Solid materials Physical bases of dental material science Classification of solid materials crystalline Irén Bárdos-Nagy monocrystal amorphous polycrystal porcelain veneer moldavite sapphire calcite crystal structure: Most important characteristics of crystalline materials - definite shape and volume cuprite a unique arrangement of atoms or molecules longe – range order and symmetry unit cell repeated periodically in 3D The seven lattice system: cubic - macroscopic range order (crystals) - periodic crystal structure, symmetry - relatively small number of defects in the structure - low degree of translational motion of the individual building elements simple cubic body-centered cubic face-centered cubic hexagonal - frequent anisotropy (the physical properties depend on the direction of the measurement) triclinic monoclinic orthorhombic rhombohedral tetragonal Properties of crystalline materials type of bond building units binding energy melting point rigidity conductivity (kJ/mol) sodium chloride cesium chloride covalent atoms 100 – 1000 high + - ionic ions 200 – 1500 high + - 70 – 1000 high ductile + quartz metallic diamond graphite free electrons and ions H-bond molecules 15 – 20 low + - van der Waals molecules 0.5 – 3 low soft - tungsten carbid graphite fluorapatite gold ice sulfur Polymorphism - allotropy the ability of solid material to exist in more than one form or crystal structure polymorph forms of SiO2 allotrop forms of carbon Polycrystalline materials - no macroscopic range order - large number of crystallites (grains, microscopic size crystals) - grain boundaries (interfaces where crystals of different orientations meet) - large number of crystal defects α quartz cristobalite tridymite coesite - mainly isotrope property a./ diamond b./ graphite c./ lonsdaleit d.-f./ fullerenes g. amorphous carbone h./ carbon nanotube Crystal defects b/ doping ideal crystal Point defects substitutional a/ thermal Schottky – defect (vacancy or hole) interstitium interstitial Frenkel – defect (vacancy and interstitia) Line defects Properties of amorphous solids: edge dislocation no longe-range order of the position of atoms screw dislocation Surface defects the crystalline and amorphous structure of silica in two dimension Transmission electron micrograph of dislocation large number of structure defects no definite shape (large viscosity liquid, supercooled liquid) mechanical hardness glass transition temperature Tg (the amorphous material becomes brittle The defects strongly influence the material properties! Al2O3 and Al2O3 + Cr3+ isotrope property on cooling or soft on heating) Ti Fe Cr Ni Co Ag Pd Hg Au Crystallization (metals applied in the dentistry) high melting-point fragile precious metals low melting-point ductile Properties of metals -solid at room temperature (except Ga and Hg) chromium titanium iron - high luster - relatively high density (tightly packed crystal lattice) - large strength and toughness nickel cobalt - ability to be deformed under stress without cleaving (ductile) palladium - good electric and thermal conductivity silver gold mercury tin Microscopic structure of metals Submicroscopic structure of metals crystallites with different orientation, grains small homogeneous particles the properties of the material strongly depend on the structure hexagonal Ti, Cd, Co, Zn Space filling factor 74 % face-centered cubic Ag, Au, Pd, Pt, Al, Cu, Ni Space filling factor 74 % Stucture analysis: polishing (fine, rough) chemical etching microscopic technics body-centered cubic Fe, Cr Microscopic view of metal surfaces Space filling factor 68 % homogeneous Phase transitions Classification of the phase transitions: G = E + pV − TS Tm and Tb strongly depend on the type of bond between the particles heterogeneous Crystallization (phase transition from liquid to solid phase) cooling curve Supercooling (phase transition from liquid to solid phase) Transition from the liquid to the solid state two stages: a./ nucleus (seed crystal) formation b./ crystal growth nucleus formation growth of the crystallites solidus point dentritic (tree) increase liquidus point supercooling grain boundaries The role of the size and the shape of the grains !! isotrope increase Nucleus formation solid phase a./ homogeneous nucleation nucleous liquid phase important parameters: - free energy + manganese dentrites on a limestone critical radius of the nucleus r* ~r2 rate of nucleation nucleus (stable) Diffusive motion of atoms r embryo (unstable) snow crystal the size of the nucleus the rate of nucleus formation Driving force (number of nuclei) ~r3 Tm T b./ heterogeneous nucleation (on the wall of the dish, impurities, dislocations mainly earlier and faster crystallization) Crystallization The growth of the stable nuclei: glass formation rate of crystallization liquid specific volume a T = 540 °C fast nucleation and low low rate of nucleation and rate of crystal increase fast increase of crystal size b result T = 690 °C fine grain structure (a) rough grain structure (b) (Tm = 727 °C) harder, stronger, not easily ductile supercooled liquid glass crystal Tm T monocrystal glass Tg polycrystal rate of crystallization metals ceramics solid – solid state conversions !! Tm T Tm T
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