Volume 36 Received 3 June 2002 | New method for determining hexagonal direction indices and their relationship to crystallographic directionsaDepartment of Mechanical and Aerospace Engineering, University of California, San Diego, La Jolla, CA 92093-0411,USA A new method for determining the hexagonal direction indices is introduced, which is more practical than other commonly used methods. The relationship between the crystallographic directions and hexagonal direction indices for face-centered cubic crystals is derived. Different sets of hexagonal indices for equivalent crystallographic directions are discussed. |
The hexagonal direction indices are well known and routinely applied to designate the crystallographic directions in hexagonal close packed (h.c.p.) crystals. They can also be used to designate the crystallographic directions in face-centered cubic (f.c.c.) crystals, although these are commonly, and more conveniently, labeled by using the standard crystallographic direction indices (e.g. Askeland, 1994
; Smith, 1999
). In this paper, we describe a new method to determine the hexagonal indices in f.c.c. and h.c.p. crystals, which is more practical and easier to apply than other commonly used methods. We then elaborate on the relationship between the hexagonal direction indices and the crystallographic directions for f.c.c. crystals, and derive two different but related four-index notations for equivalent crystallographic directions. The results may be of interest in the geometric analysis of the faults in stacking sequences, diffraction patterns, and related problems in the theory of crystalline lattices and their defects (Barrett & Massalski, 1980
; McKie & McKie, 1986
; Kelly et al., 2000
).
Consider a unit cell of an f.c.c. crystal with the lattice parameter a. The stacking sequence ABC... of the close-packed (111) planes of interplanar spacing a/(31/2) is shown in Fig. 1
. The unit vectors along the edges of the cubic cell are i1, i2 and i3. The crystallographic direction indices for a lattice direction parallel to the vector x = x1i1 + x2i2 + x3i3 are the set of integers [m1 m2 m3], where
The hexagonal atomic packing within the (111) plane through the origin at one of the atoms, A, is shown in Fig. 2
. The directions along the cell edges project in the (111) plane along the unit directions e1, e2 and e3. These vectors are at the angle 2
/3, so that
The projected axes
1,
2 and
3 do not pass through the first-nearest neighbors to A, but through the second-nearest neighbors. Denoting the unit vector normal to the octahedral (111) plane by n = (i1 + i2 + i3)/(31/2), the direction vector x can be decomposed into the component
within the (111) plane, and the orthogonal component
, such that
If a1, a2 and a3 are the components of
along the edges of the cubic cell,
it readily follows that
and
The constraint conditions are
Note that the coefficient 1/(61/2) in equation (6)
appears in crystalline plasticity as the Schmid factor in f.c.c. crystals for uniaxial loading along the [001] direction. Indeed, the product
, where m is the vector in the close-packed direction
, is equal to this value.
| Figure 1 A unit cell of an f.c.c. crystal with the lattice parameter a. The ABC... stacking sequence of close-packed (111) planes is indicated. |
| Figure 2 The hexagonal atomic arrangement within a (111) plane. The directions along the cubic cell edges project in this plane along the directions e1, e2, e3. The interatomic spacing is a0 = a/(21/2). |
The in-plane hexagonal decomposition of the vector
along the three axes e1, e2 and e3,
is defined such that
1 is the projection of the vector component a1i1 onto e1, and similarly for
2 and
3, i.e.
Since
=
=
= (2/3)1/2, it follows that
with the redundancy condition
The following equalities are observed
To prove the first, for example, it is enough to observe that
because
1 +
2 +
3 = 0, and similarly for
and
. The formulae (12)
have simple but convenient geometric interpretations, shown in Fig. 3
. The orthogonal projections of the vector
onto the axes e1, e2 and e3, scaled by the factor of 2/3, define the hexagonal components
1,
2 and
3. The simple recipe (12)
is probably the most convenient method to determine the hexagonal in-plane indices, although it is surprisingly not mentioned in any of the standard texts on the subject (e.g. Askeland, 1994
; Smith, 1999
). There, instead, the vector
is first decomposed into the directions e1 and e2 as
so that comparison with equation (8)
establishes the connections
with the inverse relationships
These formulae are clearly not needed if the simple recipe (12)
is used.
| Figure 3 Geometric interpretation of the vector decomposition = 1e1 + 2e2 + 3e3, subject to the constraint 1 + 2 + 3 = 0. The components 1, 2, 3 are defined by the orthogonal projections on the axes e1, e2, e3, with the appropriate sign and the scaling factor of 2/3. |
As an illustration, consider a unit direction (
= 1) at an angle of 30° to the
1 axis. From Fig. 4
it immediately follows that (3/2)
1 = cos30° = 31/2/2 and
2 = 0 (because
is orthogonal to
2). Thus, the hexagonal indices are [
. On the other hand, if the classical method is used, we first need to calculate the components
= 2/(31/2) and
= 1/(31/2), then apply equations (16)
to obtain
1 = 1/(31/2) and
2 = 0, which finally yields
. The advantage of the former method is clear.
| Figure 4 The unit direction at an angle of 30° relative to the 1 axis. Two types of projections on the coordinate directions are shown, both of which can be used to determine the corresponding hexagonal indices. |
Several useful trigonometric expressions are derived as follows. From Fig. 3
it is recognized that
where
=
is the length of the vector
. Consequently, the following relationships hold:
Similarly,
and
Since
=
-
, and
=
-
, we also have
The length of the vector
can be calculated from
The identity
with similar identities for
2 -
3 and
3 -
1 are noted, in addition to
Analogous expressions in terms of the principal deviatoric stress components are well known from the theory of plasticity and geometric representation of the yield locus in the deviatoric
plane (e.g. Kachanov, 1971
; Lubarda, 2002
).
