Alkalinity: Difference between revisions

From Glossary of Meteorology
m (Rewrite with Template:Term and clean up)
m (Rewrite with Template:Term and clean up)
 
Line 3: Line 3:
|Definitions={{Definition
|Definitions={{Definition
|Num=1
|Num=1
|Meaning=
|Meaning=The relative acidity of any solution expressed in a [[pH]] range of numbers.
The relative acidity of any solution expressed in a [[pH]] range of numbers.<br/> The pH value is the negative common [[logarithm]] of the hydrogen-ion concentration in a  solution, expressed in moles per liter of solution. A neutral solution, that is, one that is neither  acidic nor alkaline, such as pure water, has a concentration of 10 moles per liter; its pH is thus  7. Acidic solutions have pH values ranging with decreasing acidity from 0 to nearly 7; alkaline or  basic solutions have a pH ranging with increasing alkalinity from just beyond 7 to 14. In [[seawater]],  the alkalinity is a measure of the excess of [[hydroxyl ions]] over [[hydrogen ions]], generally expressed  as milliequivalents per liter.
|Explanation=The pH value is the negative common [[logarithm]] of the hydrogen-ion concentration in a  solution, expressed in moles per liter of solution. A neutral solution, that is, one that is neither  acidic nor alkaline, such as pure water, has a concentration of 10 moles per liter; its pH is thus  7. Acidic solutions have pH values ranging with decreasing acidity from 0 to nearly 7; alkaline or  basic solutions have a pH ranging with increasing alkalinity from just beyond 7 to 14. In [[seawater]],  the alkalinity is a measure of the excess of [[hydroxyl ions]] over [[hydrogen ions]], generally expressed  as milliequivalents per liter.
}}
}}
}}
}}

Latest revision as of 21:16, 13 January 2024

The relative acidity of any solution expressed in a pH range of numbers.

The pH value is the negative common logarithm of the hydrogen-ion concentration in a solution, expressed in moles per liter of solution. A neutral solution, that is, one that is neither acidic nor alkaline, such as pure water, has a concentration of 10 moles per liter; its pH is thus 7. Acidic solutions have pH values ranging with decreasing acidity from 0 to nearly 7; alkaline or basic solutions have a pH ranging with increasing alkalinity from just beyond 7 to 14. In seawater, the alkalinity is a measure of the excess of hydroxyl ions over hydrogen ions, generally expressed as milliequivalents per liter.


Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.