Interplanar Spacing (Cubic)
Relates the unit cell dimension and Miller indices to the distance between lattice planes.
This public page keeps the free explanation visible and leaves premium worked solving, advanced walkthroughs, and saved study tools inside the app.
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
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°).
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.
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
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
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.
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
- Charles Kittel, Introduction to Solid State Physics
- William D. Callister Jr., David G. Rethwisch, Materials Science and Engineering: An Introduction
- Wikipedia: Miller index
- Elements of X-ray Diffraction (3rd ed.) by B.D. Cullity and S.R. Stock
- Introduction to Mineralogy by William D. Nesse (4th ed., Oxford University Press)
- Introduction to Solid State Physics by Charles Kittel (8th ed., Wiley)
- Wikipedia article "Diamond
- Wikipedia article "Halite