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Radium-bearing Barite

A variety of Baryte
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About Radium-bearing BariteHide

Formula:
(Ba,Ra)SO4
Colour:
White
Lustre:
Vitreous
Hardness:
3 - 3½
Crystal System:
Orthorhombic
Name:
From radium replacing barium and from the Greek, baryos, "heavy."
A "variety" of baryte containing trace amounts of radium.
The activity of 226Ra in the material from Ohře Rift area, Czech Republic, may reach 8 Bq/g. Scaly precipitates on oil industry equipment may show a radioactivity as high as 103 Bq/g (Ulrych et al., 2007).

See also under Hokutolite.


Unique IdentifiersHide

Mindat ID:
7267 (as Radium-bearing Barite)
549 (as Baryte)
Long-form identifier:
mindat:1:1:7267:6 (as Radium-bearing Barite)
mindat:1:1:549:0 (as Baryte)

Physical Properties of Radium-bearing BariteHide

Vitreous
Colour:
White
Streak:
White
Hardness:
3 - 3½ on Mohs scale

Optical Data of Radium-bearing BariteHide

Type:
Biaxial (+)
RI values:
nα = 1.634 - 1.637 nβ = 1.6355 - 1.638 nγ = 1.646 - 1.648
2V:
Measured: 36° to 40°, Calculated: 36° to 42°
Max. Birefringence:
δ = 0.011 - 0.012
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
weak

Chemistry of Radium-bearing BariteHide

Mindat Formula:
(Ba,Ra)SO4
Element Weights:
Element% weight
Ba58.840 %
O27.421 %
S13.739 %

Calculated from ideal end-member formula.
Ba
O
S

Crystallography of Radium-bearing BariteHide

Crystal System:
Orthorhombic

Synonyms of Radium-bearing BariteHide

Other Language Names for Radium-bearing BariteHide

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Radium-bearing Barite associated with BaryteBaSO4

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 Radium-bearing BariteHide

References for Radium-bearing BariteHide

Localities for Radium-bearing BariteHide

Showing 1 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.
Czech Republic
 
  • Moravian-Silesian Region
    • Karviná District
      • Orlová
        • ČSA Mine
Matýsek et al. (2026)
 
and/or  
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