Calciolangbeinite
About Calciolangbeinite
Forms a solid solution with the latter. The content of 20 mol%, or more, of the langbeinite end-member induces breakdown into cubic lower-magnesian calciolangbeinite and langbeinite, upon slow cooling.
The calciolangbeinite-O (low-temperature) polymorph, although topologically similar to calciolangbeinite-C (probably stabilized by Mg admixture), is "the first natural orthorhombic langbeinite-like sulfate".
Note: the original (first-described) material was the cubic polymorph.
Unique Identifiers
IMA Classification of Calciolangbeinite
Classification of Calciolangbeinite
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
A : Sulfates (selenates, etc.) without additional anions, without H2O
D : With only large cations
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Clgb | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Calciolangbeinite
Optical Data of Calciolangbeinite
Relative to Canada balsam mounting medium (n ≈ 1.537).
Chemistry of Calciolangbeinite
Crystallography of Calciolangbeinite
| Calciolangbeinite-C | Calciolangbeinite-O |
|---|---|
| K2Ca2(SO4)3 | K2Ca2(SO4)3 |
| Isometric | Orthorhombic |
| 23 - Tetartoidal | 222 - Disphenoidal |
| P213 | P212121 |
| a = 10.1887(4) Å | a = 10.3330(2) Å, b = 10.5027(2) Å, c = 10.1763(2) Å |
| a:b:c = 0.984 : 1 : 0.969 | |
| V 1057.68 ų | V 1104.37 ų |
| 4 | 4 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 5.84 Å | (8) |
| 4.54 Å | (9) |
| 4.15 Å | (27) |
| 3.218 Å | (100) |
| 2.838 Å | (8) |
| 2.736 Å | (37) |
| 2.006 Å | (11) |
| 1.658 Å | (8) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 45a : [Sulfates, arsenates, selenates, antimonates] | |
| 46 : Near-surface hydrothermal alteration of minerals (see also #22) | |
| Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
| 51 : Pyrometamorphic minerals (see also #54 and #56) | <0.36 |
Type Occurrence of Calciolangbeinite
Synonyms of Calciolangbeinite
Other Language Names for Calciolangbeinite
Relationship of Calciolangbeinite to other Species
| Efremovite | (NH4)2Mg2(SO4)3 | Iso. 23 : P213 |
| Ferroefremovite | (NH4)2Fe2+2(SO4)3 | Iso. 23 : P213 |
| Langbeinite | K2Mg2(SO4)3 | Iso. 23 : P213 |
| Manganolangbeinite | K2Mn2(SO4)3 | Iso. 23 : P213 |
Related Minerals - Strunz-mindat Grouping
| 7.AD. | Bubnovaite | K2Na8Ca(SO4)6 |
| 7.AD. | Dobrovolskyite | Na4Ca(SO4)3 |
| 7.AD. | Murphyite | Pb(Te6+O4) |
| 7.AD. | Cuprodobrovolskyite | Na4Cu(SO4)3 |
| 7.AD. | Kristjánite | KNa2H(SO4)2 |
| 7.AD.05 | Mascagnite | (NH4)2SO4 |
| 7.AD.05 | Arcanite | K2SO4 |
| 7.AD.10 | Mercallite | KHSO4 |
| 7.AD.15 | Misenite | K8H6(SO4)7 |
| 7.AD.20 | Letovicite | (NH4)3H(SO4)2 |
| 7.AD.25 | Thénardite | Na2SO4 |
| 7.AD.25 | Glauberite | Na2Ca(SO4)2 |
| 7.AD.30 | Metathénardite | Na2SO4 |
| 7.AD.30 | Anhydrite | CaSO4 |
| 7.AD.35 | Baryte | BaSO4 |
| 7.AD.35 | Celestine | SrSO4 |
| 7.AD.35 | Olsacherite | Pb2(Se6+O4)(SO4) |
| 7.AD.35 | Anglesite | PbSO4 |
| 7.AD.40 | Kalistrontite | K2Sr(SO4)2 |
| 7.AD.40 | Palmierite | K2Pb(SO4)2 |
| 7.AD.45 | Ivsite | Na3H(SO4)2 |
| 7.AD.55 | Markhininite | TlBi(SO4)2 |
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) | 17.5117% | 5,429 | 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.
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: –
| Distance | Dose rate | Risk |
|---|---|---|
| 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
Fluorescence of Calciolangbeinite
Other Information
Internet Links for Calciolangbeinite
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References for Calciolangbeinite
Localities for Calciolangbeinite
Showing 4 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Israel | |
| Galuskin et al. (2016) |
Palestine | |
| Galuskina et al. (2019) |
| Galuskina et al. (2014) |
Russia (TL) | |
| Williams et al. (2011) +2 other references |


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Yadovitaya fumarole, Second scoria cone, Northern Breakthrough, Great Fissure eruption, Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia