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

• Solid-state reactionRelated: Reactant and product structures determine which atomic rearrangements are possible.

• Ball-and-stick modelRelated: Ball-and-stick diagrams show how bonded units form repeating crystal networks.

• CarnalliteRelated: Carnallite’s structure accommodates six water molecules per formula unit.

• Chrome yellowRelated: Lead chromate’s structure determines how it interacts with visible light.

• DiopsideRelated: Its repeating arrangement controls diopside’s physical properties and mineral identification.

• HornblendeRelated: Hornblende’s double-chain arrangement determines its characteristic cleavage directions.

• Lester GermerRelated: The regular atomic planes in the nickel target shaped the measured scattering pattern.

• Magnesium carbonateRelated: The arrangement of ions helps distinguish magnesium carbonate minerals and their properties.

• Max von LaueRelated: Diffraction patterns made crystal structure experimentally accessible.

• Oxide mineralRelated: Atomic arrangements control the physical properties of individual oxide minerals.

• Phosphate mineralRelated: How phosphate groups and other ions repeat determines each mineral's structure.

• Potassium perchlorateRelated: The ordered lattice helps explain potassium perchlorate’s solid-state properties.

• BiotiteRelated: Biotite’s crystal structure organizes its tetrahedral and octahedral sheets into layers.

• Iron(III) sulfateRelated: Different hydration states can have distinct solid structures and properties.

• John B. GoodenoughRelated: Layered oxide structures let lithium ions move while retaining a stable host lattice.

• Mineral physicsRelated: Mineral behavior depends on how atoms are arranged and bonded in crystals.

• Native element mineralRelated: Different atomic arrangements help distinguish native minerals with similar compositions.

• PetaliteRelated: Petalite's atomic arrangement distinguishes it from other minerals with similar chemistry.

• PhaseRelated: Different crystal structures can define distinct solid phases of one substance.

• SillimaniteRelated: Sillimanite’s atomic arrangement distinguishes it from other Al₂SiO₅ polymorphs.

• Sodium azideRelated: The solid-state arrangement helps determine sodium azide’s physical and chemical behavior.

• Sodium iodideRelated: Solid NaI adopts an extended lattice rather than existing as separate molecules.

• Zinc chlorideRelated: Anhydrous zinc chloride forms extended structures rather than isolated ZnCl₂ molecules.

• Barium chlorideRelated: The solid arranges its ions in a repeating lattice.

• Copper(II) hydroxideRelated: The arrangement of copper and hydroxide units determines solid-state properties.

• HedenbergiteRelated: Hedenbergite’s monoclinic structure determines its cleavage, symmetry, and mineral-group classification.

• KyaniteRelated: Kyanite’s arrangement of aluminum, silicon, and oxygen helps produce its directional properties.

• Potassium superoxideRelated: KO₂’s solid-state properties depend on how potassium and superoxide ions pack and orient.

• SodaliteRelated: Sodalite’s framework structure creates cages that host chloride and other ions.

• Sodium bromideRelated: The ions in solid NaBr occupy an ordered repeating lattice.

• Allotropes of phosphorusRelated: The crystalline allotropes differ in how phosphorus atoms repeat through space.

• AluniteRelated: Alunite’s structure accommodates sulfate groups, aluminum octahedra, and potassium.

• Arsenide mineralRelated: Different atomic arrangements distinguish arsenide species with similar chemical compositions.

• Barium nitrateRelated: Its ordered ionic lattice determines solid-state properties such as density and melting behavior.

• Barium peroxideRelated: The arrangement of barium and peroxide ions determines the solid's structural properties.

• Cobalt(II) hydroxideRelated: The arrangement of cobalt and hydroxide units helps distinguish solid forms and properties.

• Halide mineralRelated: Ion arrangement governs the shapes and properties of halide crystals.

• Inorganic compoundRelated: Many inorganic compounds form extended lattices rather than discrete molecular units.

• JarositeRelated: Jarosite’s structure determines which elements can substitute into its lattice.

• Mercury(II) oxideRelated: HgO’s crystal arrangement varies between its red and yellow forms.

• Potassium bisulfateRelated: Its solid-state properties depend on how potassium and hydrogen sulfate ions pack together.

• Potassium bitartrateRelated: Its crystal structure determines the form of the tartrate deposits.

• Sodium permanganateRelated: Its solid-state structure describes how sodium and permanganate ions pack together.

• AllotropeRelated: Many solid allotropes differ in the repeating arrangement of their atoms.

• ElectrideRelated: Its cavities and channels determine where an electride can host anionic electrons.

• Lithium iodideRelated: The solid's ions occupy repeating positions rather than forming isolated pairs.

• Manganese(II) chlorideRelated: Anhydrous MnCl₂ and its hydrates have distinct solid-state arrangements.

• PentlanditeRelated: Pentlandite's cubic arrangement helps distinguish it from related nickel sulfides.

• PolluciteRelated: Pollucite’s framework structure governs its composition, ion sites, and relation to other zeolites.

• Potassium hydrideRelated: KH forms an extended ionic lattice rather than discrete KH molecules in the solid.