pH is a measure of the acidity (H+) or basicity (OH-) (alkalinity) of a particular solution. pH is technically defined as the negative logarithm of hydrogen ion concentration, symbolized as pH=-log[H+]. It is the ratio of hydrogen ions to hydroxide ions. It was introduced to avoid writing the molarity (moles of hydrogen ion per liter of solution) of a solution in an awkward manner. For example, a solution with 0.00000007 M of hydrogen ions can be written as a solution with pH 7. The concept of pH was first described by the Danish biochemist named Søren Peder Lauritz Sørensen of Carlsberg Laboratory in 1909. Some references state that the “p” in pH stands for “power”, others say that it stands for the German of “power” which is “potenz”, while others say that it is a constant.
The pH scale has a range of 0 to 14. Seven is considered the neutral pH where the concentration of hydrogen ions is equal to the concentration of hydroxide ions. Water has a pH of 7 at room temperature. When the pH is below 7, it means that the solution is acidic and the concentration of hydrogen ions exceeds the concentration of hydroxide ions. If the concentration of hydroxide ions is greater than the concentration of hydrogen ions, the solution is said to be basic or alkaline. An aqueous solution with pH of 6 is considered slightly acidic while a pH of 0 is considered extremely acidic. A solution with pH greater than 7 is considered basic where pH 14 is considered extremely basic.