Vandendriesscheite
About Vandendriesscheite
Unique Identifiers
IMA Classification of Vandendriesscheite
Classification of Vandendriesscheite
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
G : Uranyl Hydroxides
B : With additional cations (K, Ca, Ba, Pb, etc.); with mainly UO2(O,OH)5 pentagonal polyhedra
5 : OXIDES CONTAINING URANIUM OR THORIUM
8 : AX7O22·xH2O
7 : Oxides and Hydroxides
16 : Oxides of U
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Vdd | 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 Vandendriesscheite
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Optical Data of Vandendriesscheite
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.
Relative to Canada balsam mounting medium (n ≈ 1.537).
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
golden yellow
Chemistry of Vandendriesscheite
Crystallography of Vandendriesscheite
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0001951 | Vandendriesscheite | Burns P C (1997) A new uranyl oxide hydrate sheet in vandendriesscheite: Implications for mineral paragenesis and the corrosion of spent nuclear fuel American Mineralogist 82 1176-1186 | ![]() | 1997 | Shinkolobwe (Congo) | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 7.18 Å | (80) |
| 3.61 Å | (60) |
| 3.54 Å | (50) |
| 3.19 Å | (100) |
| 2.539 Å | (30) |
| 2.001 Å | (30) |
| 1.784 Å | (30) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Near-surface Processes | |
| 27 : Radioactive decay; auto-oxidation | |
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47f : [Uranyl (U⁶⁺) minerals] |
Type Occurrence of Vandendriesscheite
Other Language Names for Vandendriesscheite
Common Associates
| 40 photos of Vandendriesscheite associated with Uraninite | UO2 |
| 27 photos of Vandendriesscheite associated with Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
| 21 photos of Vandendriesscheite associated with Zircon | Zr(SiO4) |
| 16 photos of Vandendriesscheite associated with Microcline | K(AlSi3O8) |
| 11 photos of Vandendriesscheite associated with Schoepite | (UO2)8O2(OH)12 · 12H2O |
| 9 photos of Vandendriesscheite associated with Paulscherrerite | UO2(OH)2 |
| 8 photos of Vandendriesscheite associated with Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
| 6 photos of Vandendriesscheite associated with Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| 6 photos of Vandendriesscheite associated with Quartz | SiO2 |
| 5 photos of Vandendriesscheite associated with Fourmarierite | Pb(UO2)4O3(OH)4 · 4H2O |
Related Minerals - Strunz-mindat Grouping
| 4.GB.05 | Rameauite | K2Ca(UO2)6O6(OH)4 · 6H2O |
| 4.GB.05 | Agrinierite | K2(Ca,Sr)[(UO2)3O3(OH)2]2 · 5H2O |
| 4.GB.05 | Compreignacite | K2(UO2)6O4(OH)6 · 7H2O |
| 4.GB.10 | Becquerelite | Ca(UO2)6O4(OH)6 · 8H2O |
| 4.GB.10 | Billietite | Ba(UO2)6O4(OH)6 · 4-8H2O |
| 4.GB.10 | Protasite | Ba(UO2)3O3(OH)2 · 3H2O |
| 4.GB.15 | Richetite | (Fe3+,Mg)Pb 8.6(UO2)36O36(OH)24 · 41H2O |
| 4.GB.20 | Calciouranoite | (Ca,Ba,Pb)U2O7 · 5H2O |
| 4.GB.20 | Bauranoite | Ba(UO2)2(OH)6 · 1-2H2O |
| 4.GB.20 | Metacalciouranoite | (Ca,Ba,Pb,K2)U2O7 · 2H2O |
| 4.GB.25 | Fourmarierite | Pb(UO2)4O3(OH)4 · 4H2O |
| 4.GB.30 | Wölsendorfite | Pb7(UO2)14O19(OH)4 · 12H2O |
