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Meitnerite

A valid IMA mineral species
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About MeitneriteHide

01894210017272473058691.jpg
Photo of Lise Meitner
Formula:
(NH4)(UO2)(SO4)(OH) · 2H2O
Colour:
slightly greenish yellow
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
3.320 (Calculated)
Crystal System:
Triclinic
Name:
Named in honour of Lise Meitner (7 November 1878, Vienna, Austria – 27 October 1968, Cambridge, England, UK), an Austrian-Swedish physicist who worked on radioactivity and nuclear physics. Otto Hahn and Meitner led the small group of scientists who first discovered nuclear fission of uranium. Her exclusion from the 1944 Nobel Prize in Chemistry for nuclear fission (that was awarded exclusively to her long-time collaborator Otto Hahn) is considered unfair nowadays.
Structurally related to johannite.

Contains uranyl sulfate sheets based on the phosphuranylite anion topology. The interlayer region contains an NH4+ group and two H2O groups.


Unique IdentifiersHide

Mindat ID:
52180
Long-form identifier:
mindat:1:1:52180:0

Similar NamesHide

MeieriteA valid IMA mineral speciesBa44Si66Al30O192Cl25(OH)33
MeisseriteA valid IMA mineral speciesNa5(UO2)(SO4)3(SO3OH)(H2O)
MeixneriteA valid IMA mineral speciesMg6Al2(OH)16(OH)2 · 4H2O

IMA Classification of MeitneriteHide

Classification of MeitneriteHide

7.EB.05

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
E : Uranyl sulfates
B : With medium-sized cations

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
MneIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of MeitneriteHide

Vitreous
Transparency:
Transparent
Colour:
Slightly greenish yellow
Streak:
Very pale yellow
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
{011}
Fracture:
Irregular/Uneven
Density:
3.320 g/cm3 (Calculated)

Optical Data of MeitneriteHide

Type:
Biaxial (-)
RI values:
nα = 1.568(2) nβ = 1.589(2) nγ = 1.607(2)
2V:
Measured: 84° (1)
Max. Birefringence:
δ = 0.039
Based on recorded range of RI values above.

Interference Colours:
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 Âĩm 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.

Surface Relief:
Moderate (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

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.
Dispersion:
r > v, moderate
Comments:
X nearly colourless, Z pale green yellow, Y light green yellow
Comments:
The optical orientation is X∧b=26°, Y∧a=15°, Z∧c=53°.

Chemistry of MeitneriteHide

Mindat Formula:
(NH4)(UO2)(SO4)(OH) · 2H2O
Element Weights:
Element% weight
U54.448 %
O32.938 %
S7.335 %
N3.204 %
H2.075 %

Calculated from ideal end-member formula.
U
O
S
N
H

Crystallography of MeitneriteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 6.7964(2) Å, b = 8.0738(3) Å, c = 9.2997(7) Å
α = 113.284(8)°, β = 99.065(7)°, γ = 105.289(7)°
Ratio:
a:b:c = 0.842 : 1 : 1.152
Unit Cell V:
431.96 ÅÂģ (Calculated from Unit Cell)
Z:
2
Morphology:
flattened on {011}

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.15 Å(100)
6.36 Å(30)
5.85 Å(36)
5.038 Å(21)
3.569 Å(19)
3.451 Å(18)
3.340 Å(20)
3.075 Å(21)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47b : [Sulfates and sulfites]
47f : [Uranyl (Uâķ⁚) minerals]
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
52 : Guano- and urine-derived minerals<0.4
Stage 10b: Anthropogenic minerals<10 Ka
55 : Anthropogenic mine minerals

Type Occurrence of MeitneriteHide

General Appearance of Type Material:
intergrowths of tabular crystals
Place of Conservation of Type Material:
In the mineralogical collections of the Natural History Museum of Los Angeles County, Los Angeles, CA 90007, USA, catalogue number 66623
Associated Minerals at Type Locality:

Synonyms of MeitneriteHide

Other Language Names for MeitneriteHide

German:Meitnerit

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Meitnerite associated with Ammoniozippeite(NH4)2[(UO2)2(SO4)O2] · H2O

Related Minerals - Strunz-mindat GroupingHide

7.EB.BobcookiteNaAl(UO2)2(SO4)4 · 18H2OTric. 1 : P1
7.EB.ZincorietvelditeZn(UO2)(SO4)2(H2O)5Orth. mm2 : Pmn21
7.EB.ChenowethiteMg(H2O)6[(UO2)2(SO4)2(OH)2] · 5H2OOrth. mmm(2/m2/m2/m) : Cmcm
7.EB.IShinarumpite[Co(H2O)6][(UO2)(SO4)2(H2O)] · 4H2OMon. 2/m : P21/b
7.EB.Alwilkinsite-(Y)Y(UO2)3(SO4)2O(OH)3(H2O)7 · 7H2OOrth. 222 : P212121
7.EB.GurzhiiteAl(UO2)(SO4)2F · 10H2OTric. 1 : P1
7.EB.05JohanniteCu(UO2)2(SO4)2(OH)2 · 8H2OTric. 1 : P1
7.EB.10RietvelditeFe(UO2)(SO4)2(H2O)5Orth. mm2 : Pmn21
7.EB.10DeliensiteFe[(UO2)2(SO4)2(OH)2](H2O)7Orth. mm2 : Pnn2
7.EB.15StrassmanniteAl(UO2)(SO4)2F · 16H2OMon. 2/m : B2/b
7.EB.15LeydetiteFe(UO2)(SO4)2 · 11H2OMon. 2/m : P21/m
7.EB.15MagnesioleydetiteMg(UO2)(SO4)2 · 11H2OMon. 2/m : B2/b
7.EB.20Greenlizardite(NH4)Na(UO2)2(SO4)2(OH)2 · 4H2OTric. 1 : P1
7.EB.25MarkcooperitePb2(UO2)(TeO6)Mon. 2/m : P21/b

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 54.4481% 13,612,025 Îą, Îē, Îģ
Thorium (Th) 0.0000% 0 Îą, Îē, Îģ
Potassium (K) 0.0000% 0 Îē, Îģ

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 ÂĩSv/year. Note that natural background radiation averages around 2400 ÂĩSv/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.

Interactive Simulator:

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: –

DistanceDose rateRisk
1â€Ŋcm
10â€Ŋcm
1â€Ŋm

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 MeitneriteHide

greenish-white fluorescence in 405 nm light

Other InformationHide

Notes:
At room temperature, the mineral is slowly soluble in H2O and very rapidly soluble in dilute HCl
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for MeitneriteHide

References for MeitneriteHide

Localities for MeitneriteHide

Showing 3 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- 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). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Germany
 
  • Baden-WÞrttemberg
    • Freiburg Region
      • Waldshut
        • St Blasien
          • Menzenschwand
Mangold et al. (10/21)
USA
 
  • Utah
    • San Juan County
      • La Sal Mining District
Joe Marty Collection
      • Red Canyon Mining District
HÃĨlenius et al. (2017) +2 other references
 
and/or  
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