The pH scale is a fundamental concept in chemistry that measures the acidity or alkalinity of a solution, developed by Danish chemist Søren Sørensen in 1909 while working at the Carlsberg Laboratory.
The scale is based on the Ionenprodukt des Wassers (ion product of water), which describes water's ability to undergo self-ionization through a process called Autoprotolyse. This phenomenon results in the formation of hydronium (H3O+) and hydroxide (OH-) ions in pure water. The pH scale typically ranges from 0 to 14, with 7 being neutral, below 7 being acidic, and above 7 being basic or alkaline. The relationship between pH scale and concentration is logarithmic, meaning each unit change in pH represents a tenfold change in hydrogen ion concentration.
Understanding Stärke von Säuren und Basen (strength of acids and bases) is crucial in chemistry and biology. Starke und schwache Basen Liste (strong and weak bases list) includes common substances like sodium hydroxide (strong base) and ammonia (weak base). Schwache Säuren Beispiele (weak acid examples) include acetic acid and carbonic acid, while strong acids include hydrochloric acid and sulfuric acid. Ampholytes are substances that can act as both acids and bases, depending on the environment, playing crucial roles in biological systems. The Säure-Basen-Haushalt (acid-base balance) is particularly important in medical contexts, such as understanding Nicht titrierbare Säure Niere (non-titratable acid in kidneys) and maintaining proper body pH. This balance is maintained through various buffer systems in the body, which help prevent dangerous pH fluctuations that could otherwise disrupt vital biological processes.