Struktur Kristal
Struktur Kristal
Struktur Kristal
1. Tetrahedral angles
2. Indices of planes
3. Hcp structure
The serious study of solid state physics began with the discovery of x-ray
diffraction by crystals and the publication of a series of simple calculations of
the properties of crystals and of electrons in crystals. Why crystalline solids
rather than nonclystalline solids? The important electronic properties of solids
are best expressed in crystals. Thus the properties of the most important semi-
conductors depend on the crystalline structure of the host, essentially because
electrons have short wavelength components that respond dramatically to the
regular periodic atomic order of the specimen. Noncrystalline materials, no-
tably glasses, are important for optical propagation because light waves have a
longer wavelength than electrons and see an average over the order, and not
the less regular local order itself.
We start the book with crystals. A crystal is formed by adding atoms in a
constant environment, usually in a solution. Possibly the first crystal you ever
saw was a natural quartz crystal grown in a slow geological process from a sili-
cate solution in hot water under pressure. The crystal form develops as identical
building blocks are added continuously. Figure 1 shows an idealized picture of
the growth process, as imagined two centuries ago. The building blocks here
are atoms or groups of atoms. The crystal thus formed is a three-dimensional
periodic array of identical building blocks, apart from any imperfections and
impurities that may accidentally be included or built into the structure.
The original experimental evidence for the periodicity of the structure
rests on the discovery by mineralogists that the index numbers that define the
orientations of the faces of a crystal are exact integers. This evidence was sup-
ported by the discovery in 1912 of x-ray diffraction by crystals, when Laue de-
veloped the theory of x-ray diffraction by a periodic array, and his coworkers
reported the first experimental observation of x-ray diffraction by crystals.
The importance of x-rays for this task is that they are waves and have a wave-
length comparable with the length of a building block of the structnre. Such
analysis can also be done with neutron diffraction and with electron diffraction,
hut x-rays are usually the tool of choice.
The diffraction work proved decisively that crystals are built of a periodic
array of atoms or groups of atoms. With an established atomic model of a crys-
tal, physicists could think much further, and the development of quantum the-
ory was of great importance to the birth of solid state physics. Related studies
have been extended to noncrystalline solids and to quantum fluids. The wider
field is h o w n as condensed matter physics and is one of the largest and most
vigorous areas of physics.
An ideal crystal is constn~ctedby the infinite repetition of idenbcal groups
of atoms (Fig 2) A group is called the basis. The set of mathematical points to
which the basls is attached is called the lattice The lattice in three dimensions
may be defined by three translabon vectors a,, a,, a,, such that the arrange-
ment of atoms in the crystal looks the same when viewed from the point r as
when viewed from every polnt r' translated by an mtegral multiple of the a's:
Here u,, u,, u , are arhitraryintegers. The set of points r' defined by (1)for all
u,, u,, u,defines the lattice.
The lattice is said to be primitive if any two points from which the atomic
arrangement looks the same always satisfy (1)with a suitable choice of the in-
tegers ui.This statement defines the primitive translation vectors a,. There
is no cell of smaller volume than a, .a, x a, that can serve as a building block
for the crystal structure. We often use the primitive translation vectors to de-
fine the crystal axes, which form three adjacent edges of the primitive paral-
lelepiped. Nonprimitive axes are often used as crystal axes when they have a
simple relation to the symmetry of the structure.
We may arrange the origin, wl~ichwe have called the associated lattice point,
so that 0 5 x,, yj, zj 5 1.
(b) (c)
Fieure 3a Latttce nomts of a soam lnmce m two &mensrons AU ~ a r of
s vector? a,,a, are trans-
-
V, = (a, as X a, 1 , (3)
by elementary vector analysis. The basis associated wrth a primitive cellis cdued
a prim~tivebans. No basis contans fewer atoms than a pnmibve basis contains.
Another way of choosing a primitive cell is shown in Fig. 4. This is h o w n to
physicists as a Wigner-Seitz cell.
(c) (e)
Figure 6 (a) A plane of symmetry to the faces of a cube. (b) A diagonal plane of s)rmmehy
in a cube. (c) The three tetrad xes of a cube. (d)Thc four tridaxes of a cube. (e) The six diad axes
of a cube.
symmetry: the pentagons do not fit together to fdl all space, shoulng that we can-
not combmne fwefold point symmetrywith the r e q u e d translational penodicity.
