Hydrohalite Explained

Hydrohalite
Category:Halide mineral
Formula:NaCl·2H2O
Imasymbol:Hhl[1]
Strunz:3.BA.05
System:Monoclinic
Class:Prismatic (2/m)
(same H-M symbol)
Symmetry:P21/c
Colour:Colourless or white
Diaphaneity:Transparent

Hydrohalite is a mineral that occurs in saturated halite brines at cold temperatures (below 0.1 °C). It was first described in 1847 in Dürrnberg, Austria. It exists in cold weather.

Hydrohalite has a high nucleation energy, and solutions will normally need to be supercooled for crystals to form. The cryohydric point is at . Above this temperature, liquid water saturated with salt can exist in equilibrium with hydrohalite. Hydrohalite has a strong positive temperature coefficient of solubility, unlike halite.[2] Hydrohalite decomposes at 0.1°C, giving a salty brine and solid halite. Under pressure, hydrohalite is stable between 7,900 and 11,600 atmospheres pressure. The decomposition point increases at the rate of 0.007K per atmosphere (for 1–1000 atmospheres).[2] The maximum decomposition temperature is at 25.8°C under 9400 atmospheres. Above this pressure the decomposition point goes down.[2]

Ceres

Hydrohalite was discovered on Ceres by Dawn,[3] suggesting an early ocean, possibly surviving as a relict ocean.

References

Notes and References

  1. Warr. L.N.. 2021. IMA–CNMNC approved mineral symbols. Mineralogical Magazine. 85. 3. 291–320. 10.1180/mgm.2021.43. 2021MinM...85..291W. 235729616. free.
  2. Book: Braitsch. O.. Salt Deposits Their Origin and Composition. The Stability Conditions of Salt Minerals. 1971. 42–44. 10.1007/978-3-642-65083-3_2. Springer. 978-3-642-65085-7.
  3. De Sanctis, M.C., Ammannito, E., Raponi, A. et al. Fresh emplacement of hydrated sodium chloride on Ceres from ascending salty fluids. Nat Astron 4, 786–793 (2020). https://doi.org/10.1038/s41550-020-1138-8