Pringleite – Occurrence, Properties and Distribution

Topics Covered

Introduction to Pringleite
Properties of Pringleite
How to Identify Pringleite
Global Distribution
Occurrence of Pringleite and Useful Mineral Association
References

Introduction to Pringleite

Pringleite is the triclinic dimorph of Ruitenbergite. It derived its name from Gordon J. Pringle, mineralogist, Geological Survey of Canada, Ottawa, Canada.

Chemical Formula – Ca9B26O34(OH)24Cl413H2O

Properties of Pringleite

The following are the key properties of Pringleite

  • Cell Data
    • Space Group: P1
    • a = 12.746
    • b = 13.019
    • c = 6.963
    • Z = 1
  • Crystal Data
    • Triclinic, pseudomonoclinic
    • Point Group: 1
    • Subhedral to anhedral crystals up to 2 mm in platy aggregates
    • X-ray powder pattern: 7.69 (100), 9.21 (70), 5.74 (60), 4.63 (40), 3.845 (35), 2.199 (30b), 2.058 (30)
  • Chemical Composition
    Elements Content 1 Content 2
    B2O3 46.75 45.94
    CaO 26.29 25.62
    Cl 6.48 7.2
    H2O [21.94] 22.86
    -O = Cl2 1.46 1.62
    Total [100] [100]
  • Optical Properties
    • Optical Class: Biaxial ()
    • α= 1.537 β= 1.548 γ= 1.570
  • Estimated Properties
    Electron density Bulk density (electron density)= 2.23 g/cm3
    note: Specific gravity of pringleite=2.21 g/cm3
    Photoelectric PEPringleite = 2.90 barns/electron
    U=PEPringleite x ρElectron Density= 6.49 barns/cc
    Fermion index Fermion Index = 0.02
    Boson Index = 0.98
    Radioactivity

    Pringleite is not radioactive

How to Identify Pringleite

Pringleite is transparent to translucent. It is colorless to very pale yellow. It is colorless in transmitted light and blue-gray in reflected light.

Global Distribution

Pringleite is distributed from the Potash Corporation of America mine, Penobsquis evaporite deposit, near Sussex, New Brunswick, Canada.

Occurrence of Pringleite and Useful Mineral Association

Pringleite occurs very rarely mostly in an evaporite deposit. Pringleite is associated with Hilgardite-1A, halite, ruitenbergite, sylvite, anhydrite, quartz and clays.

References


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