Silicon is the second‑most abundant element in the Earth’s crust, accounting for 25.7 % by weight. It is primarily found in silicate minerals and sand, the latter being largely composed of silicon dioxide (SiO₂), commonly known as silica. Determining the weight‑percentage of silicon in silica is useful for geologists, materials scientists, and anyone working with silica‑based materials.
Locate the atomic masses of silicon (Si) and oxygen (O) in a reliable periodic table. Typical values are:
• Silicon (Si): 28.0855 u
• Oxygen (O): 15.9994 u
Silica’s formula, SiO₂, indicates one silicon atom bonded to two oxygen atoms. The molecular mass is therefore:
28.0855 (u Si) + 2 × 15.9994 (u O) = 60.0843 u
Divide the atomic mass of silicon by the molecular mass of silica, then multiply by 100 to express it as a percentage:
(28.0855 / 60.0843) × 100 ≈ 46.69 %
Thus, silica contains approximately 46.69 % silicon by weight.
Use the same procedure to determine silicon content in hydrated silica, such as silicic acid (SiO₂·2H₂O). Include the mass of water (18 u per molecule) in the calculation:
(28.0855 / [28.0855 + 2 × 15.9994 + 2 × 18]) × 100 ≈ 29.2 %
For more details on atomic masses and element properties, consult a reputable periodic table resource.