Solids
12.1
Crystal Structure:
Materials on Earth are crystals.
Crystals are arrays of atoms.
X-Rays confirm that crystals are three dimensional arrangements of atoms.
The atoms are very close together.
- They’re the same distance apart as X-ray wavelengths.
A beam of X-rays directed on a crystal gets diffracted into a characteristic pattern.
This pattern can be made visible on a photographic film.
- The pattern is a diffraction pattern.
- The film shows that crystals are mosaics of atoms located in regular lattices.
Iron, copper, gold → simple crystal structures
Tin, cobalt → slightly more complex structures
All metals have many crystals.
- Each crystal has the same regular lattice.
- Each is slightly inclined to the crystal nearby.
When metal surface is etched, the crystals can be seen.
Etched → cleaned with acid
- Crystal structures can be seen:
- On the surface of galvanized iron
- On brass doorknobs that get etched with perspiration from hands
- There’s a formula that shows how X-rays should scatter from the atomic layers in a crystal.
- This formula combines with the analysis of the pattern of spots in a diffraction pattern to find distances between atoms in a crystal.
X-ray diffraction is vital in biological and physical sciences.
- Non-crystalline solids are amorphous.
- Amorphous → atoms and molecules are distributed randomly.
- Particles can wander.
- Eg: Rubber, glass, plastic
- In all atoms, atoms and ions vibrate in their positions.
- Atoms are tied together by electrical bonding forces.
- Called atomic bonding.
- Types of bonding in solids:
- ionic
- covalent
- metallic
- van der Waals (the weakest)
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