For the derivation of the relationship between the crystallographic directions and hexagonal direction indices for an f.c.c. crystal, it is useful first to derive the general formulae for the transformation of coordinates (
) under the rotation of the coordinate system within the (111) plane. If
is the angle of counterclockwise rotation (Fig. 5
), it can be readily verified that
and
where
=
+
. By expanding the right-hand sides of equation (26)
and by using equations (18)
, (19)
and (20)
, it follows that
The same transformation relates the unit direction vectors
,
,
and
,
,
. A text by Sands (1982
) can be consulted for further analysis of the transformation rules for vectors and tensors in crystallography.
| Figure 5 The coordinate system ( . The vector makes an angle with the negative 3 axis. |
If the angle of rotation discussed in the previous section is
=
/6, we obtain the hexagonal coordinates
,
,
within the (111) plane, which are shown in Fig. 6
. The transformation rules for the unit vectors in this case reduce to
and similarly for the two sets of coordinates
,
,
and
,
,
. By using the expressions (10)
for the components
1,
2,
3 in terms of the rectangular components x1 = m1a, x2 = m2a, x3 = m3a, it follows that
where a0 = a/(21/2) is the atomic distance between the first neighbors in the close-packed (111) plane. Thus, the projected vector
can be written as
On the other hand, the component of the vector x orthogonal to
is
where c0 = 31/2a = 61/2a0 represents the interplanar spacing between the A-type planes. This scale in the n direction is chosen so that the spacing between the A, B and C planes is equal to c0/3. Therefore, the direction vector x can be decomposed as
This representation defines the hexagonal indices [ho ko io lo] for the considered direction, which are
then
The reduction to lowest integers usually needs to be made in equation (33)
. In the matrix notation, the transformation between the two sets of indices is
The inverse relations are
with the matrix counterpart
The clearing of fractions was used in the above derivation, so that in this case m1 + m2 + m3 = 6lo. In general, an additional reduction to lowest integers is needed.
| Figure 6 The coordinate system ( /6. The new axes |
As an example which illustrates the use of the transformation formulae (35
) and (37
), consider the direction
in the crystallographic direction notation. From equation (35)
it follows that ho = 4, ko = 2, io = -6 and lo = 2, so that upon the reduction to lowest integers the hexagonal indices become
. On the other hand, for the direction with the hexagonal indices
, equation (37)
gives m1 = 6, m2 = m3 = 0, which yield the crystallographic direction indices [100].
Returning to equation (32)
, the substitution of
=
+
yields
Thus, the transformation rule between the crystallographic direction indices [m1 m2 m3] and the three-axis hexagonal direction indices
is
The inverse transformation (after clearing the fractions) is
The well known connections between the two sets of indices
and [ho ko io lo] are
The hexagonal direction indices [ho ko io lo] were derived in the previous section by using the coordinate axes
,
,
that pass through the first-nearest neighbors relative to an atom A at the origin. Another set of four hexagonal indices [h k i l] for the same crystallographic direction can be obtained by using the coordinate axes
1,
2,
3 that pass through the second-nearest neighbors (Fig. 7
). The direction
2 is a reciprocal direction to
, in the sense that
= 0. The distance between the second-nearest neighbors is
= 31/2a0 = (3/2)1/2a. Thus, considering a direction x with the crystallographic direction indices [m1 m2 m3], such that x = m1ai1 + m2ai2 + m3ai3, from equation (10)
it follows that
and
This defines the four indices
i.e.
such that
On the other hand, if the direction indices [h k i l] are known, the corresponding crystallographic direction indices are determined from
with the matrix counterpart
For example, for the previously considered direction
in the crystallographic direction notation, from equation (47
) we have h = 2, k = 8, i = -10, l = 6, so that upon reducing to lowest integers the set of four indices becomes
. Similarly, for the direction with the indices
, from equation (50)
we have m1 = 8, m2 = -4, m3 = 2, which is equivalent to the
crystallographic direction. It can also be easily verified that the crystallographic direction [100] corresponds to
.
| Figure 7 The coordinate axes 1, 2, 3 are along directions of the second-nearest atoms to the origin at A. The corresponding six atoms form the hexagon (indicated by dashed lines) of interatomic spacing |
It is of interest to establish a transformation rule between the two sets of indices [h k i l] and [ho ko io lo]. This can be accomplished by equating the expressions for x from equations (34)
and (48)
, i.e.
In view of
= 31/2a0 and the relationship (28)
between the two sets of unit vectors, it follows that
The inverse relations are
For instance, the direction [ho ko io lo]
is equivalent to [h k i l]
, while [ho ko io lo]
is equivalent to [h k i l]
, in agreement with earlier calculations. The fact that the equivalent directions have different indices is a natural consequence of different hexagonal axes used for two sets of indices. It is well known that innumerable different sets of axes can be chosen for any crystal, with the corresponding direction indices related by appropriate transformation matrices [e.g. rhombohedral versus hexagonal axes for hexagonal crystals (see Barrett & Massalski, 1980
; Hahn, 1995
; Kelly et al., 2000
)].
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