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trona
EntityQ253023· pop 23· linked from 75 articles

Trona (trisodium hydrogendicarbonate dihydrate, also sodium sesquicarbonate dihydrate, Na2CO3·NaHCO3·2H2O) is a non-marine evaporite mineral. It is mined as the primary source of sodium carbonate in the United States, where it has replaced the Solvay process used in most of the rest of the world for sodium carbonate production. Turkey is also a major producer.

Key facts

Mineral.name
Trona
Mineral.category
Carbonate mineral
Mineral.image
Trona(small).jpg
Mineral.imagesize
260px
Mineral.formula
Na2CO3·NaHCO3·2H2O
Mineral.IMAsymbol
Tn
Mineral.strunz
5.CB.15
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m)(same H-M symbol)
Mineral.symmetry
C2/c (no. 15)
Mineral.color
Colorless (in transmitted light) or white, grey-white, also grey to yellowish grey, light yellow
Mineral.habit
Columnar, fibrous and massive.
Mineral.cleavage
[100] perfect, [111] and [001] indistinct
Mineral.fracture
Brittle – subconchoidal
Mineral.mohs
2.5
Mineral.luster
Vitreous
Mineral.refractive
nα = 1.412 nβ = 1.492 nγ = 1.540
Mineral.opticalprop
Biaxial (−)

via Wikipedia infobox

~4 min read

Encyclopedic overview

7 sections
Contents
  • Etymology
  • Natural deposits
  • Crystal structure
  • Uses
  • Mining operations
  • See also
  • References

Trona (trisodium hydrogendicarbonate dihydrate, also sodium sesquicarbonate dihydrate, Na2CO3·NaHCO3·2H2O) is a non-marine evaporite mineral. It is mined as the primary source of sodium carbonate in the United States, where it has replaced the Solvay process used in most of the rest of the world for sodium carbonate production. Turkey is also a major producer.

== Etymology == The word entered English by way of either Swedish () or Spanish (), with both possible sources having the same meaning as in English: the mineral natron from North Africa. Both the Spanish and Swedish terms derive from the Arabic trōn, which comes from ancient Greek (nitron), derived ultimately from Ancient Egyptian ntry (or nitry).

Excerpted from Wikipedia’s “trona” article, available under the CC BY-SA 4.0 licence.

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