Editorial Feature

Brendelite – Occurrence, Properties, and Distribution

Brendelite was named after Christian Friedrich Brendel (1776–1861), an expert in mining equipment, in Neustadtel-Schneeberg, Germany.

Properties of Brendelite

The following are the key properties of brendelite:

  • Cell Data
    • Space group: C2/m
    • a = 12.278(2)
    • b = 3.815(1)
    • c = 6.899(1)
    • β = 111.14(1)°
    • Z = 2
  • Crystal Data
    • Monoclinic
    • Point group: 2/m
    • Crystals are tabular {201}, showing also {100}, {010}, {001}, to 0.3 mm, in aggregates
    • X-ray powder pattern: 3.011 (100), 3.372 (77), 2.750 (62), 5.726 (54), 3.217 (46), 3.322 (37), 2.863 (34)
  • Chemical Composition
    Elements Content 1 Content 2
    Bi2O3 47.10 56.12
    PbO 26.08 18.12
    P2O5 10.71 10.98
    Fe2O3 9.44 6.32
    FeO 3.12 5.58
    H2O [1.46] [1.46]
    As2O5 0.32 0.20
    V2O5 0.24 0.55
    Total [98.47] [99.33]
  • Optical Properties
    • Optical class: Biaxial (-)
    • Pleochroism: Strong; X = pale brown to brown; Y = Z = dark brown to opaque
    • Orientation: Z = b; Y ≃a
    • α = [2.06]; β = [2.15]; γ = [2.19]
    • 2V(meas.) =70.5°
  • Estimated Properties
    Electron density Bulk density (electron density) = 5.83 g/cm3
    note: Specific gravity of brendelite = 6.83 g/cm3
    Photoelectric PEBrendelite = 1,255.52 barns/electron
    U=PEBrendelite x ρ electron density= 7,324.08 barns/cm3
    Fermion index Fermion index = 0.05
    Boson index = 0.95
    Radioactivity Brendelite is not radioactive

How to Identify Brendelite

Brendelite can be identified in the field by its color variations of black and dark brown. Its opaque to translucent form has no cleavage. This mineral has a vitreous - adamantine luster with light brown streak. The density of brendelite is 6.83 g/cm3 with a hardness of 4.5 - between fluorite and apatite.

Global Distribution

Brendelite is mainly distributed in the Guldener Falk mine, near Schneeberg, Saxony, Germany.

Occurrence of Brendelite and Useful Mineral Association

Brendelite occurs in a very rare secondary mineral found on the dumps of a Bi–Co–Ni–Ag deposit. It is often associated with minerals such as eulytite, bismutite, and bismutoferrite.

References

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