cubic cell.
Each
cubic cell has four lattice points associated withit, eachrhombohedral
cell has one,and
theformer
has, correspondingly, four times thevolume
of the latter.Never-theless, it is usually
more
convenient touse the cubic cell ratherthan
therhombohedral
one because the formerimmediately
suggests the cubicsymmetry which
the lattice actually possesses. Similarly, the other cen-tered nonprimitive cells listed inTable
2-1 are preferred to the primitive cells possible intheir respective lattices.Ifnonprimitive lattice cells are used, the vector
from
the origin toany
point in the lattice willnow have components which
are nonintegralmul-tiples oftheunit-cellvectors a,b, c.
The
position ofany
lattice point in acell
may
be given interms
of itscoordinates] if the vectorfrom
the origin of the unit cell to the given point hascomponents
xa, yb, zc,where
x, y,and
z are fractions, then the coordinates of the point are xyz.Thus,
pointA
inFig. 2-7,taken
astheorigin, has coordinates000
while points Bj C,and D, when
referred to cubic axes,have
coordinatesOff,
f f,and f f
0, respectively. PointE
has coordinatesf \
1and
is equivalent FIG. 2-7. Face-centered cubicpoint lattice referred to cubic and rhombo-hedral cells.2-6]
LATTICE DIRECTIONS AND PLANES
37 to point Z), being separatedfrom
itby
the vector c.The
coordinates of equivalent points in different unit cellscan always
bemade
identicalby
the addition or subtraction of a set of integral coordinates; in this case, subtraction of 1from f
^ 1 (the coordinates ofE)
gives^ f
(the coordinates of D).Note
that the coordinates of a body-centered point, for example, arealways
| ^^ no matter whether
the unitcellis cubic, tetragonal, or ortho-rhombic,and whatever
its size.The
coordinates ofa point position, such as^ ^
\,may
alsobe regardedasan
operator which,when
"applied" to a point at the origin, willmove
or translate it to the position \\
\, the final position being obtainedby
simple addition of the operator\ \ \ and
the original position000.
In this sense, the positions000, \ \ \
are called the "body-centering translations," since they willproduce
thetwo
point positions characteristic of a body-centered cellwhen
applied to a pointatthe origin. Similarly, the four pointpositions characteristic ofa face-centered cell,namely
0, \ ^, \ ^,and
\\
0, are called the face-centering translations.The
base-centering translationsdepend on which
pair of opposite faces are centered; if centeredon
theC
face, for example, they are 0, \ \0.2-6
Lattice directionsand
planes.The
direction ofany
line in alat-tice
may
be describedby
firstdrawing
a linethrough
the origin parallel to the given lineand
then giving the coordinates ofany
pointon
the linethrough
the origin. Let the line passthrough
the origin of the unit celland any
pointhaving
coordinatesu
vw,where
thesenumbers
arenot neces-sarily integral. (This line will also passthrough
the points2u
2v2w,3u
3v3w, etc.)Then
[uvw], written in square brackets, are the indices of the direction of the line.They
are also the indices ofany
line parallel to the given line, since the lattice is infiniteand
the originmay
betaken
at
any
point.Whatever
the values of i/, v, w, theyarealways
converted toasetofsmallest integersby
multi-plication or divisionthroughout:thus,
[||l],
[112],and
[224] all represent thesame
direction, but [112] is the preferred form.Negative
indices are written with a bar over thenumber,
e.g.,[uvw]. Directionindicesare illus-trated in Fig. 2-8.
Direction^related
by symmetry
arecalled directions ofa form,
and
a set ofthese are|Pepresentedby
theindicesof
one
ofthem
enclosed in angularbracHts;
for example, the fourbody
Fib/^-8.[100]
38
THE
[CHAP.diagonals of a cube, [111], [ill], [TTl],
and
[Til],may
all be representedby
thesymbol
(111).The
orientation of planes in a latticemay
also be representedsym-bolically,accordingtoa
system
popularizedby
the English crystallographer Miller. In the general case, the given planewill be tilted with respect to the crystallographic axes, and, since these axesform
a convenientframe
of reference,
we might
describe the orientation of the planeby
giving the actual distances,measured from
the origin, atwhich
it intercepts the three axes. Better still,by
expressing these distances as fractions of the axial lengths,we
can obtainnumbers which
areindependent
of the par-ticular axial lengths involved in the given lattice.But
a difficulty then ariseswhen
the given plane is parallel to a certain crystallographic axis, because such a plane does not intercept that axis, i.e., its "intercept" can onlybe
described as "infinity."To
avoid the introduction of infinityinto the description of plane orientation,we
can use the reciprocal of the frac-tional intercept, this reciprocal being zerowhen
the planeand
axis areparallel.
We
thusarrive at aworkable symbolism
for the orientation of a plane in alattice, the Miller indices,which
are defined as thereciprocals of thefractional intercepts which the planemakes
with the crystallographic axes.For
example, if the Miller indices of a plane are (AW), written in paren-theses, then the planemakes
fractional intercepts of I/A, I/A*, \/l with the axes,and, ifthe axiallengths are a, 6, c, the planemakes
actual intercepts ofa/A, b/k, c/l, asshown
in Fig. 2-9(a). Parallel toany
plane inany
lat-tice, thereis a
whole
set ofparallelequidistant planes,one
ofwhich
passesthrough
the origin; the Miller indices (hkl) usually refer to that plane in thesetwhich
isnearest the origin, although theymay
be taken as referring toany
other plane in theset or to thewhole
settaken
together.We may
determine the Miller indices of the planeshown
in Fig. 2-9(b) as follows:1A 2A 3A 4A
(a) (b)
FIG. 2-9. Plane designationbyMillerindices.
2-6]
LATTICE DIRECTIONS AND PLANES 39
Miller indices are
always
cleared of fractions, asshown
above.As
stated earlier, ifa plane isparallelto a given axis, its fractional intercepton
that axis istaken
as infinityand
the corresponding Miller index is zero. If a plane cuts a negative axis, the corresponding indexis negativeand
is writ-tenwith
a bar over it. Planeswhose
indices are the negatives ofone
another are paralleland
lieon
oppositesides of the origin, e.g., (210)and
(2lO).
The
planes (nhnk
nl) are parallel tothe planes (hkl)and have 1/n
thespacing.The same
planemay
belong totwo
different sets, the Miller indices ofonesetbeing multiplesofthoseoftheother;thus thesame
plane belongs to the (210) setand
the (420) set, and, in fact, the planes of the (210) setform
every second plane in the (420) set. jjn the cubic system,it is convenient to
remember
that a direction [hkl] isalways
perpendicular to a plane (hkl) of thesame
indices,but
thisis not generally true in other systems.Further
familiarity with Miller indices canbe
gainedfrom
astudy
of Fig. 2-10.A
slightly differentsystem
of plane indexing isused
in the hexagonal system.The
unit cell of a hexagonal lattice is definedby two
equaland
coplanar vectors aiand
a2, at 120 toone
another,and
a third axis c at right angles [Fig. 2-11(a)].The complete
lattice is built up, as usual,by
HfeocH
(110)
(110) (111)
FIG. 2-10. Millerindices of latticeplanes.
(102)
In document
WITHIN THE
(pagina 54-57)