Ammoniolasalite
Chemical formula: (N<sup>3-</sup>H<sub>4</sub>)<sub>2</sub>Mg<sub>2</sub>[V<sup>5+</sup><sub>10</sub>O<sub>28</sub>]·20H<sub>2</sub>O
Ammoniolasalite is a very rare, water-soluble magnesium ammonium decavanadate, forming aggregates of microscopic, acicular crystals.
Properties
- Luster
- Vitreous
- Streak
- Light yellow
- Cleavage
- Perfect on {010}
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Key diagnostic features include its pale yellow color, acicular or bladed crystal habit forming stellate aggregates, and its occurrence as efflorescences on sandstones. Water solubility is a confirming feature, but testing it destroys the sample. ## Distinguishing from Similar Minerals Ammoniolasalite can be confused with other secondary vanadium minerals, such as carnotite or tyuyamunite, which also have a yellow color and occur as coatings. Differentiation requires advanced analytical methods, such as Raman spectroscopy or X-ray diffraction (XRD). It differs from lasalite, to which it is similar, by the presence of ammonium ions. ## Crystal Forms The mineral forms very fine, acicular or bladed crystals, usually grouped into radial or stellate aggregates. It also occurs as powdery coatings and efflorescences.
Geological environment
## Genesis Ammoniolasalite is a secondary mineral, formed as a result of weathering processes of sedimentary rocks containing vanadium. It forms as an evaporitic product of waters rich in vanadium, magnesium, and ammonium ions in an arid climate. Its presence is associated with uranium-vanadium sandstones. ## Mineral Associations This mineral co-occurs with other secondary vanadates. At the type locality (Burro Mine), it was found in association with gypsum, huemulite, lasalite, rossite, and metarossite. ## Localities The only confirmed locality of ammoniolasalite in the world is its type locality – the Burro Mine (formerly Williams Mine) in San Miguel County, Colorado, USA.
Rarity
Extremely rare
For collectors
## Quality Criteria Due to its extreme rarity and microscopic crystal size, every analytically confirmed specimen is valuable. The most desirable samples are those with clearly visible, rich aggregates of stellate crystals on a piece of matrix rock. A contrasting sandstone matrix enhances aesthetic appeal. ## Popular Localities The only source of specimens is the Burro Mine in Colorado, USA. Material from this locality is extremely difficult to obtain and appears on the collector's market sporadically.
Care and storage
## Cleaning The mineral is water-soluble, so it must absolutely not be cleaned wet. Contact with any liquid should be avoided. Specimens can only be cleaned using compressed air (from a safe distance) or a very soft brush, with the utmost care. ## What to Avoid Contact with water, alcohol, and other chemicals must be strictly avoided. The mineral is sensitive to atmospheric moisture, which can lead to its slow degradation. It should be protected from temperature changes and direct sunlight. ## Storage Ammoniolasalite specimens must be stored in sealed, airtight containers (e.g., "perky box" type) with a desiccant (silica gel). They should be displayed away from sources of vibration, heat, and light.