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Lecture 12 (10/30/2006) Crystallography Part 5: Internal Order and 2-D Symmetry Plane Lattices Planar Point Groups Plane Groups
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Internal Order and Symmetry Repeated and symmetrical arrangement (ordering) of atoms and molecules in minerals creates a 3-dimensional lattice array Arrays are generated by translation of a unit cell – smallest unit of lattice points that define the basic ordering Spacing of lattice points (atoms) are typically measured in angstroms (=10 -8 cm); scale of ionic radii
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Two-Dimensional Plane Lattice Translation in two directions: x and y axes Angle between axes: Translation distance: a along x and b along y Replacing motifs with points (or nodes) creates a plane lattice Generating an 2D Lattice Array (Plane Lattice) involves translation of a motif in two directions; non-unique Unit Cell
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5 Types of Plane Lattices Preferred
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Defining a Unit Cell Choose: Smallest Most orthogonal Most in line with symmetry 2 Nodes per Lattice Vector Most Primitive (non-centered)
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Symmetry Elements of Planar Motifs 10 Possible symmetry combinations; called Planar Point Groups Same limitations of rotational symmetries (1,2,3,4, & 6) as Point Groups (crystal classes)
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Symmetry Elements of Plane Lattices glide line
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17 Plane Groups
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