Mineral hydration: Difference between revisions

From Citizendium
Jump to navigation Jump to search
imported>Subpagination Bot
m (Add {{subpages}} and remove any categories (details))
mNo edit summary
 
Line 7: Line 7:
Some mineral structures, for example, [[montmorillonite]], are capable of including a variable amount of water without significant change to the mineral structure.
Some mineral structures, for example, [[montmorillonite]], are capable of including a variable amount of water without significant change to the mineral structure.


Hydration is the mechanism by which [[Portland cement]] develops strength.
Hydration is the mechanism by which [[Portland cement]] develops strength.[[Category:Suggestion Bot Tag]]

Latest revision as of 16:00, 19 September 2024

This article is a stub and thus not approved.
Main Article
Discussion
Related Articles  [?]
Bibliography  [?]
External Links  [?]
Citable Version  [?]
 
This editable Main Article is under development and subject to a disclaimer.

Mineral hydration is an inorganic chemical reaction where water is added to the crystal structure of a mineral, usually creating a new mineral, usually called a hydrate.

There are two main ways in which minerals hydrate. One is conversion of an oxide to a double hydroxide, as in the hydration of calcium oxide - CaO - to calcium hydroxide - Ca(OH)2, the other is incorporation of water molecules directly into the crystalline structure of the mineral, as in the hydration of feldspars to clay minerals.

Some mineral structures, for example, montmorillonite, are capable of including a variable amount of water without significant change to the mineral structure.

Hydration is the mechanism by which Portland cement develops strength.