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Dobrovolskyite

A valid IMA mineral species
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Formula:
Na4Ca(SO4)3
Lustre:
Vitreous
Hardness:
3½
Specific Gravity:
2.68 (Calculated)
Crystal System:
Trigonal
Name:
Named in honor of Prof. Dr. Vladimir Vitalievich Dolivo-Dobrovolsky (Владимир Витальевич Доливо-Добровольский) (1927–2009), St. Petersburg Mining Institute, one of the leading Russian scientists in the field of petrology, crystal optics and crystal chemistry.
Chemically and structurally related to bubnovaite. Also chemically similar to glauberite; also compare cesanite, antofagastaite, eugsterite, hydroglauberite, omongwaite, wattevillite; and 'ciempozuelite'.

Structure determined.


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Unique IdentifiersHide

Mindat ID:
54346
Long-form identifier:
mindat:1:1:54346:8

IMA Classification of DobrovolskyiteHide

Classification of DobrovolskyiteHide

7.AD.

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
A : Sulfates (selenates, etc.) without additional anions, without H2O
D : With only large cations

Mineral SymbolsHide

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

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

Physical Properties of DobrovolskyiteHide

Vitreous
Streak:
White
Hardness:
3½ on Mohs scale
Parting:
None observed
Fracture:
Conchoidal
Density:
2.68 g/cm3 (Calculated)
Comment:
Calculated based on empirical formula and single crystal unit-cell parameters

Optical Data of DobrovolskyiteHide

Type:
Uniaxial (+)
RI values:
nω = 1.489(2) nε = 1.491(2)
Max. Birefringence:
δ = 0.002
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:
Moderate (negative)
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 uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Dispersion:
None observed
Pleochroism:
Not Visible

Chemistry of DobrovolskyiteHide

Mindat Formula:
Na4Ca(SO4)3
Element Weights:
Element% weight
O45.688 %
S22.891 %
Na21.883 %
Ca9.537 %

Calculated from ideal end-member formula.
O
S
Na
Ca

Crystallography of DobrovolskyiteHide

Crystal System:
Trigonal
Class (H-M):
3 - Pyramidal
Space Group:
R3
Cell Parameters:
a = 15.7223(2) Å, c = 22.0160(5) Å
Ratio:
a:c = 1 : 1.4
Unit Cell V:
4713.1 ų
Z:
18

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45a : [Sulfates, arsenates, selenates, antimonates]

Type Occurrence of DobrovolskyiteHide

General Appearance of Type Material:
Aggregates of tabular crystals up to 1-2 mm in maximum dimension, with abundant gas inclusions.
Place of Conservation of Type Material:
Collections of the Saint Petersburg State University mineralogical museum, University Emb. 7/9, St. Petersburg 199034, Russia, catalogue number 1/19829
Geological Setting of Type Material:
Fumarole, about 200°C
Associated Minerals at Type Locality:

Other Language Names for DobrovolskyiteHide

Related Minerals - Strunz-mindat GroupingHide

7.AD.BubnovaiteK2Na8Ca(SO4)6Trig. 3m : P31c
7.AD.CalciolangbeiniteK2Ca2(SO4)3 Iso. 23 : P213
7.AD.MurphyitePb(Te6+O4)Mon. 2/m : P21/b
7.AD.CuprodobrovolskyiteNa4Cu(SO4)3Trig. 3 : R3
7.AD.KristjániteKNa2H(SO4)2Mon. 2/m
7.AD.05Mascagnite(NH4)2SO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.05ArcaniteK2SO4Orth. mmm(2/m2/m2/m)
7.AD.10MercalliteKHSO4Orth. mmm(2/m2/m2/m) : Pbca
7.AD.15MiseniteK8H6(SO4)7Mon.
7.AD.20Letovicite(NH4)3H(SO4)2Tric.
7.AD.25ThénarditeNa2SO4Orth. mmm(2/m2/m2/m) : Fddd
7.AD.25GlauberiteNa2Ca(SO4)2Mon. 2/m : B2/b
7.AD.30MetathénarditeNa2SO4Hex. 6/mmm(6/m2/m2/m) : P63/mmc
7.AD.30AnhydriteCaSO4Orth. mmm(2/m2/m2/m)
7.AD.35BaryteBaSO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.35CelestineSrSO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.35OlsacheritePb2(Se6+O4)(SO4)Orth.
7.AD.35AnglesitePbSO4Orth. mmm(2/m2/m2/m) : Pnma
7.AD.40