By lattice point group we mean the collection of symmetry operations
which, apphed about a lathce pomt, carry the lattice into itself The possible ro-
tations have been listed. We can have mirror reflecbons m about a plane through
by -r The symmetry axes and symmetry planes of a cube are shown in Fig 6.
Two-DimensionalLattice Types
The lattice in Fig. 3a was d r a m for arbitrary al and as. A general lattice
such as this is known as an oblique lattice and is invariant only under rotation
of .rr and 27r ahout any lattice point. But special lattices of the oblique type can
, 2 d 6 , or under mirror reflection.
he invariant under rotation of 2 ~ 1 32, ~ 1 4or
We m i s t impose restrictive conditions on a, and a% if we want to construct a lat-
tice that will he invariant under one or more of these new operations. There are
four distinct types of restriction, and each leads to what we may call a special
lattice type. Thus there are five distinct lattice types in two dimensions, the
oblique lattice and the four special lattices shown in Fig. 7. Bravais lattice is
the common phrase for a distinct lattice.%e; we say that there are five Bravdrs
lattices in two dimensions.
Triclimc
Monoclinic
Orthorhomb~c
Cubic
Trigonal
Hexagonal
Figure 8 The cubic space lattices. The cells s h m are the conventional cells.
a
Lattice points p e r cell 1 2 4
Volume. primitive cell a3 ZQ
1 3 xa
1 3
Lattice points per unit volume l/a3 2/aR 4/a3
Numher of nearest neighbors 6 8 12
Nearest-neighbor distance a 3u2a/2 = 0.866a a/2'" 0.707a
Number of second neighbors 12 6 6
Second neighbor distance 2'% a a
Packing fractionn ZW &V5 id5
=0.524 =O.B80 =0.740
"The packing fraction is the manirnum proportion of the available volume that can be filled
with hard spheres.
Figore 11 The rhombohedra1 primitive cell of the hce-centered Figore 12 Relation of the plimitive cell
cubic clystal. The primitive translation vectors a,, a,, connen in the hexagonal system (heavy lines) to
the lattice point at the origin with lattice points at the face centers, a prism of hexagonal symmew. Here
As drawn, the primitive vectors are: rr,=o,#a,.
Find the intercepts on the axes in terms of the lattice constants a,, a,, a,.
The axes may be those of a primitive or nonprimibve cell.
Figure I3 This plane intercepts
the a,, +, a, axes at 3a,, Za,, Za,
.,.
The recrprocals of these numbers
, I &
are 5, The smallest three mte-
gers havlng the same rabo are 2, 3,
3, and thus the m&ces of the plane
are (233) I
Take the reciprocals of these numbers and then reduce to three integers
having the same ratio, usually the smallest three integers. The result, en-
closed in parentheses (hkl),is called the index of the plane.
For the plane whose intercepts are 4 , 1 , 2 ,the reciprocals are $, 1,and $: the
smallest three integers having the same ratio are (142).For an intercept at infin-
ity, the corresponding index is zero. The indices of some important plades in a
cubic crystal are illustrated by Fig. 14. The indices (hkl) may denote a single
plane or a set of parallel planes. If a plane cuts an axis on the negative side of the
origin, the corresponding index is negative, indicated hy placing a minus sign
1 Crystal Structure 13
above the index: (hkl). The cube faces of a cubic crystal are (100). (OlO), (OOl),
(TOO),( o ~ o )and
, (001). Planes equivalent by s y m m e q may he denoted by curly
brackets (braces) around indices; the set of cube faces is {100}.When we speak
of the (200) plane we mean a plane parallel to (100) but cutting the a, axis at i n .
The indices [uvw] of a direction in a clystal are the set of the smallest inte-
gers that have the ratio of the components of a vector in the desired direction,
referred to the axes. The a, axis is the [loo] direction; the -a, axis is the [ o ~ o ]
direction. In cubic crystals the direction [hkl] is perpendicular to a plane (hkl)
having the same indices, but this is not generally true in other crystal systems.
separated by one-half the body diagonal of a umt cube There are four units of
NaCl ~neach unit cube, with atoms in tlie pos~tions
Each atom has as nearest neighbors six atoms of the opposire kind. Represen-
tative crystals having the ~ karrangement
l include those in the following
table. The cube edge a is given in angstroms; 1if --cm lo-'' m 0.1
nm. Figure 17 is a photograph of crystals of lead sulfide (PbS) from Joplin,
Missouri. The Joplin specimens form in beautiful cuhes.
