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    Close Packing

    Steven Dutch, Natural and Applied Sciences, University of Wisconsin - Green Bay

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    Packing and Interstices

    As shown here,

    identical atoms (or

    any round object, like

    coins or pool balls)

    can be arranged in a

    hexagonal pattern

    where each is

    surrounded by sixneighbors. This is the

    tightest possible

    packing.

    The left diagram shows what happens when we place a second layer (light gray) on top of a lower layer

    (dark gray). Each upper atom nestles into a pocket formed by three other atoms, enclosing a small space

    called an interstice. In this case, the four atoms occupy the corners of a tetrahedron, so the openings are

    called tetrahedral interstices. There are two sets. One is enclosed by an upper atom resting on three below

    (shown in purple). Another consists of a cluster of three upper atoms resting on one below (shown in blue)In both cases the centers of the four atoms are the vertices of a tetrahedron (shown in yellow) but in one

    case the tetrahedron points up, in the other it points down.

    It turns out there are much larger openings between the sheets. A cluster of three upper atoms can also

    rest on a cluster of three lower atoms (shown in red). These six atoms lie at the corners of an octahedron,

    so these openings are called octahedral interstices. In real minerals the close-packed sheets are often

    anions (usually oxygen) with cations in the interstices. Some of the tetrahedral and octahedral interstices

    are shown between the atoms (blue and yellow, respectively)

    On the right is a representation of a pair of close-packed sheets just showing the shapes of the interstices

    Each vertex is the site of an atom. We have a sheet of octahedra (blue top faces) separated by tetrahedra.The top faces of the tetrahedra are omitted and only the downward-pointing tetrahedra are shown. The

    upward-pointing tetrahedra are hidden; their top vertices are located where three octahedra join.

    We can see each octahedron has six atoms, but each atom is shared with three octahedra, so for each

    octahedron there are 6(1/3)=2 atoms. Each upward-pointing tetrahedron can be pictured as sharing the

    three base atoms with three neighbors plus having the top atom to itself, or 3(1/3)+1=2 atoms. The same i

    true for downward-pointing tetrahedra. Thus there are equal numbers of octahedra, upward-pointing

    tetrahedra and downward-pointing tetrahedra, and two atoms for each polyhedron. There are two

    tetrahedra for each octahedron, one upward and one downward.

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    Hexagonal Close Packing

    Top: Identical atoms can be

    packed into a sheet with a

    hexagonal pattern. Anotherlayer can be placed on top in

    one of two ways: over the

    upward-pointing gaps (blue) or

    the downward-pointing gaps

    (yellow). Layers B and C show

    layers in these positions.

    Bottom: If layers alternate

    (left) or are randomly stacked

    (right) the overall structure has

    only the hexagonal symmetry

    of the individual sheets. The

    alternating pattern is called

    Hexagonal close packing. The

    oxygen atoms in corundum and

    hematite have this packing.

    In real crystals the anions often have close packing with the interstices between layers occupied by cation

    Since the cations attract the anion sheets and repel nearby cations, electrical forces tend to produce

    symmetrical arrangements. Thus the regular alternating stacking is favored.

    Cubic Close Packing

    Top: The three possible

    arrangements of close-packed

    atomic layers are shown. Note

    how the three layers also form

    a square lattice of atoms. The

    lattice plane is tilted in this

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    view.

    Bottom: If the layers repeat

    cyclically, cubic close packing

    results. The two right diagrams

    show how a cube can be

    formed by this packing. Oxyge

    atoms in spinel and magnetite

    have this arrangement, as dothe chlorine atoms in halite,

    the sulfur atoms in sphalerite

    and the calcium atoms in

    fluorite.

    The face-centered cubic unit

    cell (F cell) has cubic close

    packing.

    Return to Crustal Materials Index

    Return to Crystal Structures Index

    Return to Professor Dutch's Home Page

    Created 18 September 1998, Last Update 22 September 1999

    Not an official UW Green Bay site

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