Crystalline Solids
Have well-defined shapes.
Particles (atoms, molecules, ions) are arranged in an orderly manner.
Example minerals: Wulfenite, Barite, Beryl, Quartz.
Amorphous Solids
Have poorly defined shapes.
Particles lack a consistent arrangement.
Crystals consist of tightly packed particles in a 3-D array.
Crystal Lattice
Formed from identical spheres positioned at lattice points.
Each point has identical surroundings.
Unit Cell
Fundamental building block of the crystal structure.
When the unit cell repeats in 3D, it forms the complete crystal.
Examples of analogies: checkerboard, tiled floor.
There are 7 crystal systems and several types of unit cells; focus on the cubic system.
Coordination Number: Number of nearest neighbors of a particle in a crystal.
Simple Cubic Unit Cell:
8 corner particles; coordination number = 6.
Contains 1 total particle.
Body-Centered Cubic Unit Cell:
8 corner particles + 1 in the center; coordination number = 8.
Total of 2 particles.
Face-Centered Cubic Unit Cell:
8 corner particles + 6 face-centered particles; coordination number = 12.
Total of 4 particles.
Packing Efficiency: Percentage of unit cell volume occupied by spheres.
Simple Cubic (52%):
Inefficient packing due to gaps between layers.
Body-Centered Cubic (68%):
Improved packing by aligning layers above gaps.
Cubic and Hexagonal Closest Packing (74%):
Efficient arrangements with high packing efficiency.
Coordination number: 12 for both configurations.
X-Ray Diffraction Analysis:
Diffraction of x-rays helps to determine distances and angles in crystal lattices.
Bragg's equation relates to the spacing of crystal layers.
Scanning Tunneling Microscopy:
Allows observation of surfaces at the atomic scale.
Generates 3D maps based on electron tunneling near surfaces.
Atomic Solids
Formed by noble gases with weak dispersion forces.
Low melting and boiling points.
Molecular Solids
Formed by molecules; physical properties vary by intermolecular forces (dipole-dipole, H bonding).
Generally higher melting points than atomic solids.
Ionic Solids
Comprise cations and anions with high melting points due to strong ionic bonds.
Low conductivity in solid state, but conduct when melted.
Metallic Solids
Exhibit metallic bonding and delocalized electrons, providing high conductivity and malleability.
Network Covalent Solids
Atoms covalently bonded in a network; very high melting points, varying conductivity.
Noncrystalline materials with some ordered regions, like rubber or glass.
Formed by rapid cooling from a molten state, preventing crystallization.
Band theory explains the behavior of metals and conductivity based on the formation of valence and conduction bands.
Valence Band: Lower energy orbitals occupied by valence electrons.
Conduction Band: Higher energy orbitals; electrons can easily transition to this band, allowing conductivity in metals.
Crystalline solids have repeated unit cells in their structure.
Unit cell types include simple, body-centered, and face-centered cubic; highest packing is in face-centered and hexagonal packing.
X-ray diffraction provides crystal data and atomic measurements.
Different types of solids exhibit varying physical properties driven by their unique bonding and structure.