Lattice Planes and Miller IndicesNote: DoITPoMS Teaching and Learning Packages are intended to be used interactively at a computer! This print-friendly version of the TLP is provided for convenience, but does not display all the content of the TLP. For example, any video clips and answers to questions are missing. The formatting (page breaks, etc) of the printed version is unpredictable and highly dependent on your browser. ContentsAimsOn completion of this tutorial you should:
Before you startYou should understand the concepts of a Lattice , Unit cell , Crystal axes , Crystal system and the variations, Primitive , FCC , BCC which make up the Bravais lattice . You might also like to look at the TLP on Atomic Scale Structure of Materials. You should understand the concepts of vectors and planes in mathematics. IntroductionMiller Indices are a method of describing the orientation of a plane or set of planes within a lattice in relation to the unit cell. They were developed by William Hallowes Miller. These indices are useful in understanding many phenomena in materials science, such as explaining the shapes of single crystals, the form of some materials' microstructure, the interpretation of X-ray diffraction patterns, and the movement of a dislocation , which may determine the mechanical properties of the material.
How to index a lattice planeThe next three animations take you through the basics of how to index a plane. Click “Start” to begin each animation, and then navigate through the pages using the buttons at the bottom right.
Note: This animation requires Adobe Flash Player 8 and later, which can be downloaded here.
Note: This animation requires Adobe Flash Player 8 and later, which can be downloaded here.
Note: This animation requires Adobe Flash Player 8 and later, which can be downloaded here. Parallel lattice planesThis animation explains the relationships between parallel planes and their indices. Click “Start” to begin and use the buttons at the bottom right to navigate through the pages.
Note: This animation requires Adobe Flash Player 8 and later, which can be downloaded here. Lattice planes can be represented by showing the trace of the planes on the
faces of one or more unit cells. The diagram shows the trace of the (
How to draw a lattice plane
Note: This animation requires Adobe Flash Player 8 and later, which can be downloaded here. Bracket ConventionsIn crystallography there are conventions as to how the indices of planes and directions are written. When referring to a specific plane, “round” brackets are used: (hkl) When referring to a set of planes related by symmetry, then “curly” brackets are used: {hkl} These might be the (100) type planes in a cubic system, which are (100), (010), (001), (
Note: This animation requires Adobe Flash Player 8 and later, which can be downloaded here. Directions in the crystal can be labelled in a similar way. These are effectively vectors written in terms of multiples of the lattice vectors a, b, and c. They are written with “square” brackets: [UVW] A number of crystallographic directions can also be symmetrically equivalent, in which case a set of directions are written with “triangular” brackets: <UVW> Vectors and PlanesIt may seem, after considering cubic systems, that any lattice plane (hkl) has a normal direction [hkl]. This is not always the case, as directions in a crystal are written in terms of the lattice vectors, which are not necessarily orthogonal, or of the same magnitude. A simple example is the case of in the (100) plane of a hexagonal system, where the direction [100] is actually at 120° (or 60° ) to the plane. The normal to the (100) plane in this case is [210] Click to open video (13.27 MB) ... in separate window ... video aloneWeiss Zone LawThe Weiss zone law states that: If the direction [UVW] lies in the plane (hkl), then: hU + kV + lW = 0 In a cubic system this is exactly analogous to taking the scalar product of the direction and the plane normal, so that if they are perpendicular, the angle between them, θ, is 90° , then cosθ = 0, and the direction lies in the plane. Indeed, in a cubic system, the scalar product can be used to determine the angle between a direction and a plane. However, the Weiss zone law is more general, and can be shown to work for all crystal systems, to determine if a direction lies in a plane. From the Weiss zone law the following rule can be derived: The direction, [UVW], of the intersection of (h1k1l1) and (h2k2l2) is given by: U = k1l2 − k2l1 V = l1h2 − l2h1 W = h1k2 − h2k1 As it is derived from the Weiss zone law, this relation applies to all crystal systems, including those that are not orthogonal. Examples of lattice planesThe (100), (010), (001), (
The (101), (110), (011), (10
The (111) type planes in a face centred cubic lattice are the close packed planes. Click and drag on the image below to see how a close packed (111) plane intersects the fcc unit cell. Click to open video (8.0 MB) ... in separate window ... video alone Draw your own lattice planesThis simulation generates images of lattice planes. To see a plane, enter a set of Miller indices (each index between 6 and −6), the numbers separated by a semi-colon, then click “view” or press enter.
Note: This animation requires Adobe Flash Player 8 and later, which can be downloaded here. Practical UsesAn understanding of lattice planes is required to explain the form of many microstructural features of many materials. The faces of single crystals form on certain lattice planes, typically those with low indices. In a similar way, the form of the microstructure in a polycrystalline material is strongly dependent on lattice planes. When a new Phase of material forms, the surfaces tend to be aligned on low index planes, as with single crystals. When a new solid phase is formed in another solid, the interfaces occur on along the most energetically favourable planes, where the two lattices are most coherent. This leads to plate-like precipitates forming, at specific angles to each other.