| 4.GB.35 | Masuyite | Pb(UO2)3O3(OH)2 · 3H2O |
| 4.GB.40 | Metavandendriesscheite | PbU7O22 · nH2O n < 12 |
| 4.GB.45 | Vandenbrandeite | Cu(UO2)(OH)4 |
| 4.GB.50 | Sayrite | Pb2(UO2)5O6(OH)2 · 4H2O |
| 4.GB.55 | Curite | Pb3(H2O)2[(UO2)4O4(OH)3]2 |
| 4.GB.60 | Iriginite | (UO2)Mo2O7 · 3H2O |
| 4.GB.65 | Uranosphaerite | Bi(UO2)O2(OH) |
| 4.GB.70 | Holfertite | CaxU6+2-xTi(O8-xOH4x) · 3H2O |
| 4.GB.75 | Carlosbarbosaite | (UO2)2Nb2O6(OH)2 · 2H2O |
| 4.GB.80 | Gauthierite | KPb[(UO2)7O5(OH)7] · 8H2O |
| 4.GB.85 | Kroupaite | KPb0.5[(UO2)8O4(OH)10] · 10H2O |
| 4.GB.90 | Leesite | K(H2O)2[(UO2)4O2(OH)5] · 3H2O |
| 4.GB.95 | Shinkolobweite | Pb1.333[U5+O(OH)(UO2)5O4.67(OH)5.33](H2O)5 |
| 4.GB.95 | Nollmotzite | Mg[U5+(U6+O2)2O4F3] · 4H2O |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 68.2430% | 17,060,750 | 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 Vandendriesscheite
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References for Vandendriesscheite
Localities for Vandendriesscheite
Showing 68 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 | |
| Linares |
Australia | |
| Henry et al. (2005) |
| Waite & Payne (1993) |
| Henry et al. (2005) |
Austria | |
| Strasser (1989) |
Canada | |
| Peatfield (n.d.) +1 other reference |
| Rich et al. (1977) |
| data.geology.gov.yk.ca (n.d.) |
China | |
| Wang (1992) |
| Zhu et al. (2019) |
Czech Republic | |
| Hloušek et al. (2002) |
| Möhn et al. (12/2021) | |
| Pauliš P. et al. (Kutna Hora, issue 1) |
| Pauliš P. et al. (Kutna Hora, issue 1) |
DR Congo (TL) | |
| Anderson (1978) +2 other references |
| Arliguie M collection |
France | |
| Meisser (2012) |
| |
| J. Chervet et G. Branche : ... +1 other reference | |
| |
| Bariand et al. (1993) +2 other references |
| Collection Frédéric Bonnet |
Germany | |
| Walenta (1992) |
| |
| |
| |
| Weiß (1990) |
| S Wolfsried collection |
| Gröbner et al. (2007) +1 other reference |
Hungary | |
| Zsombor Eva Collection |
Italy | |
| Probed Milan University 2006 |
| Campostrini et al. (2005) |
Norway | |
| Åmli (1969) |
Slovakia | |
| Ferenc et al. (2018) |
| Števko M. (2022) |
Spain | |
| mineralsabella.blogspot.de (n.d.) |
Sweden | |
| MinMag 46 |
| Welin (1965) |
Switzerland | |
| Stalder et al. (1998) |
| Stalder et al. (1998) |
| Stalder et al. (1998) |
| Meisser (2012) |
| Stalder et al. (1998) |
| Meisser (2012) | |
Tanzania | |
| |
UK | |
| Elton et al. (1995) |
| Braithwaite et al. (1990) |
| Knight (1978) +1 other reference | |
| R. S. W. Braithwaite and J. R. Knight (1990) +1 other reference |
USA | |
| Anthony et al. (1995) |
| Eckel et al. (1997) |
| Schooner (circa 1980s) |
| King et al. (1994) +1 other reference |
| Korzeb +3 other references |
| Segeler et al. (1981) |
| Rocks & Minerals 80:4 pp234-241 +1 other reference |
| Januzzi et al. (1976) |
| Frondel (1956) |
| Frondel (1956) |
| Frondel (1956) | |
| Frondel (1958) | |
| Frondel (1958) |
| Montgomery (Jan & May, 1970) +1 other reference |
| Smith et al. (2000) |
| Smith et al. (2000) | |
| Rocks & Min.:10:147 & 60:112 |
| Bullock (1981) |






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The
Shinkolobwe Mine, Shinkolobwe, Kambove Territory, Haut-Katanga, DR Congo