Incongruent melting

From Wikipedia, the free encyclopedia

Incongruent melting occurs when a substance does not melt uniformly and decomposes into another substance. For example, potassium feldspar (KAlSi₃O₈) decomposes to leucite (KAlSi₂O₆) when it melts. The decomposition is not complete, however. Most of the feldspar does melt, a portion of it decomposes to leucite and some quartz (SiO₂) is left over, since the chemical formulas of potassium feldspar and leucite differ by SiO₂. Another mineral that melts incongruently is enstatite (MgSiO₃), which decomposes to forsterite (Mg₂SiO₄). Enstatite does melt congruently between pressures of 2.5 and 5.5 kilobars.

[edit] See also

• Congruent melting
• Incongruent transition

[edit] References

This article does not cite any references or sources. (October 2006) Please help improve this article by adding citations to reliable sources. Unverifiable material may be challenged and removed.

[edit] External links

• Incongruent melting from Eric Weisstein's World of Physics