.
per primitive cell, with atoms at the comers 000 and body-centered positions
,l -,i -l of the simple cubic space lattice. Each atom may he viewed as at the center
-
Figure 19 A close-packed layer of spheres is shown, with centers at points marked A. A second
and identical layer of spheres can he placed on top of this, above and patallel to the plane of the
drawing, with centen over the points marked B. There are two choices for a third layer. It can go
in over A or over C . Ifit goes in over A, the sequence is AEABAB . . . and the structure is hexagonal
close-packed. If the third layer goes in over C, the sequence is ABCABCABC . . . and the Struchlre
is face-centered cubic.
of a cube of atoms of the opposite kind, $0 that the number of nearest neigh-
bors or coordination number is eight.
Diamond Structure
The diamond structure is the structwe of the semiconductors silicon and
germanium and is related to the structure of several important semicondnctor
binary compouncLs. The space lattice of damond 1s face-centered cubic. The
primitive basis of the diamond structure has two identical atoms at coordinates
000 and 2;; assoc~atedmth each point of the fcc latt~ce,as shown in Fig. 22.
Because the convenbonal unit cube of the fcc lattice contains 4 latbce points,
i t follows that the conven~onalunit cube of the dlamond structure contams
2 X 4 = 8 atoms. There is no way to choose a primitive cell such that the basis
of diamond contains only one atom.
Figure 22 Atomic positions in the cubic cell uf the diamond Figure 23 Crystal structure of diamond,
s t ~ u c h ~projected
rr on a cub? face; fiacticms denote height showingthetetrahedralbondarrangement.
above the hasp in units of a cubc edge. The paints at 0 and $
are on the fcc lattice those at and are on a similar lattice
displvcerl along the body diagonal by one-fourth of its lengh.
With a fcc space lattice, the basis consists of mia identical
atoms at 000 0 d i i ; .
The close equality of the lattice constants of several pairs, notably (Al, Ga)P
and (Al, Ga)As, makes possible the construction of sem~conductorhetemjunc-
tions (Chapter 19).
the ideal crystal is the state of minimum energy of identical atoms at the tem-
perature of absolute zero. At finite temperatures this is likely not to be true. We
give a further example here.
In Table 3 we hst the more common crystal stmctureq and lattlce structures
of the elements Values of the atomic concentration and the density are glven in
Table 4. Many dements occur m several crystal structures and transform from
Table 3 Crystal structures of the elements
.rhe data given are at morn temperature for the most common form, Y.
the stated temperature in deg K. (Inorganic Cr)-stal Stlucture Database
Table 4 Density and atomic concentration
The data are given at atmosphericpressure and mom temperature, or at the
mzg~mr~~~m~eam~s~m~~exsm~rs~vv
more stable.
SUMMARY
. crystal axes.
To form a crystal we attach to every lattice point an identical basis composed
+
of s atoms at the positions r, = xja, y,a, + zja3,withj = 1,2, . . . , s. Here
x, y, z may be selected to have values between 0 and 1.
. The axes a,, a*, a3 are primitive for the minimum cell volume la,. as X a,(
for which the crystal can be constructed from a lattice translation operator T
and a basis at every lattice point.
Problems
1. Tetrahedral angles. The angles behveen the tetrahedral bonds of diamond are the
same as the angles between the body diagonals of a cube, as in Fig. 10. Use elemen-
tary vector analysis to find the value of the angle.
2. Indices of planes. Consider the planes with indices (100) and (001);the lattice is
fcc, and the indices refer to the conventional cubic cell. What are the indices of
these planes when referred to the primitive axes of Fig. II?
3. Hcp structum. Show that the c/a ratio for an ideal hexagonal close-packed struc-
ture is (:)IR = 1.633. If c/a is significantly larger than this value, the crystal structure
may be thought of as composed of planes of closely packed atoms, the planes being
loosely stacked.