Sengierite
About Sengierite
An uncommon secondary mineral deposited from solutions derived from altering uraninite.
Visually very similar to volborthite.
Unique Identifiers
Classification of Sengierite
IMA Classification of Sengierite
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
H : V[5,6] Vanadates
B : Uranyl Sorovanodates
42 : HYDRATED PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
6 : A2(XO4)Zq·xH2O
21 : Vanadates (and vanadates with arsenate or phosphate)
4 : Vanadates of U, Mn, Fe or Ni
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Sgi | 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 Sengierite
On {001}, perfect
Optical Data of Sengierite
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. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Y = Olive-green to greenish yellow
Z = Yellowish green to colourless
Chemistry of Sengierite
Crystallography of Sengierite
β = 103.42°
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Big Balls | Small Balls | Just Balls | Spacefill
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| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0012070 | Sengierite | Piret P, Declercq J P, Wauters-Stoop D (1980) Structure cristalline de la sengierite Bulletin de Mineralogie 103 176-178 | 1980 | Shinkolobwe, Zaire | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 9.82 Å | (vvs) |
| 4.91 Å | (vs) |
| 3.735 Å | (s) |
| 3.197 Å | (s) |
| 3.179 Å | (s) |
| 3.144 Å | (s) |
| 3.094 Å | (s) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47e : [Vanadates, chromates, manganates] | |
| 47f : [Uranyl (U⁶⁺) minerals] |
Type Occurrence of Sengierite
Other Language Names for Sengierite
Relationship of Sengierite to other Species
| Carnotite | K2(UO2)2(VO4)2 · 3H2O | Mon. 2/m : P21/b |
| Margaritasite | (Cs,K,H3O)2(UO2)2(VO4)2 · H2O | Mon. 2/m : P21/b |
| Metatyuyamunite | Ca(UO2)2(VO4)2 · 3H2O | Orth. mmm(2/m2/m2/m) |
| Metavanuralite | Al(UO2)2(VO4)2(OH) · 8H2O | Tric. |
| Strelkinite | Na2(UO2)2(VO4)2 · 6H2O | Orth. |
| Tyuyamunite | Ca(UO2)2(VO4)2 · 5-8H2O | Orth. mmm(2/m2/m2/m) : Pnna |
| Vanuralite | Al(UO2)2(V2O8)(OH) · 11H2O | Mon. 2/m |
Common Associates
| 9 photos of Sengierite associated with Chalcocite | Cu2S |
| 5 photos of Sengierite associated with Brochantite | Cu4(SO4)(OH)6 |
| 5 photos of Sengierite associated with Malachite | Cu2(CO3)(OH)2 |
| 4 photos of Sengierite associated with Tyuyamunite | Ca(UO2)2(VO4)2 · 5-8H2O |
| 3 photos of Sengierite associated with Volborthite | Cu3(V2O7)(OH)2 · 2H2O |
| 3 photos of Sengierite associated with Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| 3 photos of Sengierite associated with 'Manganese Oxides' | |
| 2 photos of Sengierite associated with Talc | Mg3Si4O10(OH)2 |
| 2 photos of Sengierite associated with 'Schist' | |
| 2 photos of Sengierite associated with Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
Related Minerals - Strunz-mindat Grouping
| 4.HB.X | Spanoite | Tl2[(UO2)2(V2O8)] |
| 4.HB.05 | Margaritasite | (Cs,K,H3O)2(UO2)2(VO4)2 · H2O |
| 4.HB.05 | Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| 4.HB.15 | Francevillite | Ba(UO2)2(VO4)2 · 5H2O |
| 4.HB.15 | Fritzscheite | Mn2+(UO2)2(VO4,PO4)2 · 4H2O |
| 4.HB.15 | Curienite | Pb(UO2)2(VO4)2 · 5H2O |
| 4.HB.15 | Finchite | Sr(UO2)2(V2O8) · 5H2O |
| 4.HB.20 | Vanuralite | Al(UO2)2(V2O8)(OH) · 11H2O |
| 4.HB.20 | Metavanuralite | Al(UO2)2(VO4)2(OH) · 8H2O |
| 4.HB.25 | Metatyuyamunite | Ca(UO2)2(VO4)2 · 3H2O |
| 4.HB.25 | Tyuyamunite | Ca(UO2)2(VO4)2 · 5-8H2O |
| 4.HB.30 | Strelkinite | Na2(UO2)2(VO4)2 · 6H2O |
| 4.HB.35 | Uvanite | U6+2V5+6O21 · 15H2O (?) |
| 4.HB.40 | Rauvite | Ca(UO2)2(V10O28) · 16H2O |
| 4.HB.45 | Vandermeerscheite | K2[(UO2)2V2O8] · 2H2O |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 47.3634% | 11,840,850 | 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
Other Information
Internet Links for Sengierite
Please feel free to link to this page.
References for Sengierite
Localities for Sengierite
Showing 20 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.
Argentina | |
| Brodtkorb +1 other reference |
Czech Republic | |
| Pauliš P. et al. (Kutna Hora, issue 1) |
| Desor (05/2022) +1 other reference |
DR Congo | |
| Deliens (1996) |
| KMMA +3 other references |
| Wilson (2018) |
| KMMA +1 other reference | |
France | |
| |
Germany | |
| Kolitsch et al. (2005) |
Italy | |
| Balestra C. (2014) |
| Bonifazi (2021) |
Morocco | |
| Hutton (1957) |
Russia | |
| Pavel M. Kartashov analytical data 2012 |
Spain | |
| mineralsabella.blogspot.com (2009) +1 other reference |
| www.foro-minerales.com (n.d.) |
| www.foro-minerales.com (n.d.) | |
| www.foro-minerales.com (n.d.) |
USA | |
| Hutton (1957) +2 other references |
| Carnegie Museum of Natural History ... |
| Desor (10/2024) |






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The
Luiswishi Mine, Kawama, Kipushi Territory, Haut-Katanga, DR Congo