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The 193 pages that link to Crystal structure, each with the reason it gives.

• SemiconductorNarrower topic: Atomic order shapes the electronic bands that govern semiconductor behavior.

• Silicate mineralNarrower topic: The arrangement of tetrahedra and other ions determines each silicate mineral's structure.

• Sodium chlorideNarrower topic: NaCl's repeating arrangement gives it its characteristic cubic crystals and cleavage.

• CrystallizationNarrower topic: Crystallization produces this repeating arrangement from a disordered starting phase.

• MineralNarrower topic: Minerals are distinguished from noncrystalline solids by their ordered atomic arrangements.

• Solid solutionNarrower topic: A solid solution preserves one underlying crystalline arrangement while its site occupants vary.

• Grain boundaryNarrower topic: A grain boundary separates regions that each possess an ordered crystal structure.

• HydrateNarrower topic: A hydrate’s defining water molecules occupy positions within an ordered crystal.

• Bravais latticeNarrower topic: Unlike a Bravais lattice alone, it specifies the objects repeated at each point.

• Unit cellNarrower topic: A unit cell plus its lattice translations specifies this full arrangement.

• CrystallographyNarrower topic: It is the structural object crystallographic methods describe and determine.

• Neutron diffractionNarrower topic: Neutron diffraction determines atomic positions and occupancies in crystals.

• Iron oxideNarrower topic: Different atomic arrangements produce distinct iron oxide minerals and material properties.

• Silicon carbideNarrower topic: Different atomic arrangements give SiC its many polytypes and influence their properties.

• ZeoliteNarrower topic: Distinct crystal structures create the different channels and cavities found among zeolites.

• Coordination numberNarrower topic: Coordination numbers summarize local arrangements within a crystal structure.

• AllotropyNarrower topic: Different atomic arrangements give solid allotropes distinct structures.

• Magnesium oxideNarrower topic: MgO’s properties depend on its repeating arrangement of ions.

• QuasicrystalNarrower topic: Quasicrystals are crystal structures without translational periodicity.

• MetalNarrower topic: Atomic packing shapes how a metal deforms and how defects move through it.

• CrystallinityNarrower topic: Crystallinity describes how much of a solid possesses this repeating arrangement.

• Work hardeningNarrower topic: Lattice geometry governs slip and dislocation motion during the deformation that hardens metals.

• Carbonate mineralNarrower topic: Carbonate minerals differ in how carbonate groups and metal cations pack into repeating structures.

• Manganese dioxideNarrower topic: MnO₂ occurs in several structures whose tunnels and layers affect ion movement and reactivity.

• Calcium oxalateNarrower topic: Different arrangements and water content distinguish calcium oxalate crystal forms.

• CorundumNarrower topic: Corundum’s atomic arrangement determines its characteristic shape and physical properties.

• Isomorphous substitutionNarrower topic: Substitution changes occupants while the host arrangement remains substantially intact.

• Calcium sulfateNarrower topic: Different arrangements and water content account for gypsum and anhydrite’s distinct properties.

• Lead(II) oxideNarrower topic: Litharge and massicot differ in their crystal structures despite sharing the formula PbO.

• Coordination geometryNarrower topic: In crystals, coordination geometry describes a local part of this larger arrangement.

• Zinc sulfideNarrower topic: ZnS occurs in distinct structures whose geometry changes its properties.

• Allotropes of carbonNarrower topic: Atomic ordering separates crystalline carbon forms such as diamond and graphite.

• BastnäsiteNarrower topic: Bastnäsite’s structure determines how its carbonate, fluoride, and rare-earth ions are arranged.

• Sodium hydrideNarrower topic: The arrangement of ions explains sodium hydride’s solid-state properties.

• Sodium sulfateNarrower topic: Different hydration states give sodium sulfate distinct crystal structures and physical properties.

• Sulfate mineralNarrower topic: The sulfate group’s arrangement with other constituents distinguishes one mineral structure from another.

• Vacancy defectNarrower topic: A vacancy is defined by the site missing from this periodic arrangement.

• Borate mineralNarrower topic: Crystal structure determines how borate groups and cations combine.

• Lead(II) sulfateNarrower topic: The solid’s arrangement determines how its ions pack and interact.

• Solid-state chemistryNarrower topic: Its repeating arrangements provide the structural language used to describe solid compounds.

• Ammonium perchlorateNarrower topic: The salt's solid-state arrangement influences its density and thermal behavior.

• ArsenopyriteNarrower topic: Arsenopyrite's atomic arrangement gives it distinctive symmetry and cleavage.

• Copper(I) oxideNarrower topic: The arrangement of ions in solid Cu₂O shapes its physical and electronic properties.

• Copper(II) sulfateNarrower topic: Different water contents produce distinct copper(II) sulfate crystal arrangements.

• CrystalliteNarrower topic: A crystallite is a region in which this arrangement remains ordered.

• LazuriteNarrower topic: Lazurite’s framework and internal cavities host the components that generate its color.

• Lithium oxideNarrower topic: Li₂O forms an ordered lattice rather than discrete molecules.

• BrookiteNarrower topic: Brookite’s orthorhombic symmetry comes from its atomic arrangement.

• FeldspathoidNarrower topic: Framework topology distinguishes feldspathoids from minerals with different silicate structures.

• ForsteriteNarrower topic: The arrangement of magnesium, silicon, and oxygen determines forsterite’s physical properties.