Arsenuranylite
Chemical formula: Ca(U<sup>6+</sup>O<sub>2</sub>)<sub>4</sub>(As<sup>5+</sup>O<sub>4</sub>)<sub>2</sub>(OH)<sub>4</sub>·6H<sub>2</sub>O
Arsenuranylite is a rare, highly radioactive secondary uranium mineral, forming characteristic yellow to orange-yellow coatings and crusts.
Properties
- Mohs hardness
- 2
- Luster
- Dull, Earthy, Vitreous
- Streak
- Light yellow
- Density
- 3.66-3.88
- Cleavage
- None
- Fracture
- Uneven
- Transparency
- Translucent to opaque
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Key diagnostic features include its bright, yellow-orange color, occurrence as earthy coatings and crusts in the oxidation zones of uranium deposits, and very strong radioactivity. Under shortwave ultraviolet light, it exhibits weak, green fluorescence. ## Distinguishing from Similar Minerals Arsenuranylite can be confused with other secondary uranium minerals of similar color, such as uranophane, autunite, or torbernite. Differentiation often requires chemical analysis (test for arsenic) or X-ray diffraction (XRD) studies. Compared to the often vitreous and better-formed crystals of autunite, arsenuranylite primarily forms earthy and dull aggregates. ## Crystal Forms Crystals are extremely rare and appear as microscopic, thin, hexagonal tablets or blades. It typically forms earthy, powdery, rosette-like, or radial aggregates, as well as thin crusts.
Geological environment
## Genesis Arsenuranylite is a secondary mineral, forming in the oxidation (weathering) zones of arsenic-rich uranium deposits. It forms as a result of the alteration of primary uranium minerals, such as uraninite, in the presence of arsenic-containing solutions. ## Mineral Associations It often co-occurs with other secondary uranium minerals, such as uranophane, phosphuranylite, torbernite, zeunerite, as well as with uraninite (as a primary mineral), quartz, and hematite. ## Localities Important localities worldwide include Lachaux (Puy-de-Dôme) in France (type locality); Rabejac mine in Hérault, France; Menzenschwand and Wittichen in the Black Forest, Germany; Jáchymov in the Czech Republic; and some deposits in Utah, USA.
Rarity
Rare
For collectors
## Quality Criteria Specimens with visible, even microscopic, crystals forming rosette-like or radial aggregates are most valued by collectors. Intense, bright color and contrast with the host rock are important. Due to its rarity, even rich coatings and crusts on rock matrix are considered valuable. ## Popular Localities Specimens from classic European localities, such as Menzenschwand in Germany or Rabejac in France, are particularly sought after by specialists collecting uranium minerals.
Care and storage
## Cleaning Arsenuranylite specimens should generally not be wet-cleaned. Dust and loose particles can be removed very carefully using a soft brush or a photographic air blower. Due to its fragility and softness, any mechanical contact should be avoided. ## What to Avoid Contact with water and chemicals must be strictly avoided. The mineral is sensitive to humidity changes. As a highly radioactive mineral, it requires special precautions – avoid inhaling dust and direct skin contact. Hands should be thoroughly washed after any contact. ## Storage Arsenuranylite specimens must be stored in sealed, clearly labeled containers with a radioactivity warning label. They should be kept away from other minerals that could be damaged by radiation. Store in a dry place, away from heat sources and areas of permanent human presence.