Hydrohalite
Chemical formula: NaCl·2H₂O
Hydrohalite is hydrated sodium chloride, which forms at low temperatures from brines and is stable only below 0.1°C.
Properties
- Mohs hardness
- 1.5-2
- Color
- Colorless to white
- Luster
- Vitreous
- Streak
- White
- Density
- 0
- Cleavage
- Perfect on {110}
- Fracture
- Conchoidal
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification The key diagnostic feature of hydrohalite is its instability at room temperature. Observing the mineral melting at a temperature slightly above 0°C, leaving a white halite residue, is unequivocal proof. Under refrigerated conditions, its needle-like crystals can be observed. It has a salty taste. ## Distinguishing from Similar Minerals - **Halite (rock salt):** Halite is stable at room temperature and forms cubic crystals. Hydrohalite melts, leaving halite behind. - **Ice (H₂O):** Ice melts at 0°C, leaving no residue. Hydrohalite melts at a similar temperature but leaves a salt residue. - **Other evaporites:** Most other salt minerals (e.g., sylvite, gypsum) are stable under normal conditions. ## Crystal Forms Hydrohalite most often forms elongated, needle-like or prismatic crystals. It also occurs as fibrous aggregates, radial aggregates, and crusts.
Geological environment
## Genesis Hydrohalite crystallizes from highly concentrated aqueous solutions of sodium chloride (brines) at temperatures below 0.1°C. It is a typical cryogenic mineral. It forms seasonally in some salt lakes in cold climates and polar regions, precipitating from seawater under ice. ## Mineral Associations It most commonly co-occurs with halite (as a product of its decomposition), ice, mirabilite, gypsum, and other evaporites formed at low temperatures. ## Localities Due to its instability, confirmed localities are few. It has been observed in salt lake sediments, including the Great Salt Lake in Utah (USA), in Siberia (Russia), and in sediments from the bottom of the Caspian Sea. Its presence has also been found as inclusions in quartz crystals from Austria and in sea ice in Antarctica and the Arctic.
Rarity
Very rare
For collectors
## Quality Criteria Hydrohalite specimens practically do not exist on the collector's market due to extreme storage requirements. Its scientific value is much greater than its collector's value. Theoretically, a well-formed, large, and transparent crystal preserved under refrigerated conditions would be an object of immense value to research institutions. ## Market Prices No data on the commercial market for this mineral. ## Popular Localities This mineral does not come from any "popular" localities in the collector's sense. Specimens for research are obtained during scientific expeditions to polar regions or salt lakes during winter periods.
Care and storage
## Cleaning Hydrohalite specimens are not cleaned due to their extreme instability. Any contact with water or heating above 0°C will cause its immediate decomposition. ## What to Avoid Temperatures above 0°C must be absolutely avoided. The mineral must be stored under refrigerated conditions. It is sensitive to changes in humidity and direct light, which can heat it. It should not be touched with bare hands, as body heat will cause it to melt. ## Storage The only effective storage is to keep the specimen in an airtight container in a freezer, at a constant sub-zero temperature. Display is practically impossible outside of specialized laboratory conditions.