Section through an Fe-Ni meteorite showing plates at 60° to each other One method of plastic deformation is by dislocation slip. Understanding lattice planes, and directions is essential to explain why dislocations move, combine and tangle in the observed way. More information can be obtained in the TLP - 'Slip in Single Crystals'
A scanning electron micrograph of a single crystal of cadmium Twinning is where a part of the crystal is “flipped” to form a mirror image of the rest of the crystal, reflected in a particular lattice plane. This can either occur in annealing , or as a mechanism of plastic deformation.
Annealing twins in brass X–ray diffraction is a method of determining the crystal structure of a material. By interpreting the diffraction patterns as reflections from lattice planes in the material, the structure can be determined. More information can be obtained in the TLP - 'X-ray diffraction '
Apparatus for carrying out single crystal X-ray diffraction.
Worked examplesExample AThe figure below is a scanning electron micrograph of a niobium carbide dendrite in a Fe-34wt%Cr-5wt%Nb-4.5wt%C alloy. Niobium carbide has a face centred cubic lattice. The specimen has been deep-etched to remove the surrounding matrix chemically and reveal the dendrite. The dendrite has 3 sets of “arms” which are orthogonal to one another (one set pointing out of the plane of the image, the other two sets, to a good approximation, lying in the plane of the image), and each arm has a pyramidal shape at its end. It is known that the crystallographic directions along the dendrite arms correspond to the < 100 > lattice directions, and that the direction ab labelled on the micrograph is [10
1) If point c (not shown) lies on the axis of this dendrite arm, what is the direction cb ? Index face C , marked on the micrograph.
The diagram shows the [10 Using a right handed set of axes, we then have z-axis pointing out of the plane of the image, the x-axis pointing along the direction cb, and the y-axis pointing towards the top left of the image.
Face C must contain the direction cb, and its normal must point out of the plane of the image. Therefore face C is a (001) plane. 2) The four faces which lie at the end of each dendrite arm have normals which all make the same angle with the direction of the arm. Observing that faces A and B marked on the micrograph both contain the direction ab , and noting the general directions along which the normals to these faces point, index faces A and B . Both faces A and B have normals pointing in the positive x and z directions, i.e. positive h and l indices. Face A has a positive k index, and face B has a negative k index. The morphology of the ends of the arms is that of half an octahedron, suggesting that the faces are (111) type planes. This would make face A, in green, a (111) plane, and face B, in blue, a (1
Example B1) Work out the common direction between the (111) and (001) in a triclinic unit cell. The relation derived from the Weiss zone law in the section Vectors and planes states that: The direction, [UVW], of the intersection of (h1k1l1) and (h2k2l2) is given by: U = k1l2 − k2l1 V = l1h2 − l2h1 W = h1k2 − h2k1 We can use this relation as it applies to all crystal systems, including the triclinic system that we are considering. We have h1 = 1, k1 = 1, l1 = 1 and h2 = 0, k2 = 0, l2 = 1 Therefore U = (1 × 1) - (0 × 1) = 1 V = (1 × 0) - (1 × 1) = −1 W = (1 × 0) - (0 × 1) = 0. So the common direction is: [1 This is shown in the image below:
If we had defined the (001) plane as (h1k1l1) and the (110) plane as (h2k2l2) then the resulting direction would have been, [ 2) Use the Weiss zone law to show that the direction [1 We have U = 1, V = −1, W = 0, and h = 1, k = 1, l = 1. hU + kV + lW = (1 × 1) + (1 × −1) + (1 × 0) = 0 Therefore the direction [1 SummaryMiller Indices are the convention used to label lattice planes. This mathematical description allows us to define accurately, planes within a crystal, and quantitatively analyse many problems in materials science.
QuestionsGame: Identify the planes
Quick questionsYou should be able to answer these questions without too much difficulty after studying this TLP. If not, then you should go through it again!
Open-ended questionsThe following questions are not provided with answers, but intended to provide food for thought and points for further discussion with other students and teachers.
Going furtherBooks[1] D. McKie and C. McKie, Crystalline Solids , Thomas Nelson and Sons, 1974. A very comprehensive crystallography text. [2] C. Hammond, The Basics of Crystallography and Diffraction , Oxford, 2001. Chapter 5 covers lattice planes and directions. The rest of the book gives an introduction to crystallography and diffraction in general. [3] B.D. Cullity, Elements of X-Ray Diffraction , Prentice Hall, 2003. Covers X-Ray diffraction in detail. Chapter 2 covers the crystallography required for this. [4] C. Kittel, Introduction to Solid State Physics, John Wiley and Sons, 2004. Chapter 1 covers crystallography. The book then goes on to cover a wide range of more advanced solid state science.
Academic consultant: Noel Rutter (University of Cambridge) DoITPoMS is funded by the UK Centre for Materials Education and the Department of Materials Science and Metallurgy, University of Cambridge Additional support for the development of this TLP came from the Worshipful Company of Armourers and Brasiers' |
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