ways to combine to stack the 5 nets
    in 3D to give us 14 unique ways to translate a
    point in 3 dimensions.

20
The 14 Bravavis Lattices.
  • Stacking of the five nets (plane lattices) in
    various ways leads to the 14-possible lattices.
    These 14 lattices types are known as 14-Bravais
    lattices.
  • The orthogonallity gained by the use of these
    (14-Bravais lattices) is of considerable aid in
    visualizing and describing space lattices.
  • Multiple cells have lattice points on their
    faces, interiors (body), and their corners
  • Cells with interior points are calledBody
    centered lattice (I) or (R) space lattice
  • Cells with Face centered lattice are called
    A-B-C-or F-centered space lattice.

21
The 14 Bravais Lattices
  • When we add a third translation t3 to the 17
    plane groups, we only get 14 space lattice that
    are know as 14 Bravais Lattices.

22
The 14 Bravais Lattices
  • Monoclinic and Triclinic

23
The 14 Bravais Lattices
  • Tetragonal

24
The 14 Bravais Lattices
  • Orthorhombic

25
The 14 Bravais Lattices
  • Cubic

26
The 14 Bravais Lattices
  • The 14 Bravais Lattices can also be grouped into
    6(7) groups that are known as Crystal systems.

27
The 6 (7) Crystal Systems
  • The seven crystal systems will be very important
    in our discussion of optical properties (and
    other physical properties) of crystals and in our
    discussion of phase transitions. You must know
    this table very well.

28
Relation between, Crystal System, Space and Plane
Lattices.
29
The Six Crystal Systems
30
The Six Crystal Systems
31
The 32 Crystallographic Point Groups
  • There are 32 ways to combine the symmetry
    elements, 1, -1, m, 2, 3, 4, and 6 that are
    internally consistent. Each combination is
    called a point group.
  • The 32 point groups fall into the seven different
    crystal systems. These you must know.

32
Significance of the Unit Cell Point Groups
  • The External symmetry of the crystal will have
    the same symmetry as the Unit Cell. (Note The
    form of shape of the crystal may be different
    from that of the unit cell, however).

33
Summary
  • The 14 Bravais Lattices
  • The 6 (7) Crystal Systems
  • The 32 Point Groups (Crystal Classes)

34
Summary
  • The 32 point groups are combinations of
    inversion, rotation and mirrors
  • If in addition, we allow glide and screw we come
    up with 230 space groups and form the basis of
    mineralogical description.

35
Summary
  • Space Groups, therefore reflect the point group
    and lattice type. Space group notation includes
    reference to both.

36
Summary
  • P432 primitive, 4-fold, 3-fold, 2-fold, isometric
  • In as much as X-ray work is needed to determine
    space groups we will not dwell on it here.

37
Relation of the crystal lattice to the crystal
  • A) The 32 crystal classes (point groups)
    correspond to 32 unique combinations of symmetry
    elements (n, m, i).
  • B) From observations of natural crystals find
    that only 32 possible combinations of symmetry
    elements are needed to describe their morphology.
    (Calcite overhead)

38
Relation of the crystal lattice to the crystal
  • Infer
  • A) That crystal morphology is an expression of
    the point group (crystal class).
  • B) The plane surfaces that bound natural
    crystals develop parallel to certain sets of net
    planes in the crystal lattice of a specific
    mineral.

39
Summary
  • 1. morphology tells us of point group (crystal
    class).
  • 2. crystal class tells us of crystal system (iso,
    ortho, mono, etc.)
  • 3. Crystal system specifies certain possible
    lattices (P, I, F, R etc.)
  • 4. X-rays needed to identify lattice type.

40
Summary
  • But even without x-rays we have learned a lot!
    We can break down miriads of crystals into 32
    crystal classes, and these into 6 (7) crystal
    systems.
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