Sabugalite

IMA-GP
Uranium 40.2a.24.1
(Dana Classification Number)
(Images) 7/E.01-20
(Strunz ID)

Property Data Remarks
Named for: Sabugal, Beira Baixa Province, Vila Real District, Portugal, its type locality
Alternate
    Name(s):
  • Aluminium-Autunite
  •  
    Mineral Class:
    Phosphates, Arsenates and Vanadates
      Uranylphosphates and uranylvanadates with
    [UO2]2+ - [PO4 | AsO4]3- and
    [UO2]2+ - [V2O8]6-
        Autunite group
     
    Chemical
        Formula:
    HAl(UO2)4(PO4)4 · 16H2O
    or:
    (AlH)0.5[(UO2) | (PO4)]2 · 8H2O      † 
     
    Chemical
        Composition:
    Aluminum: (Al) 1.52%
    Hydrogen: (H) 1.87%
    Oxygen: (O) 36.03%
    Phosphorus: (P) 6.98%
    Uranium: (U) 53.60%
    by weight
    Molecular
        Weight:
    1,776.23 daltons (amu)
    Specific
        Radioactivity:

    (All radiation is for a 1 gram, fully aged specimen)

    Specific Activity Dose Rate
    Becquerels Curies milliRems/hour microSieverts/hour
    9.5950 × 1004 2.59 × 10-06 1.34 134.30

    Estimated Average Annual Exposure: 360 mRem (3.6 milliSieverts)

    Crystalography:
    System:   Tetragonal - Ditetragonal Dipyramidal Monoclinic      † 
    Axial Ratios: a: 1 1.97459      † 
    b:   1      † 
    c: 2.77298 1.0010      † 
    Cell Dimensions: a: 6.96 Å 19.43 Å      † 
    b:   9.84 Å      † 
    c: 19.3 Å 9.85 Å      † 
    Z: 1 4      † 
    b:   96.167°      † 
    V: 934.92 Å3  
    DenCalc: 3.15  
    H-M Symbol:   4/m 2/m 2/m  
    Space Group:   I4/mmm C2/m      † 
    X-Ray Diffraction:
      By Intensity ( I/Io )
    (1): 9.69 Å 3.73 Å      †   ‡ 
    (0.9): 4.86 Å 3.47 Å      †   ‡ 
    (0.8): 3.47 Å 4.90 Å      †   ‡ 
    (0.7):   3.36 Å      †   ‡ 
    Sabugalite
    Crystal


    (As Observed - Monoclinic)
    Habit:
  • Square, flat plates
  • Agregate crusts      † 
  •  
    Cleavage:
    [001] Perfect
    [010]  
    [100]  
     
    Fracture:    
    Moh's
        Hardness:
    2.5  
    Density: 3.2 grams/cm3
    Color: Light Yellow  
    Streak: Yellow white  
    Luster: Vitreous  
    Diaphaneity: Transparent to Translucent  
    Pleochroism:
    (x): Colorless
    (y:) Colorless
    (z:) Colorless
     
    Ultra Violet
        Fluorescence:
    Long Wave: Intense Lemon Yellow      † 
    Short Wave: Intense Lemon Yellow      † 
     
    Magnetism: Non-magnetic  
    Occurance:
  • Uranium bearing sandstones of the Colorado Plateau
  •  
    Associated
        Minerals:

    Arsenopyrite, Autunite, Barite, Bassetite, Chalcopyrite, Chernikovite, Coffinite, Dewindtite, Galena, 'Gummite', Hematite, Meta-Autunite, Metatorbernite, Phosphuranylite, Pitchblende, Pyrite, Quartz, Saléeite, Torbernite, Uraninite, Uranocircite, Uranophane

    Mineral   -   > 50% of sites
    Mineral   -   > 35% of sites
    Mineral   -   > 20% of sites
    Minerals   -   Uranium & Thorium
    mineral links

    These are minerals known to be found with Sabugalite
    Locations:

    Somewhat rare

    Sabugalite Locations
    Notes:

    Strongly radioactive a- and b-particles, g-rays.

    A Potassium-rich variety also exists.  † 

    Crystals are probably metamict.

     †  J.H. Bernard and J. Hyrsl, Minerals and their Localities.
     ‡  Synthetic mineral used.

    Sabugalite Images

    Specimen Top

      (001aa) (001ab)  
       
    (001a) (001b) (001c) (001d)

     
      (001e) (001f)  
       
    Sabugal County, Beira Alta Province, Portugal

    Specimen Notes

    Occurrence - The Sabugalite occurs on a partially metamorphosed high density sandstone.

    Images (001aa) and (001ab) were 'taken' using a flatbed scanner.

    The specimen is roughly shaped like a triangular prism.

    Crystals - The crystals are flat plates, most showing non-90° corners. This non-square form has to be carefully looked for in the images, best done using a reference square. This lends credibility to the Monoclinic form given by Bernard and Hyrsl.   † 

     

    Appearence - The crystals show striations parallel to the (010) and (100) axes. Striations also occur along the (110) axes, and on some crystals, these are the predominate directions, as best seen in image (001d). It is suspected that on these crystals, the axes of the striations are (010) and (100), and the crystal edges are (110). These crystals are also fragmentary.

    Diaphaniety - The crystals varry from subtransparent to translucent.

    Luster - The main pinacoid is viteous in luster. The crystals are too thin ti accurately determine the luster of the edges.

     

      -  

     

    Specimen Physical Properties
    Size   cm   cm   cm
    Weight: x grams    
    g-Radiation Level:   cmp   msieverts background: 20 cpm