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单词 pH
释义
pH

Physics
  • See pH scale.


Chemistry
  • See pH scale.


Chemical Engineering
  • A measure of the acidity or alkalinity of a liquid based on the negative logarithm of the hydrogen ion concentration:

    pH=log101[H+]

    The scale ranges from 1.0 (highly acidic) to 14.0 (highly alkaline) with neutral solutions such as deionized water with a pH of 7.0. The scale was developed in 1909 by Danish chemist Søren Peder Lauritz Sørensen (1868–1939).


Biology
  • See ph scale.


Geology and Earth Sciences
  • The negative logarithm of the hydrogen ion concentration in a solution, pH = log10 1/H+. If the hydrogen ion concentration of a solution increases, as happens with increasing acidity, the pH will decrease, and vice versa. The pH is measured on a scale of 0–14; a neutral medium (such as pure water) has a pH of 7.0, numbers above 7.0 indicate relative alkalinity, numbers below 7.0 indicate relative acidity. Most pH values in natural systems lie in the range 4.0–9.0. Human blood has a pH of 7.4, ocean water 8.1–8.3, water in saline environments may have a pH around 9.0 or higher, while for water in acidic soils it may be as low as 4.0 or less.


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