Lecture Notes: Understanding Silicates and Aluminosilicates
Introduction
- Topic: Part 3 of 4.3 on Soils.
- Focus: Understanding silicon dioxide, silicates, and aluminosilicates.
- Importance: Key components of rocks and soils; constitute 92-93% of Earth's crust.
Composition of Earth's Crust
- Elements: Silicon and oxygen are the most abundant, followed by aluminum.
- Compounds: Silicates and aluminosilicates are prevalent due to this composition.
Structure of Silicates and Aluminosilicates
- Silicates:
- Based on SiO4 tetrahedra (1 silicon covalently bonded to 4 oxygen atoms).
- Formation of stable chains and rings through bonding.
- Aluminosilicates:
- Silicon atoms replaced by aluminum, increasing the net negative charge.
- Aluminum is considered a metalloid due to covalent bonding.
Types of Silicate Structures
- Ortho silicate: Single SiO4 unit.
- Di silicate: Two SiO4 units joined by one oxygen.
- Hexa silicate: Cyclic structure.
- Other Structures: Single chains, double chains, sheet structures, and continuous networks (e.g., in silicon dioxide).
Determining Charge of Silicate and Aluminosilicate Ions
Conclusion
- More practice examples will be covered in class.
- This concludes part 3 of 4.3. Next up is the final video in the series.
Note: Ensure to understand how to write formulas and balance charges using both methods as they are fundamental to comprehending silicates and aluminosilicates.