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Interplanar Spacing (Cubic)

Relates the unit cell dimension and Miller indices to the distance between lattice planes.

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Core idea

Overview

This formula defines the perpendicular distance between adjacent parallel planes in a cubic crystal lattice, designated by their Miller indices. It serves as a fundamental geometric relationship in crystallography, linking the unit cell dimension to the observable diffraction patterns of minerals.

When to use: Apply this equation exclusively to minerals in the isometric (cubic) system where all crystal axes are equal in length and perpendicular to one another. It is typically used during X-ray diffraction analysis to calculate d-spacing from known lattice parameters or vice versa.

Why it matters: Understanding interplanar spacing is vital for mineral identification and interpreting atomic arrangements within a crystal. It allows geoscientists to relate the macroscopic physical properties of a mineral, such as cleavage and hardness, to its internal microscopic structure.

Symbols

Variables

= Interplanar Spacing, a = Lattice Parameter, h = Miller Index h, k = Miller Index k, l = Miller Index l

Interplanar Spacing
The perpendicular distance between parallel planes of atoms
Lattice Parameter
The edge length of the cubic unit cell
Miller Index h
Reciprocal intercept on the crystallographic x-axis
Miller Index k
Reciprocal intercept on the crystallographic y-axis
Miller Index l
Reciprocal intercept on the crystallographic z-axis

Walkthrough

Derivation

Derivation: Interplanar Spacing in Cubic Crystals

Relates the spacing between lattice planes to the unit cell parameter and Miller indices.

  • The crystal system is cubic (a = b = c, α = β = γ = 90°).
1

Use the geometry of a cubic lattice:

From the definition of Miller indices and the perpendicular distance between parallel lattice planes in a cubic system.

2

Solve for d:

Take the reciprocal square root to get the interplanar spacing.

Note: Combined with Bragg's law (nλ = 2d sin θ), this allows determination of the lattice parameter from X-ray diffraction data.

Result

Source: University Mineralogy — Crystallography

Free formulas

Rearrangements

Solve for

Interplanar Spacing (Cubic) for

The equation for Interplanar Spacing (Cubic) is already solved for . This sequence identifies the expression for .

Difficulty: 2/5

The static page shows the finished rearrangements. The app keeps the full worked algebra walkthrough.

Visual intuition

Graph

Graph unavailable for this formula.

The graph of interplanar spacing (d_hkl) against the square root of the sum of squared Miller indices follows an inverse relationship. As the independent variable increases, the interplanar spacing decreases along a hyperbolic curve that approaches zero as an asymptote.

Graph type: inverse

Why it behaves this way

Intuition

Imagine a 3D grid of atoms (the crystal lattice). The equation helps visualize how different sets of parallel planes, defined by their Miller indices, slice through this grid, and how the size of the repeating unit cell

The perpendicular distance between adjacent parallel planes in a crystal lattice.
This distance dictates the angles at which X-rays will diffract from the crystal, crucial for identifying minerals and understanding their internal structure.
The length of the edge of the cubic unit cell, representing the fundamental repeat unit of the crystal structure.
A larger unit cell (larger 'a') means the crystal's repeating pattern is physically larger, leading to proportionally larger interplanar spacings for any given set of planes.
h, k, l
Miller indices, a set of integers defining the orientation and relative spacing of a family of parallel crystal planes.
These indices describe the 'steepness' or 'density' of the planes. Higher absolute values of h, k, or l (e.g., (200) vs (100)) indicate planes that are more closely spaced or cut the axes more frequently, resulting in a

Signs and relationships

  • √(h^2 + k^2 + l^2): This term appears in the denominator because it represents the inverse relationship between the magnitude of the Miller indices and the interplanar spacing.

Free study cues

Insight

Canonical usage

The interplanar spacing () and the unit cell dimension (a) must be expressed in the same unit of length, while Miller indices (h, k, l) are dimensionless integers.

Common confusion

Students often forget to ensure consistent length units for 'a' and '' (e.g., mixing Ångströms and nanometers without conversion), or they misinterpret Miller indices as having units.

