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The 193 pages that link to Crystal structure, each with the reason it gives.
Melting pointRelated: Bonding and packing in a crystal help determine the energy needed to melt it.
MetallurgyRelated: Atomic packing influences deformation, diffusion, and phase stability in metals.
MineralogyRelated: Atomic arrangement distinguishes minerals that share a chemical formula.
GypsumRelated: Gypsum’s layered structure helps explain its softness and cleavage.
HardnessRelated: Crystal geometry and available slip systems shape resistance to indentation.
CalcinationRelated: Heating can alter a mineral's structure as well as its chemical composition.
SaltRelated: Solid salt forms a repeating cubic arrangement of sodium and chloride ions.
TungstenRelated: At ordinary conditions, tungsten atoms form a body-centered cubic lattice.
Potassium nitrateRelated: The ions in solid potassium nitrate occupy an ordered lattice.
Iron(III) oxideRelated: The corundum-type arrangement distinguishes hematite from other iron oxides.
EfflorescenceRelated: Water occupies specific sites in many hydrate structures before it escapes.
Molar volumeRelated: Unit-cell dimensions and particles per cell determine a solid’s molar volume.
Dihedral angleRelated: Angles between crystal planes help describe lattice geometry and interfaces.
AmphiboleRelated: Amphibole’s atomic arrangement accounts for its chain geometry and cleavage.
Sodium fluorideRelated: The repeating arrangement of sodium and fluoride ions defines solid NaF.
TalcRelated: Talc’s repeating sheets account for its softness and slippery feel.
Magnesium chlorideRelated: Its lattice organizes magnesium and chloride ions in the solid state.
Magnesium hydroxideRelated: Layered hydroxide sheets characterize brucite’s solid structure.
Mineral speciesRelated: A species is distinguished partly by its characteristic atomic arrangement.
ChromiteRelated: Chromite’s spinel structure governs its composition and physical properties.