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Torbernite
Chemical Formula	Cu(UO2)2(PO4)2·8 - 12 H2O
Species	Phosphates
Crystal System	Tetragonal
Mohs Scale	2
Specific Gravity	3.2
Color	Emerald green to apple green
Streak	Pale green
Luster	Sub-Adamantine, Vitreous, Waxy, Pearly
Refractive Index	n = 1.590 - 1.592 n = 1.581 - 1.582
Diaphaneity	Transparent, Translucent
Cleavage	PerfectPerfect on micaceous, indistinct on
Fracture	Brittle
Crystal Habit：Tabular crystals; Foliated to earthy masses and encrustations
Geological Setting：Uncommon mineral in secondary zone of copper bearing uranium deposits.

Not to be confused with Tobermorite, a Calcium Silicate Hydrate (CSH), one of the main constituents of cement paste.

Not to be confused with Torbanite, also known as boghead coal, a variety of fine-grained black oil shale.

Torbernite, whose name derives from the Swedish chemist Torbern Bergman (1735-1784), is a radioactive, hydrated green copper uranyl phosphate mineral, found in granites and other uranium-bearing deposits as a secondary mineral. Torbernite is isostructural with the related uranium mineral, autunite.

The chemical formula of torbenite is similar to that of autunite in which a Cu²⁺ cation replaces a Ca²⁺. The number of water hydration molecules can vary between 12 and 8, giving rise to the variety of metatorbernite when torbernite spontaneously dehydrates. Their respective chemical compositions are the following:

Torbernite

Cu(UO₂)₂(PO₄)₂·12 H₂O

Metatorbernite

Cu(UO₂)₂(PO₄)₂·8 H₂O

Torbernite's most common alternative names are copper uranite and cupro-uranite.

Uses of torbernite

As a radioactive mineral, torbernite has some limited significance as a uranium ore. Its rich green color and well-developed distinctive crystals (size: mm to a few cm) make it a sought-after collector's mineral, as well. However, torbernite, like other hydrated minerals, can easily suffer from loss of water molecules. This loss of water from the mineral leads to an alteration of torbernite specimens into its pseudomorph, meta-torbernite. Some collector's websites assert than any torbernite specimen more than a few years old should be considered fully transitioned to meta-torbernite. However, it likely depends on the temperature and relative humidity of ambient air in which specimens are stored.

As torbernite is radioactive and outgas radon (²²²Rn), collectors are urged to take proper precautions in the handling and storage of any specimens. An adequate ventilation of the rooms and the cabinets in which the specimens are stored is essential to evacuate the radioactive radon gas responsible for lung cancer, but it could increase the dehydration rate of the specimens. To limit radon inhalation, naked specimens should never be stored in rooms in which one spends most of his living or working time. An alternative is to store specimens in gas tight transparent containers in which radon will accumulate and decay to secular equilibrium.

Associated minerals

Torbernite frequently occurs in conjunction with other uranium minerals, as well as host rock minerals. These associated minerals include:

• autunite, Ca(UO₂)₂(PO₄)₂ · 8 - 12 H₂O
• uraninite, UO₂
• uranophane, Ca(UO₂)₂Si₂O₇ · 6 H₂O
• uranocircite, Ba(UO₂)₂(PO₄)₂ · 8 - 12 H₂O
• topaz, Al[(F,OH)₂|SiO₄]

Identification

The most obvious factor in identifying torbernite is its radioactivity. However, since it is frequently found in association with other radioactive minerals, this may not be useful in separating one uranium mineral from the rest. A next step would be to check color. Most uranium-bearing minerals are bright yellow or green. As torbernite is exclusively green, this can be a useful secondary fact. Crystal habit is also useful, but as it shares a similar structure and color with autunite. Nonetheless, regardless of identification, it is likely that at least some of the specimen will have already altered to meta-torbernite.