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Volkovskite

A valid IMA mineral species
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About VolkovskiteHide

Formula:
KCa4[B5O8OH]4[B(OH)3]2Cl · 4H2O
Colour:
Colourless, pink; varying from pale to deep orange
Lustre:
Vitreous
Hardness:
2 - 2½
Specific Gravity:
2.27
Crystal System:
Triclinic
Name:
Named in honor of A.I. Volkovskaya (А.И. Волковской), Russian petrographer who first found the mineral in water insoluble residues from drill cores.

Volkovskite was first described from Kazakhstan [TL1] by Kondrat’eva et al. (1966), and redefined by Mandarino et al. (1990) from the Salt Spring deposit [TL2]. The redefinition established the triclinic symmetry and presence of K and Cl as essential constituents in the mineral.
Structurally related to Veatchite.


Unique IdentifiersHide

Mindat ID:
4202
Long-form identifier:
mindat:1:1:4202:0

IMA Classification of VolkovskiteHide

Classification of VolkovskiteHide

6.EC.20

6 : BORATES
E : Pentaborates
C : Phyllo-pentaborates
26.5.16.1

26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
5 : Pentaborates
10.1.14

10 : Borates with other anions
1 : Borates with halide

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference
VlkIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of VolkovskiteHide

Vitreous
Transparency:
Translucent
Colour:
Colourless, pink; varying from pale to deep orange
Hardness:
2 - 2½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
{010} and {100}
Fracture:
Splintery
Density:
2.27(3) g/cm3 (Measured)    2.28 g/cm3 (Calculated)

Optical Data of VolkovskiteHide

Type:
Biaxial (+)
RI values:
nα = 1.523 - 1.539 nβ = 1.539 - 1.540 nγ = 1.596 - 1.605
2V:
Measured: 14.6° , Calculated: 14.4°
Max. Birefringence:
δ = 0.066 - 0.073
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.

Surface Relief:
Moderate
Dispersion:
No dispersion
Optical Extinction:
Y = b; Z ∧ a = 31°.

Chemistry of VolkovskiteHide

Mindat Formula:
KCa4[B5O8OH]4[B(OH)3]2Cl · 4H2O
Element Weights:
Element% weight
O59.990 %
B19.387 %
Ca13.067 %
K3.187 %
Cl2.890 %
H1.479 %

Calculated from ideal end-member formula.

Crystallography of VolkovskiteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pedial
Space Group:
P1
Cell Parameters:
a = 6.575(2) Å, b = 23.921(8) Å, c = 6.522(2) Å
α = 90.58(3)°, β = 119.10(2)°, γ = 95.56(3)°
Ratio:
a:b:c = 0.275 : 1 : 0.273
Unit Cell V:
890.15 ų (Calculated from Unit Cell)
Z:
1
Morphology:
The crystals possess perfect cleavages occurring as thinly layered pseudohexagonal/triangular, elongated platy masses.

New Brunswick material: Pseudohexagonal, platy crystals tabular on {010}. Forms identified: {010}, {010}, {001}, {001}, {281}, {281} and {181}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0020421VolkovskitePoulin R S, Grice J D (2013) Volkovskite, a complex borate mineral: refined crystallographic data and optics The Canadian Mineralogist 51 157-1692013New Brunswick, Canada0293
0014191VolkovskiteRastsvetaeva R K, Andrianov V I, Genkina E A, Sokolova T N, Kashaev A A (1992) Crystal structure of volkovskite KCa4B22O32(OH)10Cl*4H2O from Nepkii deposit (E. Siberia) Kristallografiya 37 326-3331992Eastern Siberia0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.1 Å(100)
6.03 Å(60)
5.42 Å(60)
3.28 Å(90)
2.86 Å(60)
2.81 Å(70)
2.63 Å(80)
2.15 Å(70)
2.10 Å(60)
1.980 Å(70)
Comments:
Inder deposit, Kazakhstan. Data from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
25 : Evaporites (prebiotic)

Type Occurrence of VolkovskiteHide

General Appearance of Type Material:
Pseudohexagonal to triangular crystals and micaceous plates, to 1 cm.
Place of Conservation of Type Material:
A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia; Royal Ontario Museum, Toronto, Canada, M44196.
Geological Setting of Type Material:
Evaporite deposits.
Associated Minerals at Type Locality:

Other Language Names for VolkovskiteHide

German:Volkovskit
Simplified Chinese:沃硼钙石
Spanish:Volkovskita
Traditional Chinese:沃硼钙石

Common AssociatesHide

Associated Minerals Based on Photo Data:
18 photos of Volkovskite associated with HilgarditeCa2B5O9Cl · H2O

Related Minerals - Strunz-mindat GroupingHide

6.EC.CalcioveatchiteSrCaB11O16(OH)5 · 5H2OMon. 2 : P21
6.EC.05NasiniteNa2[B5O8(OH)] · 2H2OOrth. mmm (2/m 2/m 2/m)
6.EC.05BiringucciteNa2B5O8(OH) · H2OMon. 2/m : P21/b
6.EC.10GoweriteCa[B5O8(OH)][B(OH)3] · 3H2OMon. 2/m : P21/b
6.EC.15Veatchite-2MSr2B11O16(OH)5 · H2OMon. m : Bb
6.EC.15Veatchite-ASr2B11O16(OH)5 · H2OTric. 1 : P1
6.EC.15VeatchiteSr2B11O16(OH)5 · H2OMon. m : Bb
6.EC.15Veatchite-1MSr2B11O16(OH)5 · H2OMon. 2 : P21
6.EC.25TuzlaiteNaCaB5O8(OH)2 · 3H2OMon. 2/m : P21/b
6.EC.30HeidorniteNa2Ca3B5O8(SO4)2Cl(OH)2Mon. 2/m : B2/b
6.EC.35PopugaevaiteCa3[B5O6(OH)6]FCl2 · 8H2OMon. m : Pm
6.EC.35BrianroulstoniteCa3[B5O6(OH)6](OH)Cl2 · 8H2OMon. m

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 3.1870% 988 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity:

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

Other InformationHide

IR Spectrum:
Satimola dome material [cm-1]: 3400, 3300, 3175, 3020, 1685s, 1640w, 1510, 1410s, 1386s, 1366s, 1338s, 1266s, 1250sh, 1215w, 1175sh, 1156, 1137, 1099, 1068, 1015s, 982s, 936s, 903s, 840, 812, 763, 704, 626, 610, 572w, 548w, 494w, 475w.
Notes:
Insoluble in water at room temperature.
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 VolkovskiteHide

References for VolkovskiteHide

Reference List:

Localities for VolkovskiteHide

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.

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.
Canada
 
  • New Brunswick
    • Kings Co.
      • Cardwell Parish
        • Penobsquis
Grice et al. (2002)
      • Hammond Parish
        • Salt Springs evaporite deposit
Mandarino et al. (1990)
      • Studholm Parish
Grice et al. (2005)
Kazakhstan (TL)
 
  • Atyrau Region
    • Inder District
Kondrat’eva et al. (1966) +3 other references
  • West Kazakhstan Region
    • Oral
Tony Nikischer specimen
Russia
 
  • Irkutsk Oblast
    • Lower Tunguska
      • Nepa River basin
Pekov (1998) +1 other reference
Saudi Arabia
 
  • Medina Region
Faheha et al. (2012)
UK
 
  • England
    • North Yorkshire
      • Redcar and Cleveland
        • Loftus
Lavinsky (n.d.) +1 other reference
USA
 
  • Alabama
    • Clarke County
Rocks & Min.: 64:472.
 
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