Close Packing
-
Upload
drtanilbabu -
Category
Documents
-
view
215 -
download
0
Transcript of Close Packing
-
7/29/2019 Close Packing
1/3
4/13 Close Packing
ww.uwgb.edu/dutchs/Petrology/close_packing.htm
Close Packing
Steven Dutch, Natural and Applied Sciences, University of Wisconsin - Green Bay
First-time Visitors: Please visit Site Map and Disclaimer. Use "Back" to return here.
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.
http://www.uwgb.edu/sitemap.htmhttp://weba.uwgb.edu/http://www.uwgb.edu/sitemap.htmhttp://weba.uwgb.edu/ -
7/29/2019 Close Packing
2/3
4/13
ww.uwgb.edu/dutchs/Petrology/close_packing.htm
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
-
7/29/2019 Close Packing
3/3
4/13 Close Packing
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
http://www.uwgb.edu/dutchs/index.htmlhttp://www.uwgb.edu/dutchs/Petrology/crystal_structures.htmhttp://www.uwgb.edu/dutchs/MPNOTES.HTM