Ammoniozippeite
About Ammoniozippeite
Unique Identifiers
Classification of Ammoniozippeite
IMA Classification of Ammoniozippeite
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
E : Uranyl sulfates
C : With medium-sized and large cations
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Azip | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Ammoniozippeite
{010} and {001} perfect, {100} good
Optical Data of Ammoniozippeite
Based on recorded range of RI values above.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars.
Chemistry of Ammoniozippeite
Chemical Analysis
| Sample ID | Empirical Formula |
|---|---|
| 1 | [(NH4)1.97Na0.03]Σ2.00(U1.00O2)2(S1.01O4)O2·H2O |
| 2 | [(NH4)1.99K0.06Na0.04]Σ2.09(U1.01O2)2(S0.97O4)O2·H2O |
| 3 | [(NH4)1.96K0.11]Σ2.07[(UO2)2(SO4)1.98O2.06]·H2O |
| ID | Type | Locality | Reference | Notes |
|---|---|---|---|---|
| 1 | Type Specimen | Burro Mine, San Miguel County, Colorado, USA | Electron microprobe analyses (WDS mode) for Burro Mine | |
| 2 | Type Specimen | Blue Lizard Mine, Red Canyon Mining District, San Juan County, Utah, USA | Electron microprobe analyses (WDS mode) for Blue Lizard mine | |
| 3 | Jan Evangelista vein, Svornost Mine, Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic | empirical formula basis: 2 U atoms pfu |
Crystallography of Ammoniozippeite
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 7.17 Å | (100) |
| 4.270 Å | (13) |
| 3.670 Å | (14) |
| 3.580 Å | (21) |
| 3.489 Å | (42) |
| 3.138 Å | (63) |
| 1.750 Å | (14) |
| 1.697 Å | (18) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47b : [Sulfates and sulfites] | |
| Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
| 53 : Other minerals with taphonomic origins | <0.4 |
Type Occurrence of Ammoniozippeite
Synonyms of Ammoniozippeite
Other Language Names for Ammoniozippeite
Relationship of Ammoniozippeite to other Species
| Cobaltzippeite | Co(UO2)2(SO4)O2 · 3.5H2O | Mon. 2/m : B2/m |
| Magnesiozippeite | Mg(UO2)2(SO4)O2 · 3.5H2O | Mon. 2/m : B2/m |
| Natrozippeite | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O | Mon. 2/m : P21/m |
| Nickelzippeite | Ni2(UO2)6(SO4)3(OH)10 · 16H2O | Mon. |
| Plavnoite | K0.8Mn0.6[(UO2)2O2(SO4)] · 3.5H2O | Mon. 2/m : B2/m |
| Pseudojohannite | Cu3(UO2)4(SO4)2O4(OH)2 · 12H2O | Tric. 1 : P1 |
| Sejkoraite-(Y) | Y2(UO2)8(SO4)4O6(OH)2 · 26H2O | Tric. 1 : P1 |
| Zinczippeite | Zn(UO2)2(SO4)O2 · 3.5H2O | Mon. 2/m : B2/m |
| Zippeite | K3(UO2)4(SO4)2O3(OH) · 3H2O | Mon. 2 : B2 |
Common Associates
| 1 photo of Ammoniozippeite associated with Redcanyonite | (NH4)2Mn[(UO2)4O4(SO4)2](H2O)4 |
| 1 photo of Ammoniozippeite associated with Meitnerite | (NH4)(UO2)(SO4)(OH) · 2H2O |
Related Minerals - Strunz-mindat Grouping
| 7.EC. | Nitscheite | (NH4)2[(UO2)2(SO4)3(H2O)2] · 3H2O |
| 7.EC. | Beshtauite | (NH4)2(UO2)(SO4)2 · 2H2O |
| 7.EC. | Oldsite-(K) | K2Fe2+[(UO2)(SO4)2]2(H2O)8 |
| 7.EC. | Adolfpateraite | K(UO2)(SO4)(OH)(H2O) |
| 7.EC. | Libbyite | (NH4)2(Na2◻)[(UO2)2(SO4)3(H2O)]2 · 7H2O |
| 7.EC. | Seaborgite | LiK2Na6(UO2)(SO4)5(SO3OH)(H2O) |
| 7.EC.05 | Zinczippeite | Zn(UO2)2(SO4)O2 · 3.5H2O |
