Crystal Lattices
Describes unit cell, crystal planes and diffraction in periodic solids.
Conceptual context
A crystal lattice is not a picture of one atom; it is a rule of repetition. A unit cell is copied through space, so a microscopic arrangement becomes a set of distances, directions and diffraction signatures. The central question is how and the Miller indices , and determine , and how that spacing allows radiation with to produce peaks at specific values. The lattice is not directly seen in an ordinary image. It is inferred because a periodic solid leaves a geometric fingerprint in scattered waves.
🟢 Essential level
Think of a lattice as an invisible three-dimensional scaffold. sets the basic scale: if the cubic cell is larger, many plane families are farther apart.
The Miller indices, summarized here by , do not count individual planes; they choose the orientation of a parallel family inside the crystal. When those indices become larger, the selected family cuts the cell more densely, so becomes smaller. Diffraction occurs because radiation with is scattered by many equivalent planes. Only certain values make the outgoing waves reinforce one another. A diffraction peak is therefore not just a bright spot. It is a coded message about the periodic geometry, scale and repeating plane families of the solid at atomic scale in real solids. It is similar to bouncing light off a stack of parallel, evenly spaced blinds: only at certain precise angles do the reflections from every slat arrive in phase and reinforce each other, while at other angles they cancel out.
🔵 Formal level
Basic formulas
For an ideal cubic lattice, a plane family is labeled by , and . The core relation between crystal orientation and lattice scale, which belongs to real-space cell geometry, is:
Interplanar spacing in a cubic lattice
It shows that increases with and decreases when the quadratic Miller-index combination grows. To connect that real-space spacing with a diffraction experiment, through a relation that belongs to wave reading, use:
Bragg's law
Here selects the constructive-interference order, fixes the probe scale and is the observed angle.
Real student questions
Are Miller indices distances? No. , and encode plane orientation; the distance is obtained only after combining those indices with .
Why may a crystal miss some expected peaks? Plane geometry is not enough: the atomic basis, symmetries and structure factors can cancel certain reflections.
Is the angle of the plane? No. It is the incidence angle relative to the planes that makes interference constructive.
Does determine diffraction? Not directly. It helps interpret compactness, while peaks depend on periodicity, spacings and scattering distribution.
Final synthesis
A crystal lattice turns microscopic order into measurable signals. sets the scale, , and select planes, links geometry with reciprocal space, and reveals when the wave reads the structure.
Formal development
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🔴 Structural level
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Deep physical interpretation
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Order of magnitude
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Personalized resolution method
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Special cases and extended example
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Cross-cutting connections and study paths
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