Dimension note

The Miller indices (h, k, l) are dimensionless integers, and the denominator is therefore also dimensionless. This ensures that the unit of is solely determined by the unit of 'a'.

Unit systems

Length · Represents the perpendicular distance between adjacent parallel planes. Commonly reported in Ångströms (Å), nanometers (nm), or picometers (pm).
Length · The length of the side of the cubic unit cell (lattice parameter). Must be in the same unit as d_{hkl}.
h, k, lDimensionless · Miller indices are integers that define the orientation of a crystal plane relative to the unit cell axes.

Ballpark figures

  • Quantity:

One free problem

Practice Problem

A sample of Halite (NaCl) has a cubic lattice constant of 5.64 Å. Calculate the interplanar spacing for the (200) plane.

Lattice Parameter5.64 The edge length of the cubic unit cell
Miller Index h2 Reciprocal intercept on the crystallographic x-axis
Miller Index k0 Reciprocal intercept on the crystallographic y-axis
Miller Index l0 Reciprocal intercept on the crystallographic z-axis

Solve for:

Hint: Plug the indices into the denominator: √(2² + 0² + 0²) simplifies to 2.

The full worked solution stays in the interactive walkthrough.

Where it shows up

Real-World Context

In the spacing of the (111) planes in a diamond crystal to determine the expected angle of X-ray reflection, Interplanar Spacing (Cubic) is used to calculate Interplanar Spacing from Lattice Parameter, Miller Index h, and Miller Index k. The result matters because it helps connect measured amounts to reaction yield, concentration, energy change, rate, or equilibrium.

Study smarter

Tips

  • Ensure the unit of the lattice constant 'a' (often in Angstroms or nanometers) matches your desired unit for spacing.
  • Miller indices (h, k, l) must be integers; squaring them ensures the denominator is always a positive square root.
  • For non-cubic systems (like tetragonal or orthorhombic), this simplified version of the formula does not apply.

Avoid these traps

Common Mistakes

  • Applying this cubic-specific formula to minerals in non-cubic crystal systems.
  • Neglecting to square the h, k, and l values before summing them.

Common questions

Frequently Asked Questions

Relates the spacing between lattice planes to the unit cell parameter and Miller indices.

Apply this equation exclusively to minerals in the isometric (cubic) system where all crystal axes are equal in length and perpendicular to one another. It is typically used during X-ray diffraction analysis to calculate d-spacing from known lattice parameters or vice versa.

Understanding interplanar spacing is vital for mineral identification and interpreting atomic arrangements within a crystal. It allows geoscientists to relate the macroscopic physical properties of a mineral, such as cleavage and hardness, to its internal microscopic structure.

Applying this cubic-specific formula to minerals in non-cubic crystal systems. Neglecting to square the h, k, and l values before summing them.

In the spacing of the (111) planes in a diamond crystal to determine the expected angle of X-ray reflection, Interplanar Spacing (Cubic) is used to calculate Interplanar Spacing from Lattice Parameter, Miller Index h, and Miller Index k. The result matters because it helps connect measured amounts to reaction yield, concentration, energy change, rate, or equilibrium.

Ensure the unit of the lattice constant 'a' (often in Angstroms or nanometers) matches your desired unit for spacing. Miller indices (h, k, l) must be integers; squaring them ensures the denominator is always a positive square root. For non-cubic systems (like tetragonal or orthorhombic), this simplified version of the formula does not apply.

References

Sources

  1. Charles Kittel, Introduction to Solid State Physics
  2. William D. Callister Jr., David G. Rethwisch, Materials Science and Engineering: An Introduction
  3. Wikipedia: Miller index
  4. Elements of X-ray Diffraction (3rd ed.) by B.D. Cullity and S.R. Stock
  5. Introduction to Mineralogy by William D. Nesse (4th ed., Oxford University Press)
  6. Introduction to Solid State Physics by Charles Kittel (8th ed., Wiley)
  7. Wikipedia article "Diamond
  8. Wikipedia article "Halite