| 7.EC.05 | Zippeite | K3(UO2)4(SO4)2O3(OH) · 3H2O |
| 7.EC.05 | Cobaltzippeite | Co(UO2)2(SO4)O2 · 3.5H2O |
| 7.EC.05 | Nickelzippeite | Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| 7.EC.05 | Redcanyonite | (NH4)2Mn[(UO2)4O4(SO4)2](H2O)4 |
| 7.EC.05 | Natrozippeite | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| 7.EC.05 | Magnesiozippeite | Mg(UO2)2(SO4)O2 · 3.5H2O |
| 7.EC.05 | Plavnoite | K0.8Mn0.6[(UO2)2O2(SO4)] · 3.5H2O |
| 7.EC.10 | Rabejacite | Ca(UO2)4(SO4)2(OH)6 · 6H2O |
| 7.EC.10 | Svornostite-(NH4) | (NH4)2Mg(UO2)2(SO4)4(H2O)8 |
| 7.EC.10 | Svornostite-(K) | K2Mg[(UO2)(SO4)2]2(H2O)8 |
| 7.EC.15 | Sejkoraite-(Y) | Y2(UO2)8(SO4)4O6(OH)2 · 26H2O |
| 7.EC.15 | Marécottite | Mg3(UO2)8(SO4)4O6(OH)2 · 28H2O |
| 7.EC.15 | Hubbardite | Mg(H2O)6[(UO2)2O(OH)(SO4)]2 · 8H2O |
| 7.EC.20 | Pseudojohannite | Cu3(UO2)4(SO4)2O4(OH)2 · 12H2O |
| 7.EC.40 | Bluelizardite | Na7(UO2)(SO4)4Cl(H2O)2 |
| 7.EC.45 | Meisserite | Na5(UO2)(SO4)3(SO3OH)(H2O) |
| 7.EC.45 | Fermiite | Na4(UO2)(SO4)3 · 3H2O |
| 7.EC.45 | Oppenheimerite | Na2(UO2)(SO4)2 · 3H2O |
| 7.EC.50 | Feynmanite | Na(UO2)(SO4)(OH) · 3.5H2O |
| 7.EC.50 | Plášilite | Na(UO2)(SO4)(OH) · 2H2O |
| 7.EC.55 | Geschieberite | K2(UO2)(SO4)2 · 2H2O |
| 7.EC.60 | Ottohahnite | Na6(UO2)2(SO4)5(H2O)7 · 1.5H2O |
| 7.EC.65 | Péligotite | Na6(UO2)(SO4)4 · 4H2O |
| 7.EC.70 | Klaprothite | Na6(UO2)(SO4)4 · 4H2O |
| 7.EC.75 | Lussierite | Na10[(UO2)(SO4)4](SO4)2 · 3(H2O) |
| 7.EC.80 | Navrotskyite | K2Na10(UO2)3(SO4)9 · 2H2O |
| 7.EC.85 | Pseudomeisserite-(NH4) | (NH4)2Na4[(UO2)2(SO4)5] · 4H2O |
| 7.EC.90 | Wetherillite | Na2Mg(UO2)2(SO4)4 · 18H2O |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 65.9169% | 16,479,225 | α, β, γ |
| Thorium (Th) | 0.0000% | 0 | α, β, γ |
| Potassium (K) | 0.0000% | 0 | β, γ |
For comparison:
- Banana: ~15 Bq per fruit
- Granite: 1,000–3,000 Bq/kg
- EU exemption limit: 10,000 Bq/kg
Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.
Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!
Activity: –
| Distance | Dose rate | Risk |
|---|---|---|
| 1 cm | ||
| 10 cm | ||
| 1 m |
The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).
D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield
Fluorescence of Ammoniozippeite
Other Information
Internet Links for Ammoniozippeite
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References for Ammoniozippeite
Localities for Ammoniozippeite
Showing 11 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
All localities listed without proper references should be considered as questionable.
Czech Republic | |
| Desor (04/2022) |
France | |
| Matthies et al. (03/2023) |
Germany | |
| Joy Desor (SEM-EDS analysis) +1 other reference |
| Möhn et al. (01/2021) |
Hungary | |
| Eva Zsombor collection |
Switzerland | |
| Ansermet et al. (2026) |
USA (TL) | |
| Hålenius et al. (2017) +3 other references |
| Collection of Alex Earl |
| Hålenius et al. (2017) +3 other references |
| Kampf et al. (2018) | |
| EDS and XRD analyzed by Joy Desor. |






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The
Blue Lizard Mine, Red Canyon Mining District, San Juan County, Utah, USA