The is a logarithmic measurement used to determine how acidic or basic (alkaline) an aqueous solution is. Developed by scientist S.P.L. Sørensen in 1909, it typically ranges from 0 to 14 . Core Characteristics
: Values above 7 indicate basicity, with 14 being the most basic. ph scale
: Values below 7 indicate acidity, with 0 being the most acidic. The is a logarithmic measurement used to determine
: A pH of 7.0 is considered neutral (e.g., pure water). Core Characteristics : Values above 7 indicate basicity,
: Each whole number change represents a tenfold difference in hydrogen ion concentration. For example, a solution with a pH of 4 is 100 times more acidic than one with a pH of 6. Common Examples Classification Battery Acid Highly Acidic Lemon Juice Pure Water Seawater Slightly Basic Baking Soda Liquid Drain Cleaner Highly Basic Measurement Methods pH Scale | U.S. Geological Survey - USGS.gov