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Leydetite

A valid IMA mineral species
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About LeydetiteHide

00560710017272472257462.jpg
Jean-Claude Leydet
Formula:
Fe(UO2)(SO4)2 · 11H2O
Colour:
Yellow to greenish
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
2.55 (Calculated)
Crystal System:
Monoclinic
Name:
Honours Jean-Claude Leydet (born 18 April 1961 - died 21 November 2018), an amateur mineralogist from Brest (France), a great connoisseur of uranium minerals.
New structure type. Chemically related to deliensite.
Chemically very similar to rietveldite (a lower hydrate).

Isostructural with magnesioleydetite.

The structure is based on protasite anion topology; there is a sheet of UO7 bipyramids, that share four of their equatorial vertices with sulfate tetrahedra; thus, each tetrahedron has two vertices shared with UO7. The unshared equatorial vertices contain water molecules. The sheets are perpendicular to c. Fe ions and water molecules in the interlayer space link to the sheets via hydrogen bonds.


Unique IdentifiersHide

Mindat ID:
43586
Long-form identifier:
mindat:1:1:43586:8

IMA Classification of LeydetiteHide

Approved
IMA Formula:
Fe2+(U6+O2)(S6+O4)2(H2O)8·3H2O
Approval year:
2012
First published:
2013

Classification of LeydetiteHide

7.EB.15

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

Physical Properties of LeydetiteHide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Yellow to greenish
Streak:
Yellowish white
Hardness:
Cleavage:
Perfect
Perfect cleavage on (001).
Density:
2.55 g/cm3 (Calculated)

Optical Data of LeydetiteHide

Type:
Biaxial
RI values:
nα = 1.513(2) nβ = 1.522(2)
Surface Relief:
Unknown
Pleochroism:
Non-pleochroic
Comments:
Further optical properties could not be measured.

Chemistry of LeydetiteHide

Mindat Formula:
Fe(UO2)(SO4)2 · 11H2O
Element Weights:
Element% weight
O46.915 %
U33.237 %
S8.955 %
Fe7.798 %
H3.096 %

Calculated from ideal end-member formula.
O
U
S
Fe
H
Common Impurities:
Mg

Crystallography of LeydetiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Cell Parameters:
a = 11.3173 Å, b = 7.7258 Å, c = 21.8121 Å
β = 102.383°
Ratio:
a:b:c = 1.465 : 1 : 2.823
Unit Cell V:
1,862.78 ų (Calculated from Unit Cell)
Z:
4
Comment:
C2/c

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.625 Å(100)
6.277 Å(1)
5.321 Å(66)
3.549 Å(5)
2.663 Å(4)
2.131 Å(2)
Comments:
From Type Description.

Geological EnvironmentHide

Paragenetic Mode(s):

Type Occurrence of LeydetiteHide

General Appearance of Type Material:
Tabular crystals up to 2 mm.
Place of Conservation of Type Material:
Musée Cantonal de Géologie, Lausanne, Switzerland, registration number MGL 92661.
Geological Setting of Type Material:
Supergene alteration of a uranium deposit in sandstones, pelites and conglomerates.
Associated Minerals at Type Locality:

Synonyms of LeydetiteHide

Other Language Names for LeydetiteHide

Dutch:Leydetiet
German:Leydetit

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Leydetite associated with GypsumCaSO4 · 2H2O

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.05Meitnerite(NH4)(UO2)(SO4)(OH) · 2H2OTric. 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.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) 33.2366% 8,309,150 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.

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
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 LeydetiteHide

Not fluorescent.

Other InformationHide

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 LeydetiteHide

References for LeydetiteHide

Localities for LeydetiteHide

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.
France (TL)
 
  • Occitanie
    • Hérault
      • Lodève
        • Lodève
Williams et al. (2013) +1 other reference
  • Pays de la Loire
    • Loire-Atlantique
      • Nantes
        • Gétigné
Plášil et al. (2012) +1 other reference
USA
 
  • Utah
    • San Juan County
      • Red Canyon Mining District
Kampf et al. (2018)
 
and/or  
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