Editorial Feature

Studenitsite - Occurrence, Properties, and Distribution

Studenitsite is a monoclinic-prismatic mineral containing calcium, boron, hydrogen, oxygen, and sodium. Studenitsite was named after the Studenitsa Cloister located near the area of first occurrence.

Properties of Studenitsite

The following are the key properties of studenitsite:

  • Cell Data
    • Space Group: P21/c
    • a = 11.4994(8)
    • b = 12.5878(9)
    • c = 10.5297(7)
    • β = 99.423(6)°
    • Z = 4
  • Crystal Data
    • Monoclinic
    • Point group: 2/m
    • Flattened wedge-shaped crystals- to 5 mm, dominated by {001}, {011}, {111}, with poorly developed {100}, {110}, {012}, in aggregates.
    • X-ray powder pattern: 3.04 (100), 3.35 (89), 5.41 (66), 3.27 (59), 2.210 (59), 5.20 (57), 4.20 (56)
  • Chemical Composition
    Elements Content 1 Content 2
    B2O3 59.64 59.28
    CaO 20.84 21.22
    H2O+ 13.64 -
    H2O - 13.64
    Na2O 5.96 5.86
    SiO2 0.09 -
    SrO 0.09 -
    K2O 0.08 -
    Al2O3 0.05 -
    Fe2O3 0.05 -
    MgO 0.02 -
    MnO 0.01 -
    H2O- 0.00 -
    CO2 0.00 -
    Total 100.47 100.00
  • Optical Properties
    • Optical Class: Biaxial (+)
    • Orientation: X = b; Z = a; Y ^ c = 10°
    • Dispersion: r > v, medium
    • α = 1.532(2)
    • β = 1.538(2)
    • γ = 1.564(2)
    • 2V(meas.) = 54(2)
  • Estimated Properties
    Electron density Bulk density (electron density)= 2.33 g/cm3
    note: Specific gravity of studenitsite = 2.33 g/cm3
    Photoelectric PEStudenitsite = 2.17 barns/electron
    U=PEStudenitsite x ρelectron density= 5.05 barns/cm3
    Fermion index Fermion index = 0.03
    Boson index = 0.97
    Radioactivity
     
    GRapi = 0 (Gamma Ray American Petroleum Institute Units)
    Studenitsite is not radioactive

How to Identify Studenitsite

Studenitsite can be identified in the field by its colorless to light dirty yellow or light gray color variations. The appearance of this mineral is transparent. It is a mineral with a glassy luster and a white streak. The fractures in the mineral are fragile. The mineral has striated-parallel lines on crystal surface or cleavage face. The crystals are wedge shaped. The density of studenitsite is 2.29 - 2.33 g/cm3 and hardness is 5.5-6 between knife blade and orthoclase.

Global Distribution

Studenitsite is widely distributed in Yugoslavia - From the Piskaya deposit, Yarondolskii Basin, on the Ibar River, 280 km south of Belgrade.

Occurrence of Studenitsite and Useful Mineral Association

Studenitsite is often associated with minerals such as howlite, colemanite, ulexite, and pentahydroborite.

Studenitsite occurs as lenses in clay and carbonate-bearing volcanogenic-sedimentary borate deposits.

References

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