The pH Scale
The pH scale is a logarithmic scale used to measure the acidity or alkalinity of a solution. It quantifies the concentration of hydrogen ions (H⁺) in a solution, providing a way to express how acidic or basic a solution is. The scale ranges from 0 to 14:
- Acidic Solutions: Solutions with a pH less than 7 have a higher concentration of H⁺ ions than OH⁻ ions.
- Neutral Solutions: A pH of 7 indicates a balanced concentration of H⁺ and OH⁻ ions, typical of pure water.
- Basic Solutions: Solutions with a pH greater than 7 have a higher concentration of OH⁻ ions than H⁺ ions.
The formula for calculating pH is given by:
pH = -log₁₀[H⁺]
In dilute solutions, this calculation shows how the concentration of H⁺ ions in a solution affects its acidity. For instance, a solution of HCl with a concentration of 0.01 M has a pH of 2. Additionally, water has a constant ionic product, Kw, which at 25 °C (298 K) is 1.0 × 10⁻¹⁴, leading to the relationship:
pH + pOH = 14
Understanding the pH scale is critical in fields such as chemistry, biology, and environmental science as it affects various chemical reactions and biological processes.